大别造山带北缘中生代沉积学、盆地分析和构造演化
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摘要
以现代沉积学和大陆动力学理论为指导，结合岩石学、地球化学、同位素年代学等诸多学科，对大别山造山带北缘地区中生代地层进行沉积学、盆地分析以及构造演化研究。主要研究内容包括：①厘定大别山北缘地区中生代地层的年代格架；②划分岩相，确立沉积体系；③确定中生代盆地古流向，恢复盆地的古地理；④确定物源区物质组成、演绎物源区原始构造层序、建立盆地沉积物与物源区地质单元的耦合关系；⑤根据沉积学以及区域地质研究，重塑大别山中生代构造演化历史，探讨大别山造山带的碰撞成因机制。本文取得了如下成果和认识。
1．在周公山组中在凤凰台组中发现了火山凝灰岩层利火山岩碎屑，结合同位素年代学研究以及沉积相和重矿物对比，重新厘定了大别造山带北缘中生代地层的格架。为研究区沉积体系、造山带演化、折返年代学以及山盆耦合关系研究等奠定了基础。
2．根据岩相、相组合以及沉积层序的研究，确立了研究区的沉积作用类型和沉积体系，它们包括碎屑流和超浓缩洪流沉积、辫状河河道沉积，以及冲积扇沉积、洪泛平原沉积、扇三角洲沉积和湖相浊流沉积。在此基础上，建立了盆地的沉积体系格架。
3．通过古水流研究，恢复了大别造山带北缘中生代的古地理。沉积盆地的水系可以分为两类，一是靠近南缘的横向水系，它们主要是从南向北，另一类是靠近盆地中部的纵向水系，它们是从西向东。物源区主要位于南部，为大别造山带。
4．首次在毛坦厂组、凤凰台组中发现了榴辉岩砾石，这一发现表明大别造山带超高压变质岩在早白垩世已经折返到地表，而且地球化学研究表明这些榴辉岩砾石的原岩形成于岩浆岛弧构造背景。
5．物源分析表明，位于肥西地区中生代碎屑岩主要来自佛子岭群和卢镇关群变质岩，凤凰台组的源区来自于一个已经消失的以岛弧榴辉岩为代表的含超高压变质岩单元。大别杂岩在新第三纪已经遭受剥蚀，构成了正阳关组的物源。同时也揭示了大别造山带的折返剥露历史，大别造山带在早侏罗世(205-180Ma)之前快速抬升，侏罗纪经历了相对平静阶段。侏罗纪末(135Ma)到早白垩世源区产生剧烈的持续上升和剥蚀，早白垩世晚期，源区的构造转换为拉张。晚白垩世(95Ma)，盆地边缘与源区一道抬升，遭受剥蚀。
6．大别山北缘中生代沉积作用具有穿时特征，沉积作用开始时间自东向西依次为早中侏罗世、中晚侏罗世和早白垩世。揭示了大别山造山带的折返是穿时的，隆起自东向西进行，而其控制因素主要为NE向的断裂体系。
7．大别造山带是一个具有转换叠加性质的造山带。NE向郯庐断裂系的大型平移作用叠加在原来印支期消减带之上，产生新的俯冲。大别山造山带的构造模式是三叠纪扬子陆块的向北俯冲和侏罗纪华北陆块的向南俯冲，构成大别山造山带的对冲模式，其动力学背景是太平洋构造域对古特提斯构造域的叠加。
8．将大别山造山带的构造演化与华北、扬子陆块的演化紧密结合，提出了大别山造山带三开三合的构造演化特征，即新元古代的古岛弧发育和震旦纪的拼合、奥陶-早志留世的拉张和加里东期的拼合、二叠纪-早三叠世的拉张和印支期的拼合以及侏罗纪-新生代的折返隆升剥蚀。
This research focuses on the sedimentology, basin analysis and tectonic evolution of Mesozoic strata in the north margin of the Dabie Orogenic Belt, using an integrated approach of modern sedimentology, continental dynamics, petrology, geochemistry and isotope chronology. The topics of the study include: (1). establishing the time framework of Mesozoic strata in the north margin of the Dabie Orogenic Belt; (2). analysis of lithofacies and sedimentary systems; (3). ascertaining the paleocurrent direction of the Mesozoic basin and reconstructing the paleogeography; (4). deciding the material components and original structure sequences of the basin provenance, and coupling relationship between the sediments of the basin and geologic units of the provenance; (6). establishing the Mesozoic tectonic evolution history of the Dabie Orogenic Belt and discussing the collisional mechanism of the Belt. The results are listed as follows.
1.The framework of Mesozoic strata in the north margin of the Dabie Orogenic Belt was reestablished according to the discovery of the tuff beds and volcanic debris in Zhougongshan and Fenghaungtai Formations, along with their isotope ages and the correlations of sedimentary facies and heavy minerals. This result lays a solid foundation for the research.
2.Based on the study of petrology facies, facies association and sedimentary sequences, the sedimentary processes and systems are established. They consist of debris and hyper concentration flow deposits, channel deposit of braided and meandering streams, and alluvial fans, floodplains, fan-deltas and lacustrine turbidities. Based on these results, the framework of sedimentary system in the study area is established.
3.The Mesozoic paleogeography of the north margin of the Dabie Orogenic Belt was established according to the paleocurrent study. Water system of the sedimentary basin is divided into two classes: one is transverse water system adjacent to the south margin of the basin , which flows from the south to the north, the other is longitudinal water system close to the midst and flows front the west to the east. The provenance of the basin is located in the south, which covers the Dabie Orogenic Belt.
4.It is the first time that eclogite conglomerates are discovered in Maotangchan and Fenghuangtai Formations. This suggests that ultra-high pressure metamorphic rocks in the Dabie Orogenic Belt exhumed to the earth's surface in Lower Cretaceous. The geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc.
5.Based on the analysis of their source rocks, the Mesozoic detrital rocks in Feixi area are mainly derived from metamorphic rocks of Fuziling and Luzhengguan Groups, and the provenance of Fenghuangtai Formation is a disappeared ultra-high pressure metamorphic rock unit characterized with inland arc eclogites. The Dabie complex suffered denudation in Neogene and constitutes the source rocks of Zhengyangguan Formation. These facts indicate that the Dabie Orogenic Belt was uplifted rapidly before the early Jurassic (205-180Ma), and went through a long period of tectonic calm during the Jurassic. At the late stage of Upper Jurassic (135ma), the provenance areas underwent intense and sustained uplift and denudation. In the period of Lower Cretaceous, the tectonic setting of the provenance areas turned into strike-slip. In the Later Cretaceous (95Ma), the provenance
areas and the margin of the basin uplifted and suffered denudation together.
6.The Mesozoic sedimentation in the north margin of the Dabie Orogenic Belt is diachronous. From east to west, the onset of the sedimentation is successively in Lower-Middle Jurassic, Middle-Later Jurassic and Lower Cretaceous. This indicates that the exhumation of the Dabie Orogenic Belt was diachronous, and that its uplift happened from east to west and was mainly controlled by the NE fault system.
7.The Dabie Orogenic Belt is of transformation and superposition character. Its new superimpose
1．在周公山组中在凤凰台组中发现了火山凝灰岩层利火山岩碎屑，结合同位素年代学研究以及沉积相和重矿物对比，重新厘定了大别造山带北缘中生代地层的格架。为研究区沉积体系、造山带演化、折返年代学以及山盆耦合关系研究等奠定了基础。
2．根据岩相、相组合以及沉积层序的研究，确立了研究区的沉积作用类型和沉积体系，它们包括碎屑流和超浓缩洪流沉积、辫状河河道沉积，以及冲积扇沉积、洪泛平原沉积、扇三角洲沉积和湖相浊流沉积。在此基础上，建立了盆地的沉积体系格架。
3．通过古水流研究，恢复了大别造山带北缘中生代的古地理。沉积盆地的水系可以分为两类，一是靠近南缘的横向水系，它们主要是从南向北，另一类是靠近盆地中部的纵向水系，它们是从西向东。物源区主要位于南部，为大别造山带。
4．首次在毛坦厂组、凤凰台组中发现了榴辉岩砾石，这一发现表明大别造山带超高压变质岩在早白垩世已经折返到地表，而且地球化学研究表明这些榴辉岩砾石的原岩形成于岩浆岛弧构造背景。
5．物源分析表明，位于肥西地区中生代碎屑岩主要来自佛子岭群和卢镇关群变质岩，凤凰台组的源区来自于一个已经消失的以岛弧榴辉岩为代表的含超高压变质岩单元。大别杂岩在新第三纪已经遭受剥蚀，构成了正阳关组的物源。同时也揭示了大别造山带的折返剥露历史，大别造山带在早侏罗世(205-180Ma)之前快速抬升，侏罗纪经历了相对平静阶段。侏罗纪末(135Ma)到早白垩世源区产生剧烈的持续上升和剥蚀，早白垩世晚期，源区的构造转换为拉张。晚白垩世(95Ma)，盆地边缘与源区一道抬升，遭受剥蚀。
6．大别山北缘中生代沉积作用具有穿时特征，沉积作用开始时间自东向西依次为早中侏罗世、中晚侏罗世和早白垩世。揭示了大别山造山带的折返是穿时的，隆起自东向西进行，而其控制因素主要为NE向的断裂体系。
7．大别造山带是一个具有转换叠加性质的造山带。NE向郯庐断裂系的大型平移作用叠加在原来印支期消减带之上，产生新的俯冲。大别山造山带的构造模式是三叠纪扬子陆块的向北俯冲和侏罗纪华北陆块的向南俯冲，构成大别山造山带的对冲模式，其动力学背景是太平洋构造域对古特提斯构造域的叠加。
8．将大别山造山带的构造演化与华北、扬子陆块的演化紧密结合，提出了大别山造山带三开三合的构造演化特征，即新元古代的古岛弧发育和震旦纪的拼合、奥陶-早志留世的拉张和加里东期的拼合、二叠纪-早三叠世的拉张和印支期的拼合以及侏罗纪-新生代的折返隆升剥蚀。
This research focuses on the sedimentology, basin analysis and tectonic evolution of Mesozoic strata in the north margin of the Dabie Orogenic Belt, using an integrated approach of modern sedimentology, continental dynamics, petrology, geochemistry and isotope chronology. The topics of the study include: (1). establishing the time framework of Mesozoic strata in the north margin of the Dabie Orogenic Belt; (2). analysis of lithofacies and sedimentary systems; (3). ascertaining the paleocurrent direction of the Mesozoic basin and reconstructing the paleogeography; (4). deciding the material components and original structure sequences of the basin provenance, and coupling relationship between the sediments of the basin and geologic units of the provenance; (6). establishing the Mesozoic tectonic evolution history of the Dabie Orogenic Belt and discussing the collisional mechanism of the Belt. The results are listed as follows.
1.The framework of Mesozoic strata in the north margin of the Dabie Orogenic Belt was reestablished according to the discovery of the tuff beds and volcanic debris in Zhougongshan and Fenghaungtai Formations, along with their isotope ages and the correlations of sedimentary facies and heavy minerals. This result lays a solid foundation for the research.
2.Based on the study of petrology facies, facies association and sedimentary sequences, the sedimentary processes and systems are established. They consist of debris and hyper concentration flow deposits, channel deposit of braided and meandering streams, and alluvial fans, floodplains, fan-deltas and lacustrine turbidities. Based on these results, the framework of sedimentary system in the study area is established.
3.The Mesozoic paleogeography of the north margin of the Dabie Orogenic Belt was established according to the paleocurrent study. Water system of the sedimentary basin is divided into two classes: one is transverse water system adjacent to the south margin of the basin , which flows from the south to the north, the other is longitudinal water system close to the midst and flows front the west to the east. The provenance of the basin is located in the south, which covers the Dabie Orogenic Belt.
4.It is the first time that eclogite conglomerates are discovered in Maotangchan and Fenghuangtai Formations. This suggests that ultra-high pressure metamorphic rocks in the Dabie Orogenic Belt exhumed to the earth's surface in Lower Cretaceous. The geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc.
5.Based on the analysis of their source rocks, the Mesozoic detrital rocks in Feixi area are mainly derived from metamorphic rocks of Fuziling and Luzhengguan Groups, and the provenance of Fenghuangtai Formation is a disappeared ultra-high pressure metamorphic rock unit characterized with inland arc eclogites. The Dabie complex suffered denudation in Neogene and constitutes the source rocks of Zhengyangguan Formation. These facts indicate that the Dabie Orogenic Belt was uplifted rapidly before the early Jurassic (205-180Ma), and went through a long period of tectonic calm during the Jurassic. At the late stage of Upper Jurassic (135ma), the provenance areas underwent intense and sustained uplift and denudation. In the period of Lower Cretaceous, the tectonic setting of the provenance areas turned into strike-slip. In the Later Cretaceous (95Ma), the provenance
areas and the margin of the basin uplifted and suffered denudation together.
6.The Mesozoic sedimentation in the north margin of the Dabie Orogenic Belt is diachronous. From east to west, the onset of the sedimentation is successively in Lower-Middle Jurassic, Middle-Later Jurassic and Lower Cretaceous. This indicates that the exhumation of the Dabie Orogenic Belt was diachronous, and that its uplift happened from east to west and was mainly controlled by the NE fault system.
