新疆哈密地区矿产资源成矿规律及评价研究
|
摘要
哈密地区地层分布齐全、沉积建造多样、地质构造复杂、岩浆活动频繁、变形变质作用明显,成矿地质条件优越,形成了区内多种类型的矿产资源远景区。本区主体属中亚成矿域,是研究大陆成矿作用的典型地区;同时,也是全球古生代多旋回造山带的典型地区之一。哈密地区目前已知矿点和已发现矿床达680多处,基础地质和矿产勘查工作有一定的基础,但以往工作侧重于某些区块或某些基础地质问题,对全地区性的成矿规律的综合性研究还较为薄弱,影响到矿产勘查部署与开发的长远规划。为此,开展哈密地区成矿规律的研究,不但有助于深化对成矿作用的认识,而且有助于为地质找矿工作提供理论指导。
哈密地区是新疆对外开放“东出西进”的门户,被称为“欧亚大陆桥”的中哈铁路横贯本区,交通位置上,扼新疆与内地交通的要冲,是新疆乃至全国重要的黑色金属、有色金属、贵金属和煤炭资源的重要基地,是新疆东部最重要的经济区。因此,开展地区性矿产资源的评价研究,对于地方经济发展具有现实意义。
本文在对哈密地区各类矿床开展野外地质调查的基础上,充分整理、吸收消化前人大量研究成果,运用矿床成矿系列的理论,对哈密地区四维成矿规律进行了综合分析、研究;比较系统地阐明了哈密地区的地质构造格局及矿产资源的基本特征,划分了成矿区带,对各区带的地质特征、成矿规律进行了总结。结合日常工作,参加编制了哈密地区地质矿产图;
在典型矿床研究方面,选择前寒武纪的池西铁铜矿床和天湖铁矿、古生代的葫芦和黄山东等铜镍硫化物矿床、中生代的小红山铁矿和镜儿泉的伟晶岩型稀有金属矿床等代表性矿床进行了重点调研,其中池西和小红山属于本次工作新发现的矿产地。经过初步评价,池西铁铜矿中铁的最高品位可达62%以上,铜品位最高可达1.7%,Au最高可达5.89g/t;小红山铁矿铁的最高品位可达60%以上。
利用Re-Os法测定了葫芦铜镍硫化物矿床的成矿年龄为283Ma,利用40Ar-39Ar法测定了镜儿泉伟晶岩型稀有金属矿床的成矿年龄为243Ma,丰富了成矿系列与成矿规律的研究,进一步讨论了地壳演化与成矿作用的演化轨迹,建立了重要矿床的区域成矿模式。
在成矿规律和成矿系列研究的基础上,对哈密地区的大型矿集区进行了预测评价,提出了进一步勘查与研究的建议,为地区矿产资源规划提供了依据。
文中指出,哈密的特征性矿产资源主要是黑色金属、有色金属矿床可以形成于加里东期、海西期、印支期和燕山期等不同时代;同时也指出了在中新生代岩浆活动区寻找黑色金属和贵金属矿床以及在前寒武系分布区寻找铁、铜、铅锌矿床的可能性。这些规律及其它成矿规律的揭示丰富了区域成矿学的内容,深化了对于哈密地区成矿规律的理性认识,对该区今后地质矿产勘查具有重要的指导意义。
MinerogeneTic series of ore deposits is related to the research on the mineralizaTion rule in the four-dimensional space, the evoluTion of metallogenic Time, space and substance during the earth development and their distribuTion rule. MinerogeneTic series study can increase the cogniTion of global substance rule, effecTively guide the ore prospecTing, and speed the exploraTion of mineral resources.
Hami area is the significant producing area of ferrous metal, nonferrous metal, noble metal and coal resources in Xinjiang, even in the whole China, and also one of the typical mulTi-cycle orogen belts. In Hami area, at present, there have been discovered more than 680 ore spots and ore deposits. Although there have certain fundamental geology and mineral exploraTion been done, the previous work emphasized parTicularly on some regions or some fundamental geological problems and weakened the syntheTic research on the regional metallogenic rule, so it influenced the long-range programming of mineral exploraTion and exploitaTion. therefor, based on the field geological research into each type of ore deposits in Hami area, and fully coordinaTing and assimilaTing the abundant previous research fruits, the author has selected some key ore deposits for further dissecTion under the help of lithology and isotope chronology. through the research on Hami regional tectonic evoluTion and its ore-control effecTion, and on regional magmaTic acTivity and heat evoluTion history and its ore-control effecTion, and especially on minerogeneTic series and metallogenic rule, this paper has relaTively and systemaTically clarified the pattern of geological structure in Hami area and the evoluTion locus of the crustal evoluTion and mineralizaTion, and also tried to apply the minerogeneTic series theory to further understand the space-Time distribuTion and evoluTion lineage of mineral resources in Hami area. Since the author has raTionally compartmentalized the minerogeneTic series, systemaTically concluded the metallogenic rule, established the regional metallogenic model and further summarized the metallogenic rule in Hami area more systemaTically and integratedly, this paper can provide the theory reference for strategical target opTimality of mineral concentraTion regions, and propose the programming on the metallogenic prognosis and mineral exploraTion.
According to the recent new fruits about the isotope chronology and inert gases isotope geochemistry, this paper has systemaTically established the minerogeneTic series and subseries of ore deposits in Hami area, and discussed the geological and geochemical feature of the minerogeneTic series and subseries of each type of ore deposits and their genesis. Moreover, it has also discussed the relaTionship between the evoluTion history of minerogeneTic series of ore deposits and the development history of orogen belts, and set up the metallogenic lineage and rule in Hami area, especially during the Hercynian cycle. In this paper, it’s pointed out that the characterisTic minerals in Hami mainly are ferrous metal and nonferrous metal, whose deposits formed during Caledonian epoch, Hercynian epoch, Indo-Sinian epoch and Yanshan epoch. then it also points that it’s very possible to prospect the ferrous and noble metal deposits in the Cenozoic and Mesozoic magmaTic acTive regions, and the iron and copper-lead-zinc deposits in the Precambrian distribuTion regions. the study on these rules and the metallogenic rules enriches the content of regional metallogeny, and deepenes the raTional cogniTion on the metallogenic rule in Hami area, and plays an important role in guiding the geological mineral work by theory.
哈密地区是新疆对外开放“东出西进”的门户,被称为“欧亚大陆桥”的中哈铁路横贯本区,交通位置上,扼新疆与内地交通的要冲,是新疆乃至全国重要的黑色金属、有色金属、贵金属和煤炭资源的重要基地,是新疆东部最重要的经济区。因此,开展地区性矿产资源的评价研究,对于地方经济发展具有现实意义。
本文在对哈密地区各类矿床开展野外地质调查的基础上,充分整理、吸收消化前人大量研究成果,运用矿床成矿系列的理论,对哈密地区四维成矿规律进行了综合分析、研究;比较系统地阐明了哈密地区的地质构造格局及矿产资源的基本特征,划分了成矿区带,对各区带的地质特征、成矿规律进行了总结。结合日常工作,参加编制了哈密地区地质矿产图;
在典型矿床研究方面,选择前寒武纪的池西铁铜矿床和天湖铁矿、古生代的葫芦和黄山东等铜镍硫化物矿床、中生代的小红山铁矿和镜儿泉的伟晶岩型稀有金属矿床等代表性矿床进行了重点调研,其中池西和小红山属于本次工作新发现的矿产地。经过初步评价,池西铁铜矿中铁的最高品位可达62%以上,铜品位最高可达1.7%,Au最高可达5.89g/t;小红山铁矿铁的最高品位可达60%以上。
利用Re-Os法测定了葫芦铜镍硫化物矿床的成矿年龄为283Ma,利用40Ar-39Ar法测定了镜儿泉伟晶岩型稀有金属矿床的成矿年龄为243Ma,丰富了成矿系列与成矿规律的研究,进一步讨论了地壳演化与成矿作用的演化轨迹,建立了重要矿床的区域成矿模式。
在成矿规律和成矿系列研究的基础上,对哈密地区的大型矿集区进行了预测评价,提出了进一步勘查与研究的建议,为地区矿产资源规划提供了依据。
文中指出,哈密的特征性矿产资源主要是黑色金属、有色金属矿床可以形成于加里东期、海西期、印支期和燕山期等不同时代;同时也指出了在中新生代岩浆活动区寻找黑色金属和贵金属矿床以及在前寒武系分布区寻找铁、铜、铅锌矿床的可能性。这些规律及其它成矿规律的揭示丰富了区域成矿学的内容,深化了对于哈密地区成矿规律的理性认识,对该区今后地质矿产勘查具有重要的指导意义。
MinerogeneTic series of ore deposits is related to the research on the mineralizaTion rule in the four-dimensional space, the evoluTion of metallogenic Time, space and substance during the earth development and their distribuTion rule. MinerogeneTic series study can increase the cogniTion of global substance rule, effecTively guide the ore prospecTing, and speed the exploraTion of mineral resources.