7.The Dabie Orogenic Belt is of transformation and superposition character. Its new superimpose
引文
[1] 安徽省地质局区域地质调查队．1：20万六安幅、岳西幅区域地质调查报告．1974，432
[2] 安徽省区域地层编写组．华东地区地层表(安徽省分册)．北京：地质出版社．1978，181-185
[3] 安徽省地质矿产局．安徽省区域地质志．北京：地质出版社，1987，721
[4] 安徽省地质局区域地质调查队．安徽省地层志．前寒武纪分册．合肥：安徽科学技术出版社，1988，170
[5] 安徽省地质矿产局．安徽省岩石地层．武汉：中国地质大学出版社，1997，198．206
[6] 曹荣龙，朱寿华．大别山含柯石英榴辉岩区一个晚太古代的超高压变质带．地质学报，1995，69(3)：232-242
[7] 陈宣华，王小凤，张青，等．郯庐断製带形成演化的年代学研究．长春科技大学学报，2000，30(3)：215-220
[8] 陈跃志，桑宝梁．佛子岭群变质岩石学变质作用及时代的初步研究．中国区域地质，1995，14(3)：280-288
[9] 陈华成，吴其切．长江中下游地层志．合肥：安徽科学技术出版社．1989，528-529
[10] 陈江峰，董树文，邓衍尧，等．大别造山带钾氩年龄的解释—差异上升的地块．地质论评，1993，39(1)：17-22
[11] 陈江峰，谢智，刘顺生，等．大别造山带冷却年龄的 ~(40)Ar/~(39) Ar和裂变径迹测定．中国科学(B辑)，1995，25(10)：1086-1092
[12] 陈丕基．郯庐断裂巨大平移的时代与格局．科学通报，1989，34(4)：289-293
[13] 陈丕基．中国陆相侏罗-白垩系划分对比评述．地层学杂志，2000，24(2)：114-119
[14] 陈世悦．华北地块南部晚古生代至三叠纪沉积构造演化．中国矿业大学学报，2000，29(5)：536-540
[15] 程裕淇，刘敦，Williams，等．大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析．地质学报，2000，74(3)：193-205
[16] 从柏林，王清晨．大别山苏鲁超高压变质带研究的最新进展．科学通报，1999，44(11)：1127-1141
[17] 丁林．东喜马拉雅构造自上新世以来快速抬升的裂变径迹证据．科学通报，1995，40(16)：1497-1501
[18] 董树文，孙先如，张勇，等．大别山碰撞造山带基本结构．科学通报，1993，38(6)：542-545
[19] 邓晋福，叶德隆，赵海玲，等．下扬子地区火山左右深部过程与盆地形成．武汉：中国地质大学出版社，1992，184
[20] 杜建国，张鹏．大别山北部的中生代火山岩．现代地质，1999，13(1)：57-65
[21] 杜建国．大别造山带中生代岩浆作用与成矿地球化学研究．合肥工业大学博士论文，2000，176
[22] 冯宁升，丁保良．浙江白垩系古地磁研究的新认识．《第三届全国地层会议论文集》编委会．第三届全国地层会议论文集．北京：地质出版社，2000，300-303
[23] 冯增昭．下扬子地区中、下三叠统青龙群岩相古地理研究．昆明：云南科技出版社，1988，197
[24] 傅斌，郑永飞，肖益林，等．大别山苏家河地区榴辉岩和大理岩的地球化学研究．地质学报，1998，72(4)：323-338
[25] 高山，张本仁，谷晓明，等．华北与扬子板块志留-泥盆纪对接的沉积地球化学证据．中国科学(B辑)，1991，6：645-651
[26] 葛宁洁，周导之．安徽肥东群变质岩的同位素地质定年．安徽地质，1993，3(3)：22-25
[27] 管运财，高天山．等．大别山(安徽)中生代花岗岩类岩体特征与形成机制．安徽地质，1995，5(3)：19-28
[28] 金玉轩，王向东，王钥．国际地层表．地层学杂志，2003，27(2)：161
[29] 郭振宇，董火根，郭令智．大别造山带变质岩地层年龄及其构造意义．地层学杂志，1998，22(3)：185-195
[30] 韩树芬等．安徽北部中新生代沉积盆地分析．北京：地质出版社，1996，18-19
[31] 韩宗珠，袁齐林，盛兴土．安徽岳西碧溪岭榴辉岩及伴生石榴石橄榄岩的岩石学和地球化学．岩石学报，1989，4：22-33．
[32] 郝杰，刘小汉．桐柏．大别碰撞造山带大型推覆-滑脱构造及其演化．地质科学，1988，(1)：1-10
[33] 河南省地质矿产局．河南省区域地质志．北京：地质出版社，1989，772
[34] 胡克，张树业，周高志，等．鄂北榴辉岩带地质．长春地质学院学报，1989(鄂皖蓝片岩带地质专辑)，84-95
[35] 胡世玲，郝杰，李曰俊，等．大别山碧溪岭榴辉岩激光探针Ar-Ar年龄．地质科学，1999，34(4)：427-431
[36] 黄汲青．中国主要地质构造单位(英文)．地质专报甲种20号，1945，162
[37] 黄汲清，姜春发．从多旋回构造运动观点初步探讨地壳发展规律．地质学报，1962，42，2：105-152
[38] 黄杏珍，何明喜，李振西，等．中国河南省白湾盆地的白垩系特征．沉积学报，1996，14(增刊)：38-47
[39] 简平，杨巍然，李志昌，等．大别山西部熊店加里东期榴辉岩-同位素地质年代学的证据．地质学报，1997，71(2)：113—140
[40] 贾红义，刘国宏，张云银，等．合肥盆地形成机制与油气勘探前景．安徽地质，2001，11(1)：9-18
[41] 贾蓉芬，赵林，江钠言．安徽巢湖地区二叠系有机地球化学特征及其古环境意义．沉积学报，1996，14(2)：21-29
[42] 江来利，刘贻灿，吴维平，等．大别山北部漫水河灰色片麻岩的锆石U-Pb年龄及其地质意义．地球化学，2002，31(1)：66-70
[43] 姜再兴，赵澄林，熊继辉．皖中下志留统的等深岩及其地质意义．科学通报，1989，34(20)：1575-1576
[44] 金成伟，郑祥身．大别岳西地区花岗岩类岩石学及其成因．岩石学报，1998，14(4)：493-502
[45] 金福全，颜怀学，吕培基，等．北淮阳区地层研究的新进展-论北淮阳区的地层层序．合肥工业大学学报(地质论文专辑)，1987，9：3-12
[46] 晋慧娟，李育慈．西秦岭造山带中三叠统复理石相研究．沉积学报，2001，19(3)：321-326
[47] 李宝芳，马文璞，张惠良，等．大别山北麓石炭纪盆地沉积和构造研究．地学前缘，2000，7(3)：153-166
[48] 李春昱．用板块构造学说对中国部分地区构造发展的初步分析．地球物理学报，1975，18(1)：52-76
[49] 李石，王彤．桐柏山-大别山花岗岩类地球化学．武汉：中国地质大学出版社，1991，208
[50] 李曙光，Hart S R，郑双根，等．中国华北、华南陆块碰撞时代的Sm-Nd同位素年龄证据．中国科学(B辑)，1989，(3)：312—319
[51] 李曙光，孙卫东，葛宁洁，等．青岛榴辉岩相蛇绿混杂岩的岩石学证据及退变质P-T轨迹．岩石学报，1992，8(4)：351-362．
[52] 李曙光．蛇绿岩生成构造环境的Ba-Th-Nb-La判别图．岩石学报，1993，9(2)：146-157．
[53] 李任伟，江茂生，李忠，等．大别山北麓侏罗系大理岩砾石的碳-氧同位素组成及地质意义．岩石学报，1999，15(4)：623—629
[54] 李任伟，李忠，江茂生，等．合肥盆地碎屑石榴石组成及其对源区恢复和地层对比的意义．中国科学(D辑)，2000，30(增刊)：91-98
[55] 李任伟．孙枢，李忠，江茂生，金福全．奎双座．高压-超高压岩石对合肥盆地侏罗系沉积的贡献．岩石学报，2002，18(4)：526-530
[56] 李四光．新华夏海之起源．区域地质构造分析．北京：科学出版社，1974，49-58
[57] 李双应．安徽巢县南陵湖组火山碎屑流沉积物的发现．地层学杂志，1996，20(4)：277-279
[58] 李双应．安徽巢湖地区早三叠世火山碎屑流的岩石学特征及形成机理．安徽地质，2000，10(1)：24-28
[59] 李双应，李忠，王忠诚．等．胜利油区孤岛油田馆上段沉积模式研究．沉积学报，2001a，19(3)：386-393
[60] 李双应，洪天求，金福全．等．巢县二叠系栖霞组臭灰岩段异地成因碳酸盐岩．地层学杂志，2001b，25(1)：69-73
[61] 李双应，岳书仓，王道轩，等．大别造山带超高压变质岩折返隆升的地层学证据-晚侏罗世榴辉岩砾石的启示．地质论评，2002a，48(4)：345-352
[62] 李双应，岳书仓，王道轩，等．大别造山带北缘中生代地层格架厘定．地层学杂志，2002b，26(3)：178-186
[63] 李双应，王道轩，刘因，等．大别造山带北缘中生代冲积沉积体系对源区构造的沉积响应．地质通报，2002c，21(8-9)：541-546
[64] 李双应，岳书仓．安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积．沉积学报，2002d，20(1)：7-12
[65] 李双应，李任伟，岳书仓，等．大别造山带北缘石炭系胡油坊组砾石特征及其构造意义．地层学杂志，2003a，27(2)：116-121
[66] 李双应，岳书仓，王道轩，等．大别造山带北缘中生代地层中榴辉岩砾石地球化学特征及构造意义．地球化学，2003b，32(5)：436-444
[67] 李双应，岳书仓，杨建，等．皖北新元古代刘老砷组页岩的地球化学特征及其地质意义．地质科学，2003c，38(2)：241-253
[68] 李阳，李双应，岳书仓，等．胜利油用孤岛油区馆陶组上段沉积结构单元．地质科学，2002，37(2)：219-230
[69] 李耀西，汪迎平，丁保良．中国东南部白垩系综合地层学研究的新进展．地质学报，2001，75(4)：451-458
[70] 李勇，王成善，曾允孚．造山作用与沉积响应．矿物岩石，2000，20(2)：49-56
[71] 李忠，李任伟，孙枢，等．合肥盆地南部侏罗系砂岩碎屑组分及其物源构造属性．岩石学报，1999，15(3)：438-445
[72] 李忠，孙枢，李任伟，等．合肥盆地中生代充填序列及共对大别山造山作用的指示．中国科学(D辑)，2000，30(3)：256-263
[73] 李忠，李任伟，孙枢，等．大别地块北缘侏罗系花岗岩类砾石的Rb-Sr年代学特征．科学通报，2001，46(7)：582-585
[74] 刘宝珺．沉积岩石学．北京：地质出版社，1980，497
[75] 刘护军．秦岭新生代构造隆升研究．陕西师范大学学报(自然科学版)，2002，30(1)：121-124
[76] 刘景波，游振东，钟增球．豫南鄂北大别山中部和北部的榴辉岩类．中国科学(D辑)，1996，26(3)：277-281
[77] 刘少峰，张国伟，张宗清，等．合肥盐地花岗岩砾石的同位素年代学示踪．科学通报，2001，46(9)：748-753
[78] 刘晓春．大别山榴辉岩的成因-原岩属性提供的证据．安徽地质，1992，2(4)：24-34．
[79] 刘晓春，胡克，李学燮，等．大别-苏鲁高压变质带中榴辉岩的多样性及其成因．地质论评，1994，40(6)：494—501
[80] 刘贻灿，徐树桐等．佛子岭群的岩石化学及构造环境．安徽地质，1996，6(2)：1-6．
[81] 刘贻灿，徐树桐，李曙光，等．大别山北部榴辉岩的地球化学特征和Sr，Nd同位素组成及其大地构造意义．中国科学(D辑)，2000，30(增刊)：99—107
[82] 刘志刚，富云莲，牛宝贵，等．大别山北坡苏家河群及原信阳群龟山组变基性杂岩 ~(40)Ar-~(39)测年及其地质意义．科学通报，1993，38(13)：1214-1218
[83] 陆光森，金福全，王道轩．河南固始杨山组底砾岩中早古生代化石的新发现及其意义．合肥工业大学学报(地质论文专辑)，1987：13-19
[84] 陆光森，金福全，五道轩．河南商城胡油坊组中Protomonocarina(原单脊叶肢介)的发现及其重要意义．合肥工业大学学报(地质论文专辑)，1987，9：20-24
[85] 陆镜元．大别山东段佛子岭(片岩系)群的时代．地质论评，1963，21(1)：155-161
[86] 马昌前，杨坤光，许长海，等．大别山中生代钾质岩浆作用与超高压变质地体的剥露机理．岩石学报，1999，15(3)：379-395
[87] 马文璞，王关玉，王果胜．佛子岭岩群中的晋宁期深成岩带及其构造意义．地质论评，2000，47(5)：476-482
[88] 潘国强，吴海权．大别山碰撞造山带后缘的火山作用．李兆鼎，王碧香．火山岩、火山作用及有关矿产．北京：地质出版社，1993，45-51
[89] 潘国强，陆现彩，于航波．北淮阳中生代adakite岩石地球化学特征及成因讨论．岩石学报，2001，17(4)：541-550
[90] 任纪舜，张正坤．论秦岭造山带．秦岭造山带学术讨论会论文选集．1991，99-109
[91] 任润生．合肥盆地周公山群中火山岩砾石的发现及意义．华东地质，1979，3，27-31
[92] 孙勇．东秦岭古洋盆与加里东运动．地质论评，1991，37(6)：555-559
[93] 桑宝梁．陈跃志，邵桂清．大别山东南麓宿松群铷-锶年龄及其构造意义．中国区域地质，1987，4：364-370
[94] 桑隆康，王人镜，张泽明，等．九资河-天堂寨地区燕山晚期花岗岩与大别造山带核部隆升．地质学报，2000，74(3)：234—246
[95] 索书田，钟增球，游振东，等．大别-苏鲁超高压和高压变质带碰撞后韧性伸展构造框架．安徽地质，2000，10(3)：212—215
[96] 沈渭洲，凌洪飞，王德滋，等．浙江省中生代火成岩的Nd-Sr同位素研究．地质科学，1999，34(2)：223-232
[97] 苏育民．大别山北麓变质岩的时代问题．地质论评，1960，20(6)：258-261
[98] 汤加富，孙先如，候明金，等．安徽大别山-张八岭地区新的构造格局与非板块碰撞造山过程．安徽地质，1995，5(1)：1-12．
[99] 陶铨，徐明才，袁晓儒，等．鄂东北前寒武纪地层地质年代研究．中国地质科学院天津地质研究所所刊，1986，16：75-89
[100] 万天丰，朱鸿，赵磊，等．郯庐断裂带的形成与演化综述．现代地质，1996，10(2)：159-168
[101] 王道轩，李双应，刘因，等．六安小华山周公山组火山碎屑岩的发现及意义．安徽地质，2000，10(4)，248—251
[102] 王道轩，金福今，谢宪德，等．合肥盆地三尖铺组 ~(40)Ar-~(39)Ar同位素年代地层学研究．地层学杂志，2000，24(3)：236—242
[103] 王道轩，刘因，李双应，等．大别超高压变质岩折返至地表的时间下限：大别山北麓晚侏罗世砾岩中发现榴辉岩砾石．科学通报，2001，46(14)：1216-1220
[104] 王强，许继锋，赵振华，等．大别山燕山期亏损重稀十元素花岗岩类的成因及动力学意义．岩石学报，2001，17(4)：551-564
[105] 王清晨，张儒瑗，从柏林，等．鲁东-苏北榴辉岩的构造特征及其折返机制．岩石学报，1992，8(2)：153-160．
[106] 王清晨，从柏林，马力．大别山造山带与合肥盆地的构造偶合．科学通报，1997，42(6)：575-580
[107] 王清晨，从柏林．大别山超高压变质带的大地构造框架．岩石学报，1998，14(4)：481-492
[108] 王清晨．中国超高压变质岩十五年研究进展．地球学报，2001，22(1)：11-16
[109] 王式光，谭绪荣，赵云龙．苏北榴辉岩的稀土元素地球化学及其成因讨论．地质论评，1995，41(5)：401-408
[110] 王随继，任明达．根据河道形态和沉积物特征的河流新分类．沉积学报，1999，17(2)：240-246
[111] 王晓燕，崔文元，刘树忠，等．豫南地区含柯石英榴辉岩的发现．岩石学报，1993，9(2)：181-185．
[112] 王蓉，沈后．合肥盆地侏罗-白垩系界线附近的孢粉组合．地球科学进展学术讨论会编辑委员会．地球科学进展-学术讨论会论文摘要．武汉，中国地质大学出版社，1992，78-79
[113] 王岳军，范蔚，郭锋．北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束．科学通报，2002，47(20)：1528-1534
[114] 王中刚，于学元，赵振华．稀土元素地球化学．北京：科学出版社，1989，535
[115] 魏春景，单振刚，张立飞，等．1997．北大别榴辉岩的确立及其地质意义．科学通报，42(17)：1832-1836
[116] 吴根耀．造山带地层学．成都：四川科学技术出版社，2000，98-101
[117] 吴浩若．放射虫硅质岩对华南古地理的启示．古地理学报，1999，1(2)：28-35
[118] 吴利仁，徐贵忠．东秦岭-大别山碰撞造山带的地质演化．北京：科学出版社，1998，177-183
[119] 吴元保，陈道公，Deloule，E．等．北大别片麻岩的锆石 U-Pb离子探针测定及其地质意义．地质论评，2001，47(3)：239-244
[120] 夏邦栋，李培军．中国东部扬子板块同华北板块在中．晚三叠世拼接的沉积学证据．沉积学报，1996，14(1)：12-20
[121] 肖庆辉，李晓波，贾跃明，等．当代造山带研究中值得重视的若干前沿问题．地学前缘，1995,2(1-2)：43-50
[122] 薛爱民，金维浚，袁学诚．大别山北缘合肥盆地中、新生代构造演化．高校地质学报，1999，5(2)：157-163
[123] 徐辉．华北地区石炭二叠系陆源物质及来源分析．石油实验地质，1987，9(1)：57-64
[124] 徐嘉炜．初论大别山碰撞带．合肥工业大学学报，1981，3：82-94
[125] 徐嘉炜，朱光，吕培基，等．郯庐断裂带平移年代学研究的进展．安徽地质，1995，5(1)：1-12．
[126] 徐树桐，江来利，刘贻灿，等．大别山区(安徽部分)的构造格局和演化过程．地质学报，1992，66(1)：1-14
[127] 徐树桐，刘贻灿，江来利，等．大别山的构造格局和演化．北京：科学出版社，1994，34—60
[128] 徐树桐，刘贻灿，吴维平，等．大别山造山带研究的主要进展及存在问题．自然科学进展，2001，11(8)：796-803
[129] 许志琴．扬子板块北缘的大型深层滑脱构造及动力学分析．中国区域地质，1987，6(4)：289-300
[130] 颜怀学，金福全，吕培基，等．关于中国南北板块在北淮阳地区界线的探讨．石油天然气地质，1988，9(2)：125-132
[131] 杨坤光，马昌前，简平，等．大别山北缘两次俯冲(碰撞)的岩石学和构造学证据．中国科学(D辑)，2000，30(4)：364-372
[132] 杨巍然，王国灿，简平．大别造山带构造年代学．武汉：中国地质大学出版社，2000，68-128
[133] 杨巍然，王国灿，李长安．造山带中、新生代隆升作用构造年代学研究新进展．地质科技情报，1999，19(4)：19-22
[134] 杨为民，杨有根．北淮阳地区的中生界．安徽地质，1995，5(4)：11-17
[135] 杨志坚．佛子岭群的地质时代问题．地质论评，1964，22(5)：327-336
[136] 杨志坚．试论桐柏-大别山地质构造演化特征．地质学报，1982，56(2)：123-135
[137] 杨祝良，沈加林，沈渭洲，等．大别山北缘中生代火山-侵入岩锶-钕同位素组成特征及其物质来源．岩石矿物学杂志，2002，22(3)：223-230
[138] 杨祝良，沈加林，沈渭洲，等．北淮阳中生代火山-侵入岩同位素年代学研究．．地质论评，1999，45(增刊)：674-680
[139] 叶凯，徐平．山东荣城大疃榴辉岩成因岩石学研究．岩石学报，1992，8(1)：27-39
[140] 叶大年，李达周，董光福，等．河南信阳变质带的3T型多硅白云母和C型榴辉岩．科学通报，1979，5：217-220
[141] 伊海生，王成善，李亚林，等．构造事件的沉积响应．沉积与特提斯地质，2001，21(2)：1-15
[142] 俞云文，徐步台．浙江中生代晚期火山-沉积岩系层序和时代．地层学杂志，1999，23(2)：136-145
[143] 于在平，孙勇，张成立．秦岭尚丹缝合带变质砂岩地球化学特征及构造环境探讨．地质论评，1991，37(6)：492-507
[144] 游振东，索书田，钟增球，等．大别山超高压变质岩的退变质显微构造：折返过程的启示．地质学报，2000，74(3)：224—233
[145] 翟明国，从柏林．苏鲁-大别山变质带岩石大地构造学．中国科学(D辑)，1996，26(30：258～264
[146] 张国栋，朱静昌，仇福康，等．早、中三叠世下扬子海沉积盆地研究．地质学报，1989，63(2)：134-146
[147] 张国伟，孟庆任，于在平，等．秦岭造山带的造山过程及其动力学特征．中国科学(D辑)，1996，26(3)：193-208
[148] 张建珍，杜建国，张友联，等．大别山榴辉岩岩石学及地球化学特征．地质论评，1998，44(3)：255-263
[149] 张鹏，北淮阳东段几组铷锶等时线年龄及其区域地质意义．中国区域地质，1996，15(4)：304-310
[150] 张鹏．北淮阳东段变花岗岩的锆石U-Pb年龄及地层意义．安徽地质，1999，9(2)：90-93
[151] 张希道，陈允福，王桂枝．鲁东南莒南县一带榴辉岩的特征．岩石学报，1992，8(1)：40-49．
[152] 张旗，简平，刘敦一，等．宁芜火山岩的锆石SHRIMP定年及其意义．中国科学(D辑)2003，33(4)：309-314
[153] 张旗，马宝林，刘若新，等．一个消减带之上的大陆岩石圈地幔残片-安徽饶拨寨超镁铁岩的地球化学特征．中国科学，1995，25(8)：967-973
[154] 张儒媛，从柏林，刘忠光．苏鲁超高压变质地体及其成因研究．岩石学报，1993a，9(3)：211-225
[155] 张儒嫒，刘忠光，王小民，等．中国中部河南省榴辉岩中柯石英的发现及冀其构造意义．岩石学报，1993b，9(2)：186-191．
[156] 张希道，陈允福，王桂枝．鲁东南莒南县一带榴辉岩的特征．岩石学报，1992，8(1)：40-49
[157] 张一勇，李建国．江苏白垩纪孢粉组合序列．地层学杂志，2000，24(1)：65-71
[158] 张勇，江来利，刘贻灿．大别山超高压榴辉岩带榴辉岩的特征和变质作用．岩石学报，1991，3：1-13．
[159] 张泽明，游振东，韩郁箐，等．大别-苏鲁榴辉岩带的岩石学、变质作用过程及成因研究．地质学报，1995，69(4)：306-325
[160] 赵宗举，杨树锋，陈汉林，等．合肥盆地基底构造属性．地质科学，2000，35(3)：288-296
[161] 郑文武．大别山东段“佛子岭群”的划分和时代问题．地质论评，1964，22(5)：337-347
[162] 郑祥身，金成伟，翟明国，等．1999．北大別灰色片麻岩的岩石化学特征及大地构造背景．岩石学报，15(3)：350-358
[163] 《中国地层典》编委会．中国地层典-侏罗系．北京：地质出版社．2000，24-26
[164] 《中国地层典》编委会．中国地层典-白垩系．北京：地质出版社．2000，11-21
[165] 钟大赉，丁林．青藏高原隆升过程及其机制探讨．中国科学(D辑)，1996，26(4)：289-295
[166] 周鼎武，董云鹏，华洪，等．“磨拉石建造”和“不整合”在地层对比中的意义．地质论评，1996，42(5)：416-423
[167] 周汉文，李献华，刘颖．南大别花凉亭榴辉岩退变质作用过程的元素地球化学变异．地球化学，1997，26(5)：25-33
[168] 周存亭，高天山，汤加富，等．安徽大别山北部榴辉岩的分布及主要特征．中国区域地质，2000，19(3)：253-257
[169] 周存亭，汤加富，等．大别山地区片麻岩套的建立与成岩时代讨论．安徽地质，1995，5(3)：29-40．
[170] 周泰祕，陈江峰，李学明，等．安徽霍舒正长岩带侵入体的Ar-Ar法同位素地质年龄．安徽地质，1992，2(1)：4-11
[171] 周祖翼，许长海，Reiners P. W等．大别山天堂寨晚白垩世以来剥露历史的(U-Th)／He和裂变径迹分析证据．科学通报，2003，48(6)：599-602
[172] 朱光，宋传中，王道轩，等．郯庐断裂带走滑时代的 ~(40)Ar/~(39)Ar年代学研究及其构造意义．中国科学(D辑)，2001，31(3)：250-256
[173] 朱洪发，秦德余，刘翠章．论华南孤峰组和大隆组硅质岩成因、分布规律及其构造机制．石油实验地质，1989，11(4)：341-348
[174] 朱夏，徐旺．中国中新生代沉积盆地．北京：石油工业出版社，1990，319
[175] Ames L, Tilton G R, Zhou G.Timing of collision of the Sino- Korean and Yangtze cratons: U - Pb zircon dating of coesite -bearing edogites: Geology, 1993, 21: 339-342.
[176] Baker J A, Matthews M D, Rowley D, et al. Fluid- rock interactions during ultra - high pressure metamor-phism, Dabie Shan, China. Geochimica et Cosmochimica Acta, 1997, 61:1685-1696
[177] Behrensmeyer A k, Tauxe L. lsochronous fluvial systems in Miocene deposits of northern Pakistan. Sedimentaology, 1982, 29:331-352
[178] Bhatia M R. Plate tectonics and geochemical composition of sandstones. Journal of Geology, 1983, 91(6): 611-627
[179] Bhatia M R, Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology, 1986, 92:181-193
[180] Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks: Province and tectonic control. Sedimentary Geology, 1985, 45:97-113
[181] Bhatia M R, Taylor S R. Trace-element geochemistry and sedimentary provinces: A study from the
Tasman geosyncline, Australia. Chemical Geology, 1981, 33: 115-125
[182] Blair T C, Bilodeau W L Development of tectonic cyclothems in rift, pull-apart, and foreland basins: sedimentary response to episodic tectonism. Geology, 1988,16:517-520
[183] Boynton W V. Cosmochemistry of the rare earth elements: Meterorite studies. Henderson P. Rare Earth Element Geochemistry. Development in Geochemistry. Elsevier Amsterdam, 1984, 63-107
[184] Brian W D, Peter F F. Grain size, sediment transport regime, and channel slope in alluvial rivers. The Journal of Geology, 1998, 106:661-675
[185] Brierley G J. Floodplain sedimentology of the Squamish River, British Columbia: relevance of element analysis. Sedimentology, 1991, 38:735-750
[186] Castle J W. Foreland-basin sequence response to collisional tectonism. GSA Bulletin, 2001, 113(7): 801-812
[187] Castle J W. Recogenition of facies, bounding surfaces, and stratigraphic patterns in foreland-ramp successions: An example from the upper Devonian, Appaliachian Basin, U.S.A. Journal of Sedimentary Research, 2000, 70(4): 896-912
[188] Carswell D A. Eclogites and the eclogite facies: Definition and classification. Carswell D A. Eeclogite Fcies Rocks, Oxford: Blackic and Son Ltd, 1990. 1-13
[189] Chavagnae V, Jahn B M. Coesite - bearing eclogites from the Bixiling Complex, Dabie Mountains, China: Sm-Nd agess, geo-chemical characteristics and tectonic implications. Chemical Geology. 1996, 133, 29-51.