Hami area is the significant producing area of ferrous metal, nonferrous metal, noble metal and coal resources in Xinjiang, even in the whole China, and also one of the typical mulTi-cycle orogen belts. In Hami area, at present, there have been discovered more than 680 ore spots and ore deposits. Although there have certain fundamental geology and mineral exploraTion been done, the previous work emphasized parTicularly on some regions or some fundamental geological problems and weakened the syntheTic research on the regional metallogenic rule, so it influenced the long-range programming of mineral exploraTion and exploitaTion. therefor, based on the field geological research into each type of ore deposits in Hami area, and fully coordinaTing and assimilaTing the abundant previous research fruits, the author has selected some key ore deposits for further dissecTion under the help of lithology and isotope chronology. through the research on Hami regional tectonic evoluTion and its ore-control effecTion, and on regional magmaTic acTivity and heat evoluTion history and its ore-control effecTion, and especially on minerogeneTic series and metallogenic rule, this paper has relaTively and systemaTically clarified the pattern of geological structure in Hami area and the evoluTion locus of the crustal evoluTion and mineralizaTion, and also tried to apply the minerogeneTic series theory to further understand the space-Time distribuTion and evoluTion lineage of mineral resources in Hami area. Since the author has raTionally compartmentalized the minerogeneTic series, systemaTically concluded the metallogenic rule, established the regional metallogenic model and further summarized the metallogenic rule in Hami area more systemaTically and integratedly, this paper can provide the theory reference for strategical target opTimality of mineral concentraTion regions, and propose the programming on the metallogenic prognosis and mineral exploraTion.
According to the recent new fruits about the isotope chronology and inert gases isotope geochemistry, this paper has systemaTically established the minerogeneTic series and subseries of ore deposits in Hami area, and discussed the geological and geochemical feature of the minerogeneTic series and subseries of each type of ore deposits and their genesis. Moreover, it has also discussed the relaTionship between the evoluTion history of minerogeneTic series of ore deposits and the development history of orogen belts, and set up the metallogenic lineage and rule in Hami area, especially during the Hercynian cycle. In this paper, it’s pointed out that the characterisTic minerals in Hami mainly are ferrous metal and nonferrous metal, whose deposits formed during Caledonian epoch, Hercynian epoch, Indo-Sinian epoch and Yanshan epoch. then it also points that it’s very possible to prospect the ferrous and noble metal deposits in the Cenozoic and Mesozoic magmaTic acTive regions, and the iron and copper-lead-zinc deposits in the Precambrian distribuTion regions. the study on these rules and the metallogenic rules enriches the content of regional metallogeny, and deepenes the raTional cogniTion on the metallogenic rule in Hami area, and plays an important role in guiding the geological mineral work by theory.
引文
1.程裕淇,陈毓川,赵一鸣,初论矿床的成矿系列问题,中国地质科学院院报,1979,总第 1 号,32-58
2.马天林,杨建民,孙立倩等.土屋铜矿成矿过程与东天山矿产分布.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 129-131
3. 马瑞士,舒良树,孙家齐.东天山构造演化与成矿作.1997.北京:地质出版社,202P.
4. 毛景文,宋叔和,陈毓川.桂北地区成岩系列和锡多金属矿床成矿系列.北京:北京科学技术地质出版社,1988, P 196
5. 毛景文,杨建民,韩春明等.东天山金铜成矿系统和成矿动力学研究.地球科学,2002
6.毛景文,华仁民,李晓波.浅议大规模成矿作用与大型矿集区.矿床地质,1999, 18(4):291-299.
7. 王之田,秦克章.中国铜矿床类型、成矿环境及其时、空分布特点地质学报,1988,62 (3):257-267
8 毛景文,张招崇,任丰寿等.北祁连西段金属矿床时分布规律与成矿环境.地质学报,1999. 73(1):73-82.
9. 陈毓川,毛景文,王平安.桂北地区矿床成矿系列和成矿历史演化轨迹.广西:科学技术出版社,1995
10. 陈毓川,毛景文,王平安.桂北地区矿床成矿系列和成矿多旋回性.第五届全国矿床会议论文集,北京:地质出版社,91-93
11.陈毓川,王登红,林文蔚.中国岩金矿床成矿系列.矿床地质[J] , 1998 增刊:87-92
12.陈毓川,黄民智,徐压等.大厂锡石一硫化物多金属矿带地质特征及成矿系列.地质学报,1985, 59 (3): 228-240
13 陈毓川,裴荣富,宋天锐等,中国矿床成矿系列.第五届全国矿床会议论文集.北京:地质出版社,1993, 89-91
14.陈毓川,裴荣富,宋天锐等,中国矿床成矿系列初论.北京二地质出版社,1998, P 104
15 王元龙,成守德.新疆大地构造四个阶段的演化及其基本特征.见陈海乱等主编,中国碰撞造山带研究.1999,北京:地质出版社,122131.
16 王元龙.成矿系列研究及其应用.新疆地质,1993, 11(4) :332-338
17.王作勋,乌牡继易,吕喜超等.天山多旋回演化与成矿.北京:科学技术出版社,1990,83-130
18.王登红,陈毓川,李红阳等.新疆阿尔泰造山带成矿规律成矿系列研究进展.地质论评,1998, 44(1):62
19.王福同,玛京,胡建卫等.新疆土屋大型斑岩铜矿床特征及发现意义.中国地质,2001 年 1 月,第 28 卷 1 期,36-39.
20.王福同,庄道泽,胡建卫等.物探在新疆土屋地区铜矿床找矿中的应用.中国地质,2001,28 (3):40-X16.
21 车自成,刘洪福,刘良.中大山造山带的形成与演化.北京:地质出版社,1994, 135P
22.邓万明,壳一慢过渡带及其在岩石圈构造演化中的地质意义,科学通报,1997, 42 (23):2474-24820
23. 王龙生,丙宗瑶.超大型斑岩型铜矿形成的必要条件.第六届全国矿床会议论文集北京:地质出版社,1998 , 15-18.
24.叶庆同,石桂华,川一锦华等.怒江、澜仓 l1. ,金沙江地区铅锌矿床成矿特征和成矿系列,北京:科学技术出版社,161p
25.田培仁.新疆北部主要矿产成矿区带划分新疆地质,1994, 12 (1 ): 67-74
26 田培仁.新疆北部主要矿产成矿规律.新疆地质,1994, 12 ( 1): 83-87
27.白云来.新疆东部梧桐窝子群的大地构造背景及其地球化学论证.新疆地质,1994,12(2):106-114
28.王登红,陈毓川.阿尔泰成矿省的成矿系列及成矿规律.北京,原子能出版社.2002,16-410
29 王登红,陈毓川.与海相火山作用有关的铁-铜-铅-锌矿床系列类型及成因初探.矿床地质, 2001, 20 (1)
30.陈毓川,刘德权等.2006 新疆国家紧缺矿产大型矿集区预测评价研究报告.305 项目专题研究报告.代号: 2003BA612A-06-07-18A
31.胡旺亮等.东准噶尔成矿区成矿条件与矿产资源评价研究.305 项目专题研究报告.代号:85-902-03
32.刘德权,唐延龄,周汝洪,中亚古生代造山带成矿作用基本特征.西北地质,2001, 34(2):1-10
33.刘德权,唐延龄,周汝洪,新疆斑岩铜矿的成矿条件和远景新疆地质,2001, 19 (1):43-18.
34.刘德权,唐延龄,周汝洪.中国新疆矿床系列类型.矿床地质,1996. 15 (3 ): 207215.
35.刘德权,唐延龄,周汝洪.新疆北部古生代地壳演化及成矿系列.矿床地质,1992. 11(4):307314.