[190] Channell J E T, Erba E, Muttoni G, et al. Early Cretaceous magnetic stratigraphy in the APTICORE drill core and adjacent outcrop at Cismon (Southern Alps, Italy), and correlation to the proposed Barremian-Aptian boundary stratotype. GSA Bulletin, 2000, 112(9): 1430-1443
[191] Chris P, Jim M, Chris E, et al. Experimental stratigraphy. GSAToday, 2001, 11(7): 4-9
[192] Chung S L, Lo C H, Li X H, et al. From mountains to basin: a Tibetan model for the post-collisional magmatic and tectonic evolution in Noah China. EOS Trans. Am. Geophys. 1997,Union 78:F649
[193] Chung S L. Trace element and isotope characteristics of Cenozoic basalts around the Tanlu Fault with implications for the eastern plate boundary between North and South China. The Journal of Geology, 1999, 107:301-312
[194] Coleman R G, Lee D E, Beatty" L B, et al. Eclogites and eclogites: their differences and similarities. Bull Geol Soc Am, 1965, 76:483-508
[195] Colombo F. Normal and reverse unroofing sequences in syntectonic conglomerates as evidence of progressive basinward deformation. Geology, 1994, 22(3): 235-238
[196] Cong B L, Zhai M, Carswell D A, et al. Petrogenesis of the ultrahigh- pressure rocks and their country rocks a.t Shuanghe in Dabieshan, central China. EuropeanJ. Mineralogy, 1995, 7: 119-138
[197] Cong B L(ed) Ultrahigh- pressure Metamorphic Rocks in the Dabieshan- Sulu Region of China. Science Pres, Beijing, China, Kluwer Academic Publishers, 1996, 224.
[198] Coussot P, Meunier M. Recognition, classification and mechnical description of debris flows. Earth Science Review, 1996, 40:209-227
[199] Cuthbert S J. Evolution of the Devonian Hornelen Basin, west Norway: new constraints from petrolgical studies of metamorphic clasts. Morton A C, et al. Developments in sedimentary provenance studies. Geological society special publication. 1991, 57:343-360
[200] David A S, Mark R H, Fleck R J, et al. Episodic caldera volcanism in the Miocene southwestern Nevada volcanic field: Revised stratigraphic framework, ~(40)Ar/~(39)Ar geochronology, and implications for magmatism and extension. GSA Bulletin, 1994, 106 (10): 1304-1318.
[201] Davies J H, Von Blanckenburg F. Slab breakoff: A model of lithosphere detachment and its test in the magmatism and deformation of collisional orogens. Earth &Planet. Sci. Let., 1995, 129, 85-93
[202] DeCelles P G, Gray M B, Ridgway K D, et al. Controls on synorogenic alluvial-fan architecture, Beartooth conglomerate (Palaeocene), Wyoming and Montana. Sedimentology, 1991, 38:567-590
[203] Dickinson W R. Plate tectonics and sedimentation. Dickinson W R. Tectonics and sedimentaion Soc Econ Paleontol Mineral Spec Publ, 1974, 22:1-27
[204] Dickinson W R. Plate tectonics and sandstone compositions. AAPG Bull, 1979, 63(12): 2164-2182
[205] Donato M M. Geochemical recognition of a captured back-arc basin metabasaltic complex, southwestern orogen. Journal of Geology, 1991, 99:711-728
[206] Eide E, McWilliarns M O, Liou J. G. ~(40)Ar/~(39)Ar geochronology and exhumation of high-pressure to ultrahigh - pressure metamorphic rocks in east China: Geology, 1994, 22:601-604
[207] Eisbacher G H. Evolution of successor basins in the Canadian Cordillera. D ott R H, Shaver R H. Modern and ancient geosynclinal sedimentation. SEPM Spec. Publ., 1974, 19:274-291
[208] Ellam R M, Hawkesworth C J. Elemental and isotopic variations in subduction related basalts: Evidence for a three component model. Contrib Mineral Petrol, 1988, 16:207-219
[209] Ernst W G, Zhou G, Liou J G, et al. High - pressure and superhigh - pressure metamorphic terranes in the Qinling- Dabie mountain belt, central China: early - to mid -Phanerozoie aecretionof the western paleo-Pacific Rim: Pacific Sci. Assoc. Inromation Bull., 1991, 43:6-15
[210] Follo M F. Conglomerates as clues to the sedimentary and tectonic evolution of a suspect terrane: Wallowa mountain oregon. Geol. Soc. Am. Bull, 1992, 104(12):1561-1576
[211] Garver J I, Scott T J. Trace elements in shales as indicators of crustal provenance and terrane accretion in the southern Canadian Cordillera. Geological Society of America Bulletin, 1995, 107(4): 440-453
[212] Gilchrist A R, Summerfield M A, Cockburn H A P. Landscape dissection, isostatic uplift and morphologic development of orogens. Geology, 1994, 22:963-966
[213] Girty G H, Hanson A D, Knaack C, et al. Provenance determined by REE, Th, and Sc analyses of metasedimentary rocks, Boyden Cave Pendant, central Sierra Nevada, California. Joumal of Sedimentary Research, 1994, B64 (1): 68-73
[214] Graham S A, Dickinson W R, Ingesoll R V. Himalayan-Bengal model for flysch dispersal in the Appaachian-Quachita system. Geol Soc Am Bull, 1975, 86:273-286
[215] Hacker B R, Ratschbacher L, Webb L, et al. What brought them up? Exhumation of the Dabie Shan ultrahigh-pressure rocks. Geology, 1995, 23:743-746
[216] Hacker B R. Mosenfelder J L, Gnos E. Rapidophiolite emplacement constrained by geochronology and thermal consideration. Tectonics, 1996, 15:1230-1247
[217] Hacker B R, Ratschbacher L, Webb L, et al. Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing. Journal of Geophysical Research, 2000, 105(B6): 13339-13364
[218] Hartley A J. Sedimentological response of an alluvial system to source area tectonism: the Seilao Member of the Late Cretaceous to Eocene Purilactis Formation of northem Chile. Marzo M, Puigdefabregas C. Alluvial sedimentation. Blackwell scientific publications, Oxford London. 1993, 489-500
[219] Hawkesworth C J, et al. Continal Basalts and Mantle Xenoliths. Nantwich: Shiva Publishing, 1983, 230-249
[220] Heller P L, Bowdler S S, Chambers H P et al. Time of initial thrusting in the Sevier orogenic belt, Idaho-Wyoming and Utah. Geology, 1986, 14:388-391
[221] Hofmann A W. Chemical differentiation of the Earth: The relationship between mantle, continental crust and oceanic crust. Earth Planet Sci Lett, 1988, 90:297-314
[222] Hyndman D W.岩浆岩和变质岩岩石学(中译本)．武汉：中国地质大学出版社，1991，192-239
[223] Jensen B A. Patterns of trace element partitioning. Geochim Cos Acta, 1973, 37:2227-2242
[224] Jordan T E, Flemings P B, Beer J A. Dating thrust-fault activity by use of foreland basin strata. Kleinspehn K L, Paola C. New perspectives in basin analysis. Springer, Berlin Heidelberg New York, 1988, 307-330
[225] King P B. The north American Cordillea. Tectonic History and mineral deposits of the western cordillera. Can. Inst. Mining and Metallurgy Special. 1966, 8:1-25
[226] Lang S C. Evolution of Devonian alluvial systems in an oblique-slip mobile zone-an example from the Broken River Province, northeastern Australia, Sedimentary Geology, 1993, 85:501-535
[227] Leake B E. Nomenclature of amphibolites. Mineral Mag., 1978, 42, 533-563
[228] Li S, Liou D, Chen Yet al. The Sm-Nd isotopic age of coesite- bearing eclogite from the southern Dabie Mountains. Chinese Science Bulletin, 1992, 37(19): 1638-1641.
[229] Li S, Chen Y, Cong B, et al. Collision of the North China and Yangtze Blocks and formation of coesitebearing eclogites: Timing and processes. Chemical Geology, 1993, 109: 70-89.
[230] Li S, Jagoutz E, Lo C H, et al. Sm/Nd, Rb/Sr, and ~40Ar/~39Ar isotopic systematics of the ultrahigh-pres-sure metamorphic rocks in the Dabie-Sulu Belt, Central China: a retrospective review. International Geology Review, 1999, 41, 1114-1124.
[231] Liou J G, Zhang R Y. Significance of ultrahigh-P talc bearing eclogitic assemblages. Mineralogical Magazine, 1995, 59, 93-102.
[232] Liou J G, Zhang R Y. Occurrence of intergranular coesite in Sulu ultrahigh-P rocks from China: Implications for fluid activity during exhumation. American Mineralogist, 1996, 81, 1217-1221.
[233] MacLean W H, Barrertt T J. Lithogeochemical techniques using immobile elements. Journal of Geochemical Exploration, 1993, 48:109-133
[234] Maruyama S, Liou J G, Zhang R. Tectonic evolution of the ultrahigh-pressure and high-pressure metamorphic belts from central China. The Island Are, 1994, 3: 112-121.
[235] Massonne H J, Schreyer W. Stability field of the high-pressure assemblage talc+phengite and two new phengite barometers. Eur. J. Miheral, 1989, 1: 391-410
[236] Maurizio A, Enrico D, Fabio T. Geochemical and mineralogical criteria for the identification of ash layers in the stratigraphic framework of a foredeep; the Early Miocene Mt. Cervarola Sandstones, northern Italy. Chemical Geology, 1997, 137(1-2): 23-39
[237] McCulloch M T, Gamble J A. Geochemical and geodynamical constraints on subduction zone magmatism. Earth Planet Set Left, 1991, 102:358-374
[238] Mclennan S M, Taylor S R. Th and U in sedimentary rocks: crustal evolution and sedimentary recycling. Nature, 1980, 285:621-624
[239] Meng Q R, Zhang G W. Geologic framework and tectonic evolution of the Qinling Orogen, central China. Tectonophysics, 2000, 323:183-196
[240] Miall A D. Architectural element analysis: a new method of facies analysis applied to fluvial deposits. Earth Science Review, 1985, 22:261-308
[241] Miall A D. Architectural elements and bounding surfaces in fluvial deposits: anatomy of the Kayenta Formation (Lower Jurassic), southwest Colorado. Sedimentary Geology, 1988, 55:233-262
[242] Miall A D. 沉积盆地分析原理(中译本)．北京：石油工业出版社．1991, 472
[243] Miall, A D. The geology of flucial deposits. Springer, Berlin Heidelberg New York, 1996, 272-273
[244] Mocek B. Geochemical evidence for arc-type volcanism in the Aegean Sea: The blueschist unit of Siphons, Cyclades (Greece). Lithos, 2001, 57:263-289
[245] Molnar P, England P. Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature, 1990, 346:29-34
[246] Nemec W, Steel R J. Fan delta: Sedimentology and tectonic settings. Blackie and Son, Glasgow, 1988, 3-13
[247] Okay A I, Seng(?)r A M C. Evidence for intracontinental thurst-related exhumation of the ultra-high-pressure rocks in China. Geology, 1992, 20:411-414
[248] Pearce J A. Role of the sub-continental lithosphere in the magma genesis at active continental margins. Hawkesworth C J, et al. Continal Basalts and Mantle Xenoliths. Nantwich: Shiva Publishing, 1983, 230-249
[249] Pearce J A, Lippard S J, Roberts S. Characteristics and tectonic significance of super-subduction ophiolites. Kokelaar B P, et al. Marginal Basin Geology. Oxford: Blackwell Scientific Publications, 1984, 77-96
[250] Pettijohn F J, Potter P E, Siever R. Sand and sandstone. Berlin: Springer-Verlag, 1972, 618
[251] Pettijohn F J. Sedimentary rocks(3rd Edn). Harper, New York, 1975, 628
[252] Posamentier H W, Allen G P. Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins. Geology, 1993, 21:455-458
[253] Ratschbacher L, Harcker B R, Webb L E, et al. Exhumation of the ultrahigh-pressure continental crust in east central China: Cretaceous and Cenozoic unroofing and the Tan-Lu fault. Journal of Geophysical Research, 2000, 105 (B6): 13303-13338
[254] Ronov B, Yaroshevskiy A A, Migdisov A A. Chemical constitution of the Earth's crust and geochemical balance of the major elements. International Geology Review, 1991, 33(10):941-1097
[255] Rumble D, Wang Q and Zhang R. Stable isotope geochemistry of marbles from the ecesite UHP terranes of Dabieshan and Sulu, China. Lithos, 2000, 52: 79-98.