36.孙宝生.中国天山东部矿床组合和矿床分布模式的大地构造意义.第五届全国矿床会议论文集,1993,北京:地质出版社,68-70
37.毛景文,杨建民等.东天山铜金成矿地质背景和成矿过程研究.2002.国土资源大调查项目研究报告:编号:DKD9902001
38. 成守德,李耀增,王元龙.新疆矿产资源成矿特征与分布规律.矿床地质,1993, 12 (1) : 1-9
39. 朱裕生.论矿床成矿模式.地质论评,1993,39 (3):216-222
40.李华芹,陈富文.2004.中国新疆区域成矿作用年代学.北京:地质出版社,59-83,103-169
41.李锦轶,肖序常,汤耀庆等.新疆北部金属矿产与板块构造.新疆地质,1992, 10 ( 2 ):138-146
42.祁思敬,李英,南秦岭晚古生带海底喷气-沉积成矿系统,地学前缘,1999 6(1)171 一 180
43.何国琦,刘德权,李茂松等.中国新疆古生代地壳演化及成矿.乌鲁木齐:新疆人民出版社,1994
44 何国琦,刘德权,李茂松等新疆土要造山带地壳发展的五阶段模式及成矿系列,新疆地质,1995 年 2 期
45.宋天锐.沉积成矿系列研究的新进展.地质论评,42 (4):357-- 363
46.宋叔和.中国一些主要金属矿床类型及其时空分布规律.矿床地质,1991, 10 (1) :10---18
47.张文淮,成矿流体与成矿机制,地学前缘,1996, 3 (4 ): 245-2520
48.张连昌,曾章仁,杨兴科等,康古尔韧性剪切带型金矿构造地球化学特征.贵金属地质, 1997,6: 13-21.
49.张德润.新疆东部地区大地构造问题探讨.新疆地质,1990, 18 (2) :99-106
50.杨兴科,程宏宾,姬金生等.东天山金铜成矿背景与成矿系统分析.西安工程学院学报,2000, 22 (2):7-14
51.杨兴科,姬金生,张连昌.东天山金矿带区域成矿规律解析.矿床地质,1998 17(增刊):131-134.
52.杨树德.浅议古板块构造的划分原则.新疆地质,新疆地质,1994, 12 (1): 175-179
53.杨树德.新疆北部的古板块构造.新疆地质,新疆地质,1994, 12 (1): 1-8
54.肖序常,汤耀庆,冯益民等.新疆北部及邻区大地构造.北京:地质出版社,1992, 169p
55.芮宗瑶,王龙生,王义大,东大山大地构造格局与成矿动力学探讨.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 3-4
56.芮宗瑶,王龙生,王义天等,东天山土屋和延东斑岩铜矿床时代讨论,矿床地质,2002,21(1):16-22.
57.芮宗瑶,王福同,李恒海.新疆东大山斑岩铜矿带的新进展.中国地质,2001.第 28 卷 2 期,1623.
58.芮宗瑶,刘玉琳,王龙生等,新疆东天山斑岩铜矿带及其大地构造格局.地质学报,2002,76(1):83-93.
59.陈从喜,蔡克勤.矿床成矿系列的若干问题与方向-兼论非金属矿床成矿系列研究的有关问题.地质论评,1998,44 (6) : 596-602
60.陈文明.论东天山土屋一延东铜矿的容矿岩.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 65-67
61.陈陶成.新疆哈密黄山一镜儿泉铜镍矿带成矿地质背景及矿例介绍.西北地质,1990,1:20-250
62.陈毓川矿床成矿系列.地学前缘,1994, 1 (3) :90-94
63.陈毓川主编,中国矿床成矿系列图(附说明书 ).北京:地质出版社,1999
64.郎智君,师波,李大德.新疆二岔口铜矿一戍因探讨.新疆地质,1992, 10(3): 244-252
65.姜立丰,李凤鸣,姬厚贵等,哈密县 885-846 高地 1: 50000 区调报告,1994, 138--151
66.姜立丰,姬厚贵,郑勇.新疆东天山区域构造演化与矿产资源潜力分析.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 73-77
67.姬金生,杨兴科,屈文军.东天山觉罗塔格金、铜成矿带成矿规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 10-1
68.姬金生,李华琴,张连昌等,东天山康古尔金矿磁铁矿绿泥石建造年代学.科学通报,1999(5),439-442
69.姬金生等,东天山康古尔塔格金矿带地质与成矿.北京:地质出版社,1999 , 1-20.