[256] Rust B R. A classfication of alluvial channel systems. In: Fluvial sedimentology. In: Miall A D ed. Fluvial sedimentology. Can Soc Petrol Geol Mem 1978, 5: 187-198
[257] Salvador A. 国际地层指南：地层分类、术语和程序(第二版，中译本) 北京：地质出版社，2000，25
[258] Saunders A D, Tarney J. Geochemical characteristics of basaltic volcanism within back-arc basins. Kokelaar B P, Howells M E Marginal Basin Geology. Oxford: Blackwell Scientific Publications, 1984, 59-76.
[259] Schwarzacher W. Repetitions and cycles in Stratigraphy. Earth science reviews, 2000,50(1-2):51-75
[260] Shatsky V S, Rozmenko O A, Soboiew N V. Behaviour of rare-earth elements during high-pressure metamorphism. Lithos, 1990, 25:219-226
[261] Smith D C. Coesite in clinopyroxene in the Caledonides and its implications for geodynsmics. Nature, 1984, 310:641--644.
[262] Smith G A. Coarse grained volcaniclastic sediment: terminology and depositional process. Bull. Geol. Soc. Am. 1986, 97, 1-10
[263] Sohn Y K, Rhee C W, Kim B C. Debris flow and hyperconcentrated flood-flow deposits in an alluvial fan, northwestern part of the Cretaceous Yongdong Basin, central Korea. The Journal of Geology, 1999, 107:111-132
[264] Taylor S R, McLennan S M. The continental crust: its composition and evolution: Oxford: Blackwell Scientific Publications, 1985, 312
[265] Todd S P. Stream driven, high-density gravelly traction carpets: possible deposits in the Traberg
Conglomerate Formation, SW Ireland and some theoretical considerations on their origin. Sedimentology, 1989, 36:513-530
[266] Turner P. Continental red beds. The Netherlands: Elsevier Scientific Publishing Company, 1980, 562
[267] Tabam H, Yamauehi K, Maruyarna S, et al. Traeeing the extent of a UHP metamorphic terrane: mineralinclusion study of zircons in gneiss from the Dabieshan. Hacker, B., Liou, J. G. When Continental Collide: Geodynamics and Geochemistry of Ultrahigh-pressure Rocks, Kluwer Academic Publishers, London, 1998, 261-273.
[268] Wang Q, Cong B. Exhumation of UHP terranes: a case study from the Dabie Mountains, Eastern China. International Geology Review, 1999, 41:994-1004.
[269] Wang Q, lshiwatari A, Zhao Z, et al. Coesite-bearing granulite retrograded from eclogite in Weihai, eastern China: a preliminary study. European Journal of Mineralogy, 1993, 5:141-152.
[270] Wang Q, Xu J, Wang J, et al. The recognition of adakite-type gneisses in the North Dabie Mountain and its implication to untrahigh pressure metamorphic geology. Chinese Science Bulletin, 2000, 45(20): 1927-1933
[271] Wang X, Liou J G. 1993. Ultrahigh-pressure metamorphism of carbonate recks in the Dabie Mountains, central China. Journal of Metamorphic Geology, 11: 575-588.
[272] Wang X, Liou J G, Mao H K. Coesite-bearing eclogite from the Dabie mountains in central China. Geology, 1989, 17:1085-1088.
[273] Wang X, Liou J G. Regional ultrahigh-pressure coesite-bearing eclogitic terrane in central China: Evidence from country rocks, gnesis, marble, and metapelite. Geology, 1991, 19:933-936
[274] Whipple K X, Parker G, Paola C et al. Channel dynamics, sediment transport, and the slope of alluvial fans: experimental study. The Journal of Geology, 1998, 106:677-693
[275] Whittaker A, Cope J C W, Cowie J W, et al. A guide to stratigraphical procedure. Journal of the geological society, London, 1991, 148:813-824
[276] William C M, Charles E C, James C R, et al. Time-stratigraphic framework for the Eocene-Oligocene Mogollon-Datil volcanic field, southwest New Mexico. GSA Bulletin, 1992, 104(7): 851-871.
[277] Wood D A. The application ofa Th-Hf-Ta diagram to problems oftectonomagmatic classification and to establish the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province. Earth Planet Sci Lett, 1980, 50:11-30
[278] Woodhead D J. Geochemistry of the Mariana arc (western Pacific): source composition and processes. Chem Geol, 1989, 76:1-24
[279] Xu S, Okay A I, Ji S, et al. Diamond from the Dabie Shah metamorphic rocks and its implication for tectonic setting. Science, 1992, 256:80-82
[280] Yang J, Smith D C. Evidence for a former sanidine-coesite-eclcgite at Lanshantou, east China, and the recognition of the Chinese "Su-Lu coesite-eclogite province". Third International Eclogite Conference; Oxford, Black-Well Scientific Publications. 1989, 26
[281] Yang J, Godard G, Kiensat J R, et al. Ultrahigh-pressure (60 kbar) magnesite-bearing garnet peridotites from northeastern Jiangsu, China. J. Geology, 1993, 101: 541-554
[282] Ye K, Cong B, Ye D. The possible subducfion of continental material to depths greater than 200 lan. Nature, 2000, 407:734-736
[283] Ye K, Yao Y, Kamyama Ikuo, et al. Large areal extent of ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of East China: new implica-tions from coesite and omphacite invlusions in zircon granitic gneiss. Lithca, 2000, 52:157-164
[284] Yin A, S Nie. An indentation model for the North and South China collision and the development of the
Tan-Lu and Honsm fault system, eastern Asia. Tectonics, 1993, 12:801-803
[285] Yu T F, Rumble D, Lo C H. Unusually low? iso ultra-high-pressure metamorphic rocks from the Sulu Terrain, eastern China. Geoch. et Cosmoch. Acta, 1995, 59:2859-2864
[286] Zhang R Y, Liou J G, Cong L. Ultrahigh-pressure meta-morphosed tale-, magnesite-and Ti-clinohumite-bearing mmic-ultrarnafic complex, Dabie Mountains, east central China. Journal of Petrology, 1995, 36:1011-1038
[287] Zhang R Y, Liou J G Significance of eoeaite inclusions indolomite from eclogite in the southern Dabie mountains, China. American Mineralogist, 1996, 80:181-186
[288] Zhang Z, You Z, Han Y, et al.. Petrology, metamophie process and genesis of the Dabie-Sulu eclogite belt, east-cenral China. Acta Geologica Sirica, 1995, 69:306-325
[289] Zheng Y F, Bin F, Li Y L, et al. Oxygen and hydrogen isotope geochemistry of ultra-high-pressure eclogites from the Dabie Mountains and the Sulu terrane. Earth Planet Sei Lett, 1998, 155:113-129
[2] 安徽省区域地层编写组．华东地区地层表(安徽省分册)．北京：地质出版社．1978，181-185
[3] 安徽省地质矿产局．安徽省区域地质志．北京：地质出版社，1987，721
[4] 安徽省地质局区域地质调查队．安徽省地层志．前寒武纪分册．合肥：安徽科学技术出版社，1988，170
[5] 安徽省地质矿产局．安徽省岩石地层．武汉：中国地质大学出版社，1997，198．206
[6] 曹荣龙，朱寿华．大别山含柯石英榴辉岩区一个晚太古代的超高压变质带．地质学报，1995，69(3)：232-242
[7] 陈宣华，王小凤，张青，等．郯庐断製带形成演化的年代学研究．长春科技大学学报，2000，30(3)：215-220
[8] 陈跃志，桑宝梁．佛子岭群变质岩石学变质作用及时代的初步研究．中国区域地质，1995，14(3)：280-288
[9] 陈华成，吴其切．长江中下游地层志．合肥：安徽科学技术出版社．1989，528-529
[10] 陈江峰，董树文，邓衍尧，等．大别造山带钾氩年龄的解释—差异上升的地块．地质论评，1993，39(1)：17-22
[11] 陈江峰，谢智，刘顺生，等．大别造山带冷却年龄的 ~(40)Ar/~(39) Ar和裂变径迹测定．中国科学(B辑)，1995，25(10)：1086-1092
[12] 陈丕基．郯庐断裂巨大平移的时代与格局．科学通报，1989，34(4)：289-293
[13] 陈丕基．中国陆相侏罗-白垩系划分对比评述．地层学杂志，2000，24(2)：114-119
[14] 陈世悦．华北地块南部晚古生代至三叠纪沉积构造演化．中国矿业大学学报，2000，29(5)：536-540
[15] 程裕淇，刘敦，Williams，等．大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析．地质学报，2000，74(3)：193-205
[16] 从柏林，王清晨．大别山苏鲁超高压变质带研究的最新进展．科学通报，1999，44(11)：1127-1141
[17] 丁林．东喜马拉雅构造自上新世以来快速抬升的裂变径迹证据．科学通报，1995，40(16)：1497-1501
[18] 董树文，孙先如，张勇，等．大别山碰撞造山带基本结构．科学通报，1993，38(6)：542-545
[19] 邓晋福，叶德隆，赵海玲，等．下扬子地区火山左右深部过程与盆地形成．武汉：中国地质大学出版社，1992，184
[20] 杜建国，张鹏．大别山北部的中生代火山岩．现代地质，1999，13(1)：57-65
[21] 杜建国．大别造山带中生代岩浆作用与成矿地球化学研究．合肥工业大学博士论文，2000，176
[22] 冯宁升，丁保良．浙江白垩系古地磁研究的新认识．《第三届全国地层会议论文集》编委会．第三届全国地层会议论文集．北京：地质出版社，2000，300-303
[23] 冯增昭．下扬子地区中、下三叠统青龙群岩相古地理研究．昆明：云南科技出版社，1988，197
[24] 傅斌，郑永飞，肖益林，等．大别山苏家河地区榴辉岩和大理岩的地球化学研究．地质学报，1998，72(4)：323-338
[25] 高山，张本仁，谷晓明，等．华北与扬子板块志留-泥盆纪对接的沉积地球化学证据．中国科学(B辑)，1991，6：645-651
[26] 葛宁洁，周导之．安徽肥东群变质岩的同位素地质定年．安徽地质，1993，3(3)：22-25
[27] 管运财，高天山．等．大别山(安徽)中生代花岗岩类岩体特征与形成机制．安徽地质，1995，5(3)：19-28
[28] 金玉轩，王向东，王钥．国际地层表．地层学杂志，2003，27(2)：161
[29] 郭振宇，董火根，郭令智．大别造山带变质岩地层年龄及其构造意义．地层学杂志，1998，22(3)：185-195
[30] 韩树芬等．安徽北部中新生代沉积盆地分析．北京：地质出版社，1996，18-19
[31] 韩宗珠，袁齐林，盛兴土．安徽岳西碧溪岭榴辉岩及伴生石榴石橄榄岩的岩石学和地球化学．岩石学报，1989，4：22-33．
[32] 郝杰，刘小汉．桐柏．大别碰撞造山带大型推覆-滑脱构造及其演化．地质科学，1988，(1)：1-10
[33] 河南省地质矿产局．河南省区域地质志．北京：地质出版社，1989，772
[34] 胡克，张树业，周高志，等．鄂北榴辉岩带地质．长春地质学院学报，1989(鄂皖蓝片岩带地质专辑)，84-95
[35] 胡世玲，郝杰，李曰俊，等．大别山碧溪岭榴辉岩激光探针Ar-Ar年龄．地质科学，1999，34(4)：427-431
[36] 黄汲青．中国主要地质构造单位(英文)．地质专报甲种20号，1945，162
[37] 黄汲清，姜春发．从多旋回构造运动观点初步探讨地壳发展规律．地质学报，1962，42，2：105-152
[38] 黄杏珍，何明喜，李振西，等．中国河南省白湾盆地的白垩系特征．沉积学报，1996，14(增刊)：38-47
[39] 简平，杨巍然，李志昌，等．大别山西部熊店加里东期榴辉岩-同位素地质年代学的证据．地质学报，1997，71(2)：113—140
[40] 贾红义，刘国宏，张云银，等．合肥盆地形成机制与油气勘探前景．安徽地质，2001，11(1)：9-18
[41] 贾蓉芬，赵林，江钠言．安徽巢湖地区二叠系有机地球化学特征及其古环境意义．沉积学报，1996，14(2)：21-29
[42] 江来利，刘贻灿，吴维平，等．大别山北部漫水河灰色片麻岩的锆石U-Pb年龄及其地质意义．地球化学，2002，31(1)：66-70
[43] 姜再兴，赵澄林，熊继辉．皖中下志留统的等深岩及其地质意义．科学通报，1989，34(20)：1575-1576
[44] 金成伟，郑祥身．大别岳西地区花岗岩类岩石学及其成因．岩石学报，1998，14(4)：493-502
[45] 金福全，颜怀学，吕培基，等．北淮阳区地层研究的新进展-论北淮阳区的地层层序．合肥工业大学学报(地质论文专辑)，1987，9：3-12
[46] 晋慧娟，李育慈．西秦岭造山带中三叠统复理石相研究．沉积学报，2001，19(3)：321-326
[47] 李宝芳，马文璞，张惠良，等．大别山北麓石炭纪盆地沉积和构造研究．地学前缘，2000，7(3)：153-166
[48] 李春昱．用板块构造学说对中国部分地区构造发展的初步分析．地球物理学报，1975，18(1)：52-76
[49] 李石，王彤．桐柏山-大别山花岗岩类地球化学．武汉：中国地质大学出版社，1991，208
[50] 李曙光，Hart S R，郑双根，等．中国华北、华南陆块碰撞时代的Sm-Nd同位素年龄证据．中国科学(B辑)，1989，(3)：312—319
[51] 李曙光，孙卫东，葛宁洁，等．青岛榴辉岩相蛇绿混杂岩的岩石学证据及退变质P-T轨迹．岩石学报，1992，8(4)：351-362．
[52] 李曙光．蛇绿岩生成构造环境的Ba-Th-Nb-La判别图．岩石学报，1993，9(2)：146-157．
[53] 李任伟，江茂生，李忠，等．大别山北麓侏罗系大理岩砾石的碳-氧同位素组成及地质意义．岩石学报，1999，15(4)：623—629
[54] 李任伟，李忠，江茂生，等．合肥盆地碎屑石榴石组成及其对源区恢复和地层对比的意义．中国科学(D辑)，2000，30(增刊)：91-98
[55] 李任伟．孙枢，李忠，江茂生，金福全．奎双座．高压-超高压岩石对合肥盆地侏罗系沉积的贡献．岩石学报，2002，18(4)：526-530
[56] 李四光．新华夏海之起源．区域地质构造分析．北京：科学出版社，1974，49-58
[57] 李双应．安徽巢县南陵湖组火山碎屑流沉积物的发现．地层学杂志，1996，20(4)：277-279
[58] 李双应．安徽巢湖地区早三叠世火山碎屑流的岩石学特征及形成机理．安徽地质，2000，10(1)：24-28
[59] 李双应，李忠，王忠诚．等．胜利油区孤岛油田馆上段沉积模式研究．沉积学报，2001a，19(3)：386-393
[60] 李双应，洪天求，金福全．等．巢县二叠系栖霞组臭灰岩段异地成因碳酸盐岩．地层学杂志，2001b，25(1)：69-73
[61] 李双应，岳书仓，王道轩，等．大别造山带超高压变质岩折返隆升的地层学证据-晚侏罗世榴辉岩砾石的启示．地质论评，2002a，48(4)：345-352
[62] 李双应，岳书仓，王道轩，等．大别造山带北缘中生代地层格架厘定．地层学杂志，2002b，26(3)：178-186
[63] 李双应，王道轩，刘因，等．大别造山带北缘中生代冲积沉积体系对源区构造的沉积响应．地质通报，2002c，21(8-9)：541-546
[64] 李双应，岳书仓．安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积．沉积学报，2002d，20(1)：7-12
[65] 李双应，李任伟，岳书仓，等．大别造山带北缘石炭系胡油坊组砾石特征及其构造意义．地层学杂志，2003a，27(2)：116-121
[66] 李双应，岳书仓，王道轩，等．大别造山带北缘中生代地层中榴辉岩砾石地球化学特征及构造意义．地球化学，2003b，32(5)：436-444
[67] 李双应，岳书仓，杨建，等．皖北新元古代刘老砷组页岩的地球化学特征及其地质意义．地质科学，2003c，38(2)：241-253
[68] 李阳，李双应，岳书仓，等．胜利油用孤岛油区馆陶组上段沉积结构单元．地质科学，2002，37(2)：219-230
[69] 李耀西，汪迎平，丁保良．中国东南部白垩系综合地层学研究的新进展．地质学报，2001，75(4)：451-458
[70] 李勇，王成善，曾允孚．造山作用与沉积响应．矿物岩石，2000，20(2)：49-56
[71] 李忠，李任伟，孙枢，等．合肥盆地南部侏罗系砂岩碎屑组分及其物源构造属性．岩石学报，1999，15(3)：438-445
[72] 李忠，孙枢，李任伟，等．合肥盆地中生代充填序列及共对大别山造山作用的指示．中国科学(D辑)，2000，30(3)：256-263
[73] 李忠，李任伟，孙枢，等．大别地块北缘侏罗系花岗岩类砾石的Rb-Sr年代学特征．科学通报，2001，46(7)：582-585
[74] 刘宝珺．沉积岩石学．北京：地质出版社，1980，497
[75] 刘护军．秦岭新生代构造隆升研究．陕西师范大学学报(自然科学版)，2002，30(1)：121-124
[76] 刘景波，游振东，钟增球．豫南鄂北大别山中部和北部的榴辉岩类．中国科学(D辑)，1996，26(3)：277-281
[77] 刘少峰，张国伟，张宗清，等．合肥盐地花岗岩砾石的同位素年代学示踪．科学通报，2001，46(9)：748-753
[78] 刘晓春．大别山榴辉岩的成因-原岩属性提供的证据．安徽地质，1992，2(4)：24-34．
[79] 刘晓春，胡克，李学燮，等．大别-苏鲁高压变质带中榴辉岩的多样性及其成因．地质论评，1994，40(6)：494—501
[80] 刘贻灿，徐树桐等．佛子岭群的岩石化学及构造环境．安徽地质，1996，6(2)：1-6．
[81] 刘贻灿，徐树桐，李曙光，等．大别山北部榴辉岩的地球化学特征和Sr，Nd同位素组成及其大地构造意义．中国科学(D辑)，2000，30(增刊)：99—107
[82] 刘志刚，富云莲，牛宝贵，等．大别山北坡苏家河群及原信阳群龟山组变基性杂岩 ~(40)Ar-~(39)测年及其地质意义．科学通报，1993，38(13)：1214-1218
[83] 陆光森，金福全，王道轩．河南固始杨山组底砾岩中早古生代化石的新发现及其意义．合肥工业大学学报(地质论文专辑)，1987：13-19
[84] 陆光森，金福全，五道轩．河南商城胡油坊组中Protomonocarina(原单脊叶肢介)的发现及其重要意义．合肥工业大学学报(地质论文专辑)，1987，9：20-24
[85] 陆镜元．大别山东段佛子岭(片岩系)群的时代．地质论评，1963，21(1)：155-161
[86] 马昌前，杨坤光，许长海，等．大别山中生代钾质岩浆作用与超高压变质地体的剥露机理．岩石学报，1999，15(3)：379-395
[87] 马文璞，王关玉，王果胜．佛子岭岩群中的晋宁期深成岩带及其构造意义．地质论评，2000，47(5)：476-482
[88] 潘国强，吴海权．大别山碰撞造山带后缘的火山作用．李兆鼎，王碧香．火山岩、火山作用及有关矿产．北京：地质出版社，1993，45-51
[89] 潘国强，陆现彩，于航波．北淮阳中生代adakite岩石地球化学特征及成因讨论．岩石学报，2001，17(4)：541-550
[90] 任纪舜，张正坤．论秦岭造山带．秦岭造山带学术讨论会论文选集．1991，99-109
[91] 任润生．合肥盆地周公山群中火山岩砾石的发现及意义．华东地质，1979，3，27-31
[92] 孙勇．东秦岭古洋盆与加里东运动．地质论评，1991，37(6)：555-559
[93] 桑宝梁．陈跃志，邵桂清．大别山东南麓宿松群铷-锶年龄及其构造意义．中国区域地质，1987，4：364-370
[94] 桑隆康，王人镜，张泽明，等．九资河-天堂寨地区燕山晚期花岗岩与大别造山带核部隆升．地质学报，2000，74(3)：234—246
[95] 索书田，钟增球，游振东，等．大别-苏鲁超高压和高压变质带碰撞后韧性伸展构造框架．安徽地质，2000，10(3)：212—215
[96] 沈渭洲，凌洪飞，王德滋，等．浙江省中生代火成岩的Nd-Sr同位素研究．地质科学，1999，34(2)：223-232
[97] 苏育民．大别山北麓变质岩的时代问题．地质论评，1960，20(6)：258-261
[98] 汤加富，孙先如，候明金，等．安徽大别山-张八岭地区新的构造格局与非板块碰撞造山过程．安徽地质，1995，5(1)：1-12．
[99] 陶铨，徐明才，袁晓儒，等．鄂东北前寒武纪地层地质年代研究．中国地质科学院天津地质研究所所刊，1986，16：75-89
[100] 万天丰，朱鸿，赵磊，等．郯庐断裂带的形成与演化综述．现代地质，1996，10(2)：159-168
[101] 王道轩，李双应，刘因，等．六安小华山周公山组火山碎屑岩的发现及意义．安徽地质，2000，10(4)，248—251
[102] 王道轩，金福今，谢宪德，等．合肥盆地三尖铺组 ~(40)Ar-~(39)Ar同位素年代地层学研究．地层学杂志，2000，24(3)：236—242
[103] 王道轩，刘因，李双应，等．大别超高压变质岩折返至地表的时间下限：大别山北麓晚侏罗世砾岩中发现榴辉岩砾石．科学通报，2001，46(14)：1216-1220
[104] 王强，许继锋，赵振华，等．大别山燕山期亏损重稀十元素花岗岩类的成因及动力学意义．岩石学报，2001，17(4)：551-564
[105] 王清晨，张儒瑗，从柏林，等．鲁东-苏北榴辉岩的构造特征及其折返机制．岩石学报，1992，8(2)：153-160．
[106] 王清晨，从柏林，马力．大别山造山带与合肥盆地的构造偶合．科学通报，1997，42(6)：575-580
[107] 王清晨，从柏林．大别山超高压变质带的大地构造框架．岩石学报，1998，14(4)：481-492
[108] 王清晨．中国超高压变质岩十五年研究进展．地球学报，2001，22(1)：11-16
[109] 王式光，谭绪荣，赵云龙．苏北榴辉岩的稀土元素地球化学及其成因讨论．地质论评，1995，41(5)：401-408
[110] 王随继，任明达．根据河道形态和沉积物特征的河流新分类．沉积学报，1999，17(2)：240-246
[111] 王晓燕，崔文元，刘树忠，等．豫南地区含柯石英榴辉岩的发现．岩石学报，1993，9(2)：181-185．
[112] 王蓉，沈后．合肥盆地侏罗-白垩系界线附近的孢粉组合．地球科学进展学术讨论会编辑委员会．地球科学进展-学术讨论会论文摘要．武汉，中国地质大学出版社，1992，78-79
[113] 王岳军，范蔚，郭锋．北淮阳晚中生代火山岩定年及火山砾石地球化学：对大别灰色片麻岩隆升和中生代地层格架的约束．科学通报，2002，47(20)：1528-1534
[114] 王中刚，于学元，赵振华．稀土元素地球化学．北京：科学出版社，1989，535
[115] 魏春景，单振刚，张立飞，等．1997．北大别榴辉岩的确立及其地质意义．科学通报，42(17)：1832-1836
[116] 吴根耀．造山带地层学．成都：四川科学技术出版社，2000，98-101
[117] 吴浩若．放射虫硅质岩对华南古地理的启示．古地理学报，1999，1(2)：28-35
[118] 吴利仁，徐贵忠．东秦岭-大别山碰撞造山带的地质演化．北京：科学出版社，1998，177-183
[119] 吴元保，陈道公，Deloule，E．等．北大别片麻岩的锆石 U-Pb离子探针测定及其地质意义．地质论评，2001，47(3)：239-244
[120] 夏邦栋，李培军．中国东部扬子板块同华北板块在中．晚三叠世拼接的沉积学证据．沉积学报，1996，14(1)：12-20
[121] 肖庆辉，李晓波，贾跃明，等．当代造山带研究中值得重视的若干前沿问题．地学前缘，1995,2(1-2)：43-50
[122] 薛爱民，金维浚，袁学诚．大别山北缘合肥盆地中、新生代构造演化．高校地质学报，1999，5(2)：157-163
[123] 徐辉．华北地区石炭二叠系陆源物质及来源分析．石油实验地质，1987，9(1)：57-64
[124] 徐嘉炜．初论大别山碰撞带．合肥工业大学学报，1981，3：82-94
[125] 徐嘉炜，朱光，吕培基，等．郯庐断裂带平移年代学研究的进展．安徽地质，1995，5(1)：1-12．
[126] 徐树桐，江来利，刘贻灿，等．大别山区(安徽部分)的构造格局和演化过程．地质学报，1992，66(1)：1-14
[127] 徐树桐，刘贻灿，江来利，等．大别山的构造格局和演化．北京：科学出版社，1994，34—60
[128] 徐树桐，刘贻灿，吴维平，等．大别山造山带研究的主要进展及存在问题．自然科学进展，2001，11(8)：796-803
[129] 许志琴．扬子板块北缘的大型深层滑脱构造及动力学分析．中国区域地质，1987，6(4)：289-300
[130] 颜怀学，金福全，吕培基，等．关于中国南北板块在北淮阳地区界线的探讨．石油天然气地质，1988，9(2)：125-132
[131] 杨坤光，马昌前，简平，等．大别山北缘两次俯冲(碰撞)的岩石学和构造学证据．中国科学(D辑)，2000，30(4)：364-372
[132] 杨巍然，王国灿，简平．大别造山带构造年代学．武汉：中国地质大学出版社，2000，68-128
[133] 杨巍然，王国灿，李长安．造山带中、新生代隆升作用构造年代学研究新进展．地质科技情报，1999，19(4)：19-22
[134] 杨为民，杨有根．北淮阳地区的中生界．安徽地质，1995，5(4)：11-17
[135] 杨志坚．佛子岭群的地质时代问题．地质论评，1964，22(5)：327-336
[136] 杨志坚．试论桐柏-大别山地质构造演化特征．地质学报，1982，56(2)：123-135
[137] 杨祝良，沈加林，沈渭洲，等．大别山北缘中生代火山-侵入岩锶-钕同位素组成特征及其物质来源．岩石矿物学杂志，2002，22(3)：223-230
[138] 杨祝良，沈加林，沈渭洲，等．北淮阳中生代火山-侵入岩同位素年代学研究．．地质论评，1999，45(增刊)：674-680
[139] 叶凯，徐平．山东荣城大疃榴辉岩成因岩石学研究．岩石学报，1992，8(1)：27-39
[140] 叶大年，李达周，董光福，等．河南信阳变质带的3T型多硅白云母和C型榴辉岩．科学通报，1979，5：217-220
[141] 伊海生，王成善，李亚林，等．构造事件的沉积响应．沉积与特提斯地质，2001，21(2)：1-15
[142] 俞云文，徐步台．浙江中生代晚期火山-沉积岩系层序和时代．地层学杂志，1999，23(2)：136-145
[143] 于在平，孙勇，张成立．秦岭尚丹缝合带变质砂岩地球化学特征及构造环境探讨．地质论评，1991，37(6)：492-507
[144] 游振东，索书田，钟增球，等．大别山超高压变质岩的退变质显微构造：折返过程的启示．地质学报，2000，74(3)：224—233
[145] 翟明国，从柏林．苏鲁-大别山变质带岩石大地构造学．中国科学(D辑)，1996，26(30：258～264
[146] 张国栋，朱静昌，仇福康，等．早、中三叠世下扬子海沉积盆地研究．地质学报，1989，63(2)：134-146
[147] 张国伟，孟庆任，于在平，等．秦岭造山带的造山过程及其动力学特征．中国科学(D辑)，1996，26(3)：193-208
[148] 张建珍，杜建国，张友联，等．大别山榴辉岩岩石学及地球化学特征．地质论评，1998，44(3)：255-263
[149] 张鹏，北淮阳东段几组铷锶等时线年龄及其区域地质意义．中国区域地质，1996，15(4)：304-310
[150] 张鹏．北淮阳东段变花岗岩的锆石U-Pb年龄及地层意义．安徽地质，1999，9(2)：90-93
[151] 张希道，陈允福，王桂枝．鲁东南莒南县一带榴辉岩的特征．岩石学报，1992，8(1)：40-49．
[152] 张旗，简平，刘敦一，等．宁芜火山岩的锆石SHRIMP定年及其意义．中国科学(D辑)2003，33(4)：309-314
[153] 张旗，马宝林，刘若新，等．一个消减带之上的大陆岩石圈地幔残片-安徽饶拨寨超镁铁岩的地球化学特征．中国科学，1995，25(8)：967-973
[154] 张儒媛，从柏林，刘忠光．苏鲁超高压变质地体及其成因研究．岩石学报，1993a，9(3)：211-225
[155] 张儒嫒，刘忠光，王小民，等．中国中部河南省榴辉岩中柯石英的发现及冀其构造意义．岩石学报，1993b，9(2)：186-191．
[156] 张希道，陈允福，王桂枝．鲁东南莒南县一带榴辉岩的特征．岩石学报，1992，8(1)：40-49
[157] 张一勇，李建国．江苏白垩纪孢粉组合序列．地层学杂志，2000，24(1)：65-71
[158] 张勇，江来利，刘贻灿．大别山超高压榴辉岩带榴辉岩的特征和变质作用．岩石学报，1991，3：1-13．
[159] 张泽明，游振东，韩郁箐，等．大别-苏鲁榴辉岩带的岩石学、变质作用过程及成因研究．地质学报，1995，69(4)：306-325
[160] 赵宗举，杨树锋，陈汉林，等．合肥盆地基底构造属性．地质科学，2000，35(3)：288-296
[161] 郑文武．大别山东段“佛子岭群”的划分和时代问题．地质论评，1964，22(5)：337-347
[162] 郑祥身，金成伟，翟明国，等．1999．北大別灰色片麻岩的岩石化学特征及大地构造背景．岩石学报，15(3)：350-358
[163] 《中国地层典》编委会．中国地层典-侏罗系．北京：地质出版社．2000，24-26
[164] 《中国地层典》编委会．中国地层典-白垩系．北京：地质出版社．2000，11-21
[165] 钟大赉，丁林．青藏高原隆升过程及其机制探讨．中国科学(D辑)，1996，26(4)：289-295
[166] 周鼎武，董云鹏，华洪，等．“磨拉石建造”和“不整合”在地层对比中的意义．地质论评，1996，42(5)：416-423
[167] 周汉文，李献华，刘颖．南大别花凉亭榴辉岩退变质作用过程的元素地球化学变异．地球化学，1997，26(5)：25-33
[168] 周存亭，高天山，汤加富，等．安徽大别山北部榴辉岩的分布及主要特征．中国区域地质，2000，19(3)：253-257
[169] 周存亭，汤加富，等．大别山地区片麻岩套的建立与成岩时代讨论．安徽地质，1995，5(3)：29-40．
[170] 周泰祕，陈江峰，李学明，等．安徽霍舒正长岩带侵入体的Ar-Ar法同位素地质年龄．安徽地质，1992，2(1)：4-11
[171] 周祖翼，许长海，Reiners P. W等．大别山天堂寨晚白垩世以来剥露历史的(U-Th)／He和裂变径迹分析证据．科学通报，2003，48(6)：599-602
[172] 朱光，宋传中，王道轩，等．郯庐断裂带走滑时代的 ~(40)Ar/~(39)Ar年代学研究及其构造意义．中国科学(D辑)，2001，31(3)：250-256
[173] 朱洪发，秦德余，刘翠章．论华南孤峰组和大隆组硅质岩成因、分布规律及其构造机制．石油实验地质，1989，11(4)：341-348
[174] 朱夏，徐旺．中国中新生代沉积盆地．北京：石油工业出版社，1990，319
[175] Ames L, Tilton G R, Zhou G.Timing of collision of the Sino- Korean and Yangtze cratons: U - Pb zircon dating of coesite -bearing edogites: Geology, 1993, 21: 339-342.
[176] Baker J A, Matthews M D, Rowley D, et al. Fluid- rock interactions during ultra - high pressure metamor-phism, Dabie Shan, China. Geochimica et Cosmochimica Acta, 1997, 61:1685-1696
[177] Behrensmeyer A k, Tauxe L. lsochronous fluvial systems in Miocene deposits of northern Pakistan. Sedimentaology, 1982, 29:331-352
[178] Bhatia M R. Plate tectonics and geochemical composition of sandstones. Journal of Geology, 1983, 91(6): 611-627
[179] Bhatia M R, Crook K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology, 1986, 92:181-193
[180] Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks: Province and tectonic control. Sedimentary Geology, 1985, 45:97-113
[181] Bhatia M R, Taylor S R. Trace-element geochemistry and sedimentary provinces: A study from the
Tasman geosyncline, Australia. Chemical Geology, 1981, 33: 115-125
[182] Blair T C, Bilodeau W L Development of tectonic cyclothems in rift, pull-apart, and foreland basins: sedimentary response to episodic tectonism. Geology, 1988,16:517-520
[183] Boynton W V. Cosmochemistry of the rare earth elements: Meterorite studies. Henderson P. Rare Earth Element Geochemistry. Development in Geochemistry. Elsevier Amsterdam, 1984, 63-107
[184] Brian W D, Peter F F. Grain size, sediment transport regime, and channel slope in alluvial rivers. The Journal of Geology, 1998, 106:661-675
[185] Brierley G J. Floodplain sedimentology of the Squamish River, British Columbia: relevance of element analysis. Sedimentology, 1991, 38:735-750
[186] Castle J W. Foreland-basin sequence response to collisional tectonism. GSA Bulletin, 2001, 113(7): 801-812
[187] Castle J W. Recogenition of facies, bounding surfaces, and stratigraphic patterns in foreland-ramp successions: An example from the upper Devonian, Appaliachian Basin, U.S.A. Journal of Sedimentary Research, 2000, 70(4): 896-912
[188] Carswell D A. Eclogites and the eclogite facies: Definition and classification. Carswell D A. Eeclogite Fcies Rocks, Oxford: Blackic and Son Ltd, 1990. 1-13
[189] Chavagnae V, Jahn B M. Coesite - bearing eclogites from the Bixiling Complex, Dabie Mountains, China: Sm-Nd agess, geo-chemical characteristics and tectonic implications. Chemical Geology. 1996, 133, 29-51.
[190] Channell J E T, Erba E, Muttoni G, et al. Early Cretaceous magnetic stratigraphy in the APTICORE drill core and adjacent outcrop at Cismon (Southern Alps, Italy), and correlation to the proposed Barremian-Aptian boundary stratotype. GSA Bulletin, 2000, 112(9): 1430-1443
[191] Chris P, Jim M, Chris E, et al. Experimental stratigraphy. GSAToday, 2001, 11(7): 4-9
[192] Chung S L, Lo C H, Li X H, et al. From mountains to basin: a Tibetan model for the post-collisional magmatic and tectonic evolution in Noah China. EOS Trans. Am. Geophys. 1997,Union 78:F649
[193] Chung S L. Trace element and isotope characteristics of Cenozoic basalts around the Tanlu Fault with implications for the eastern plate boundary between North and South China. The Journal of Geology, 1999, 107:301-312
[194] Coleman R G, Lee D E, Beatty" L B, et al. Eclogites and eclogites: their differences and similarities. Bull Geol Soc Am, 1965, 76:483-508
[195] Colombo F. Normal and reverse unroofing sequences in syntectonic conglomerates as evidence of progressive basinward deformation. Geology, 1994, 22(3): 235-238
[196] Cong B L, Zhai M, Carswell D A, et al. Petrogenesis of the ultrahigh- pressure rocks and their country rocks a.t Shuanghe in Dabieshan, central China. EuropeanJ. Mineralogy, 1995, 7: 119-138
[197] Cong B L(ed) Ultrahigh- pressure Metamorphic Rocks in the Dabieshan- Sulu Region of China. Science Pres, Beijing, China, Kluwer Academic Publishers, 1996, 224.
[198] Coussot P, Meunier M. Recognition, classification and mechnical description of debris flows. Earth Science Review, 1996, 40:209-227
[199] Cuthbert S J. Evolution of the Devonian Hornelen Basin, west Norway: new constraints from petrolgical studies of metamorphic clasts. Morton A C, et al. Developments in sedimentary provenance studies. Geological society special publication. 1991, 57:343-360
[200] David A S, Mark R H, Fleck R J, et al. Episodic caldera volcanism in the Miocene southwestern Nevada volcanic field: Revised stratigraphic framework, ~(40)Ar/~(39)Ar geochronology, and implications for magmatism and extension. GSA Bulletin, 1994, 106 (10): 1304-1318.
[201] Davies J H, Von Blanckenburg F. Slab breakoff: A model of lithosphere detachment and its test in the magmatism and deformation of collisional orogens. Earth &Planet. Sci. Let., 1995, 129, 85-93
[202] DeCelles P G, Gray M B, Ridgway K D, et al. Controls on synorogenic alluvial-fan architecture, Beartooth conglomerate (Palaeocene), Wyoming and Montana. Sedimentology, 1991, 38:567-590
[203] Dickinson W R. Plate tectonics and sedimentation. Dickinson W R. Tectonics and sedimentaion Soc Econ Paleontol Mineral Spec Publ, 1974, 22:1-27
[204] Dickinson W R. Plate tectonics and sandstone compositions. AAPG Bull, 1979, 63(12): 2164-2182
[205] Donato M M. Geochemical recognition of a captured back-arc basin metabasaltic complex, southwestern orogen. Journal of Geology, 1991, 99:711-728
[206] Eide E, McWilliarns M O, Liou J. G. ~(40)Ar/~(39)Ar geochronology and exhumation of high-pressure to ultrahigh - pressure metamorphic rocks in east China: Geology, 1994, 22:601-604
[207] Eisbacher G H. Evolution of successor basins in the Canadian Cordillera. D ott R H, Shaver R H. Modern and ancient geosynclinal sedimentation. SEPM Spec. Publ., 1974, 19:274-291
[208] Ellam R M, Hawkesworth C J. Elemental and isotopic variations in subduction related basalts: Evidence for a three component model. Contrib Mineral Petrol, 1988, 16:207-219
[209] Ernst W G, Zhou G, Liou J G, et al. High - pressure and superhigh - pressure metamorphic terranes in the Qinling- Dabie mountain belt, central China: early - to mid -Phanerozoie aecretionof the western paleo-Pacific Rim: Pacific Sci. Assoc. Inromation Bull., 1991, 43:6-15
[210] Follo M F. Conglomerates as clues to the sedimentary and tectonic evolution of a suspect terrane: Wallowa mountain oregon. Geol. Soc. Am. Bull, 1992, 104(12):1561-1576
[211] Garver J I, Scott T J. Trace elements in shales as indicators of crustal provenance and terrane accretion in the southern Canadian Cordillera. Geological Society of America Bulletin, 1995, 107(4): 440-453
[212] Gilchrist A R, Summerfield M A, Cockburn H A P. Landscape dissection, isostatic uplift and morphologic development of orogens. Geology, 1994, 22:963-966
[213] Girty G H, Hanson A D, Knaack C, et al. Provenance determined by REE, Th, and Sc analyses of metasedimentary rocks, Boyden Cave Pendant, central Sierra Nevada, California. Joumal of Sedimentary Research, 1994, B64 (1): 68-73
[214] Graham S A, Dickinson W R, Ingesoll R V. Himalayan-Bengal model for flysch dispersal in the Appaachian-Quachita system. Geol Soc Am Bull, 1975, 86:273-286
[215] Hacker B R, Ratschbacher L, Webb L, et al. What brought them up? Exhumation of the Dabie Shan ultrahigh-pressure rocks. Geology, 1995, 23:743-746
[216] Hacker B R. Mosenfelder J L, Gnos E. Rapidophiolite emplacement constrained by geochronology and thermal consideration. Tectonics, 1996, 15:1230-1247
[217] Hacker B R, Ratschbacher L, Webb L, et al. Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing. Journal of Geophysical Research, 2000, 105(B6): 13339-13364
[218] Hartley A J. Sedimentological response of an alluvial system to source area tectonism: the Seilao Member of the Late Cretaceous to Eocene Purilactis Formation of northem Chile. Marzo M, Puigdefabregas C. Alluvial sedimentation. Blackwell scientific publications, Oxford London. 1993, 489-500
[219] Hawkesworth C J, et al. Continal Basalts and Mantle Xenoliths. Nantwich: Shiva Publishing, 1983, 230-249
[220] Heller P L, Bowdler S S, Chambers H P et al. Time of initial thrusting in the Sevier orogenic belt, Idaho-Wyoming and Utah. Geology, 1986, 14:388-391
[221] Hofmann A W. Chemical differentiation of the Earth: The relationship between mantle, continental crust and oceanic crust. Earth Planet Sci Lett, 1988, 90:297-314
[222] Hyndman D W.岩浆岩和变质岩岩石学(中译本)．武汉：中国地质大学出版社，1991，192-239
[223] Jensen B A. Patterns of trace element partitioning. Geochim Cos Acta, 1973, 37:2227-2242
[224] Jordan T E, Flemings P B, Beer J A. Dating thrust-fault activity by use of foreland basin strata. Kleinspehn K L, Paola C. New perspectives in basin analysis. Springer, Berlin Heidelberg New York, 1988, 307-330
[225] King P B. The north American Cordillea. Tectonic History and mineral deposits of the western cordillera. Can. Inst. Mining and Metallurgy Special. 1966, 8:1-25
[226] Lang S C. Evolution of Devonian alluvial systems in an oblique-slip mobile zone-an example from the Broken River Province, northeastern Australia, Sedimentary Geology, 1993, 85:501-535
[227] Leake B E. Nomenclature of amphibolites. Mineral Mag., 1978, 42, 533-563
[228] Li S, Liou D, Chen Yet al. The Sm-Nd isotopic age of coesite- bearing eclogite from the southern Dabie Mountains. Chinese Science Bulletin, 1992, 37(19): 1638-1641.
[229] Li S, Chen Y, Cong B, et al. Collision of the North China and Yangtze Blocks and formation of coesitebearing eclogites: Timing and processes. Chemical Geology, 1993, 109: 70-89.
[230] Li S, Jagoutz E, Lo C H, et al. Sm/Nd, Rb/Sr, and ~40Ar/~39Ar isotopic systematics of the ultrahigh-pres-sure metamorphic rocks in the Dabie-Sulu Belt, Central China: a retrospective review. International Geology Review, 1999, 41, 1114-1124.
[231] Liou J G, Zhang R Y. Significance of ultrahigh-P talc bearing eclogitic assemblages. Mineralogical Magazine, 1995, 59, 93-102.
[232] Liou J G, Zhang R Y. Occurrence of intergranular coesite in Sulu ultrahigh-P rocks from China: Implications for fluid activity during exhumation. American Mineralogist, 1996, 81, 1217-1221.
[233] MacLean W H, Barrertt T J. Lithogeochemical techniques using immobile elements. Journal of Geochemical Exploration, 1993, 48:109-133
[234] Maruyama S, Liou J G, Zhang R. Tectonic evolution of the ultrahigh-pressure and high-pressure metamorphic belts from central China. The Island Are, 1994, 3: 112-121.
[235] Massonne H J, Schreyer W. Stability field of the high-pressure assemblage talc+phengite and two new phengite barometers. Eur. J. Miheral, 1989, 1: 391-410
[236] Maurizio A, Enrico D, Fabio T. Geochemical and mineralogical criteria for the identification of ash layers in the stratigraphic framework of a foredeep; the Early Miocene Mt. Cervarola Sandstones, northern Italy. Chemical Geology, 1997, 137(1-2): 23-39
[237] McCulloch M T, Gamble J A. Geochemical and geodynamical constraints on subduction zone magmatism. Earth Planet Set Left, 1991, 102:358-374
[238] Mclennan S M, Taylor S R. Th and U in sedimentary rocks: crustal evolution and sedimentary recycling. Nature, 1980, 285:621-624
[239] Meng Q R, Zhang G W. Geologic framework and tectonic evolution of the Qinling Orogen, central China. Tectonophysics, 2000, 323:183-196
[240] Miall A D. Architectural element analysis: a new method of facies analysis applied to fluvial deposits. Earth Science Review, 1985, 22:261-308
[241] Miall A D. Architectural elements and bounding surfaces in fluvial deposits: anatomy of the Kayenta Formation (Lower Jurassic), southwest Colorado. Sedimentary Geology, 1988, 55:233-262
[242] Miall A D. 沉积盆地分析原理(中译本)．北京：石油工业出版社．1991, 472
[243] Miall, A D. The geology of flucial deposits. Springer, Berlin Heidelberg New York, 1996, 272-273
[244] Mocek B. Geochemical evidence for arc-type volcanism in the Aegean Sea: The blueschist unit of Siphons, Cyclades (Greece). Lithos, 2001, 57:263-289
[245] Molnar P, England P. Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature, 1990, 346:29-34
[246] Nemec W, Steel R J. Fan delta: Sedimentology and tectonic settings. Blackie and Son, Glasgow, 1988, 3-13
[247] Okay A I, Seng(?)r A M C. Evidence for intracontinental thurst-related exhumation of the ultra-high-pressure rocks in China. Geology, 1992, 20:411-414
[248] Pearce J A. Role of the sub-continental lithosphere in the magma genesis at active continental margins. Hawkesworth C J, et al. Continal Basalts and Mantle Xenoliths. Nantwich: Shiva Publishing, 1983, 230-249
[249] Pearce J A, Lippard S J, Roberts S. Characteristics and tectonic significance of super-subduction ophiolites. Kokelaar B P, et al. Marginal Basin Geology. Oxford: Blackwell Scientific Publications, 1984, 77-96
[250] Pettijohn F J, Potter P E, Siever R. Sand and sandstone. Berlin: Springer-Verlag, 1972, 618
[251] Pettijohn F J. Sedimentary rocks(3rd Edn). Harper, New York, 1975, 628
[252] Posamentier H W, Allen G P. Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins. Geology, 1993, 21:455-458
[253] Ratschbacher L, Harcker B R, Webb L E, et al. Exhumation of the ultrahigh-pressure continental crust in east central China: Cretaceous and Cenozoic unroofing and the Tan-Lu fault. Journal of Geophysical Research, 2000, 105 (B6): 13303-13338
[254] Ronov B, Yaroshevskiy A A, Migdisov A A. Chemical constitution of the Earth's crust and geochemical balance of the major elements. International Geology Review, 1991, 33(10):941-1097
[255] Rumble D, Wang Q and Zhang R. Stable isotope geochemistry of marbles from the ecesite UHP terranes of Dabieshan and Sulu, China. Lithos, 2000, 52: 79-98.
[256] Rust B R. A classfication of alluvial channel systems. In: Fluvial sedimentology. In: Miall A D ed. Fluvial sedimentology. Can Soc Petrol Geol Mem 1978, 5: 187-198
[257] Salvador A. 国际地层指南：地层分类、术语和程序(第二版，中译本) 北京：地质出版社，2000，25
[258] Saunders A D, Tarney J. Geochemical characteristics of basaltic volcanism within back-arc basins. Kokelaar B P, Howells M E Marginal Basin Geology. Oxford: Blackwell Scientific Publications, 1984, 59-76.
[259] Schwarzacher W. Repetitions and cycles in Stratigraphy. Earth science reviews, 2000,50(1-2):51-75
[260] Shatsky V S, Rozmenko O A, Soboiew N V. Behaviour of rare-earth elements during high-pressure metamorphism. Lithos, 1990, 25:219-226
[261] Smith D C. Coesite in clinopyroxene in the Caledonides and its implications for geodynsmics. Nature, 1984, 310:641--644.
[262] Smith G A. Coarse grained volcaniclastic sediment: terminology and depositional process. Bull. Geol. Soc. Am. 1986, 97, 1-10
[263] Sohn Y K, Rhee C W, Kim B C. Debris flow and hyperconcentrated flood-flow deposits in an alluvial fan, northwestern part of the Cretaceous Yongdong Basin, central Korea. The Journal of Geology, 1999, 107:111-132
[264] Taylor S R, McLennan S M. The continental crust: its composition and evolution: Oxford: Blackwell Scientific Publications, 1985, 312
[265] Todd S P. Stream driven, high-density gravelly traction carpets: possible deposits in the Traberg
Conglomerate Formation, SW Ireland and some theoretical considerations on their origin. Sedimentology, 1989, 36:513-530
[266] Turner P. Continental red beds. The Netherlands: Elsevier Scientific Publishing Company, 1980, 562
[267] Tabam H, Yamauehi K, Maruyarna S, et al. Traeeing the extent of a UHP metamorphic terrane: mineralinclusion study of zircons in gneiss from the Dabieshan. Hacker, B., Liou, J. G. When Continental Collide: Geodynamics and Geochemistry of Ultrahigh-pressure Rocks, Kluwer Academic Publishers, London, 1998, 261-273.
[268] Wang Q, Cong B. Exhumation of UHP terranes: a case study from the Dabie Mountains, Eastern China. International Geology Review, 1999, 41:994-1004.
[269] Wang Q, lshiwatari A, Zhao Z, et al. Coesite-bearing granulite retrograded from eclogite in Weihai, eastern China: a preliminary study. European Journal of Mineralogy, 1993, 5:141-152.
[270] Wang Q, Xu J, Wang J, et al. The recognition of adakite-type gneisses in the North Dabie Mountain and its implication to untrahigh pressure metamorphic geology. Chinese Science Bulletin, 2000, 45(20): 1927-1933
[271] Wang X, Liou J G. 1993. Ultrahigh-pressure metamorphism of carbonate recks in the Dabie Mountains, central China. Journal of Metamorphic Geology, 11: 575-588.
[272] Wang X, Liou J G, Mao H K. Coesite-bearing eclogite from the Dabie mountains in central China. Geology, 1989, 17:1085-1088.
[273] Wang X, Liou J G. Regional ultrahigh-pressure coesite-bearing eclogitic terrane in central China: Evidence from country rocks, gnesis, marble, and metapelite. Geology, 1991, 19:933-936
[274] Whipple K X, Parker G, Paola C et al. Channel dynamics, sediment transport, and the slope of alluvial fans: experimental study. The Journal of Geology, 1998, 106:677-693
[275] Whittaker A, Cope J C W, Cowie J W, et al. A guide to stratigraphical procedure. Journal of the geological society, London, 1991, 148:813-824
[276] William C M, Charles E C, James C R, et al. Time-stratigraphic framework for the Eocene-Oligocene Mogollon-Datil volcanic field, southwest New Mexico. GSA Bulletin, 1992, 104(7): 851-871.
[277] Wood D A. The application ofa Th-Hf-Ta diagram to problems oftectonomagmatic classification and to establish the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province. Earth Planet Sci Lett, 1980, 50:11-30
[278] Woodhead D J. Geochemistry of the Mariana arc (western Pacific): source composition and processes. Chem Geol, 1989, 76:1-24
[279] Xu S, Okay A I, Ji S, et al. Diamond from the Dabie Shah metamorphic rocks and its implication for tectonic setting. Science, 1992, 256:80-82
[280] Yang J, Smith D C. Evidence for a former sanidine-coesite-eclcgite at Lanshantou, east China, and the recognition of the Chinese "Su-Lu coesite-eclogite province". Third International Eclogite Conference; Oxford, Black-Well Scientific Publications. 1989, 26
[281] Yang J, Godard G, Kiensat J R, et al. Ultrahigh-pressure (60 kbar) magnesite-bearing garnet peridotites from northeastern Jiangsu, China. J. Geology, 1993, 101: 541-554
[282] Ye K, Cong B, Ye D. The possible subducfion of continental material to depths greater than 200 lan. Nature, 2000, 407:734-736
[283] Ye K, Yao Y, Kamyama Ikuo, et al. Large areal extent of ultrahigh-pressure metamorphism in the Sulu ultrahigh-pressure terrane of East China: new implica-tions from coesite and omphacite invlusions in zircon granitic gneiss. Lithca, 2000, 52:157-164
[284] Yin A, S Nie. An indentation model for the North and South China collision and the development of the
Tan-Lu and Honsm fault system, eastern Asia. Tectonics, 1993, 12:801-803
[285] Yu T F, Rumble D, Lo C H. Unusually low? iso ultra-high-pressure metamorphic rocks from the Sulu Terrain, eastern China. Geoch. et Cosmoch. Acta, 1995, 59:2859-2864
[286] Zhang R Y, Liou J G, Cong L. Ultrahigh-pressure meta-morphosed tale-, magnesite-and Ti-clinohumite-bearing mmic-ultrarnafic complex, Dabie Mountains, east central China. Journal of Petrology, 1995, 36:1011-1038
[287] Zhang R Y, Liou J G Significance of eoeaite inclusions indolomite from eclogite in the southern Dabie mountains, China. American Mineralogist, 1996, 80:181-186
[288] Zhang Z, You Z, Han Y, et al.. Petrology, metamophie process and genesis of the Dabie-Sulu eclogite belt, east-cenral China. Acta Geologica Sirica, 1995, 69:306-325
[289] Zheng Y F, Bin F, Li Y L, et al. Oxygen and hydrogen isotope geochemistry of ultra-high-pressure eclogites from the Dabie Mountains and the Sulu terrane. Earth Planet Sei Lett, 1998, 155:113-129
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