70.桑少杰.东天山地球动力学演化与成矿,东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 78-87
71.涂光炽.初议中亚成矿域地质科学,1990, 34 (4) : 397-404
72.秦克章,方同辉,王书来等,吐哈盆地南缘古生代“天窗”卡拉塔格铜金矿化区的发现及其成矿潜力.中国地质,2001年 3 月,28 (3):16-23
73.秦克章,方同辉,王书来等.东天山古生代板块构造分区、演化与成矿规律研究及勘查应用.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议, 2001,68-72
74.秦克章,孙枢,陈海泄.新疆北部金属矿床时空分布格局-古生代多岛海型碰撞造山带的标志.中国碰撞造山带研究.1999.北京:地质出版社,183-196.
75.秦克章,汪东坡,王之田.中国东部铜矿床类型、成矿集中区与成矿系统.矿床地质,1999. 18(4):359-371.
76.秦克章.新疆中亚型造山带与成矿作用.中国科学院地质与地球物理研究所,2000, 71-157.
77.恩环金川铜镍硫化物矿床成矿模式和成矿系列.地质论评,32 (3) : 276-286
78.郭召杰,马瑞士,郭令智等.新疆东部三条蛇绿棍杂岩带的比较研究.地质论评,1993,139 (3):236-247
79.郭召杰,马瑞士.东天山晚古生代康古尔弧间盆地研究.南京大学学报(地球科学), 1990 (3):103-113
80.贾跃明,流体成矿系统与成矿作用研究,地学前缘,1996, 3 (4): 253-2580
81.车自成, 刘洪福, 刘良. 中天山造山带的形成与演化. 北京:地质出版社, 1994, 135P
82.胡霭琴等. 1985. 天山东段中天山隆起带前寒武纪变质岩系时代及演化—据 U-Pb 年代学研究. 地球化学, 10(3): 285-290
83. 胡受奚,郭继春,顾连兴,周顺之,严正富,杨浩,王金珠,刘延东,1990,加里东造山带在东天山(E85°-95°)构造格架中的重要地位及其地质特征,新疆地质科学(第 1 辑), 32-46
84.姬金生,杨兴科,刘光海,觉罗塔格金、铜成矿带成矿系列分布规律研究与矿床定位预测.新疆国家 305 项目办公室内部报告,2000.
85.李华芹,谢才富,常海亮. 新疆北部有色金属贵金属矿床成矿作用年代学[M]. 北京:地质出版社,1998,202—220.
86. 李锦轶, 肖序常, 汤耀庆等. 新疆北部金属矿产与板块构造. 新疆地质,1992,10(2):138—146
87. Huang t K. On Major tectonic Forms of China., Ser. A, No.20, 165pp., 8pls. (with Chinese summary of 11pages)
88.Windley B F, Allen M B, Zhang C, Zhao Z Y, and Wang G R. 1990. Paleozoic accreTion and Cenozoic redeformaTion of Chinese Tien Shan rang, central Asia. Geology, 18: 128-131
89.马瑞士, 舒良树, 孙家齐. 1997. 东天山构造演化与成矿. 地质出版社, 北京
90.马瑞士, 王赐银, 叶尚夫等. 1993. 东天山构造格架及地壳演化
91.姬金生,陶洪祥,曾章仁,杨兴科,张连昌等. 1994. 东天山康古尔塔格金矿带地质与成矿. 北京:地质出版社
92.李锦轶. 1991. 试论新疆东准噶尔古生代板块构造演化. 见: 肖序常和汤耀庆主编, 古中亚复合巨型缝合带南缘构造演化, 北京: 北京科学技术出版社, 92-108
93.李先梓,李行等. 新疆铂族元素成矿地质条件及找矿方向.中国地质科学院西安地质矿产研究所所刊,1991,第 33号.
94.刘德权,唐延龄,周汝洪. 中国新疆矿床系列类型. 矿床地质,1996.15(3):207 2 15.
95.马瑞士,叶尚夫,王赐银等.东天山造山带构造格架与演化.新疆地质科学,1990(2):21-36
96. 秦克章,孙枢,陈海泓.新疆北部金属矿床时空分布格局—古生代多岛海型碰撞造山带的标志[C]. 见陈海泓主编,中国碰撞造山带研究. 1999.北京:地质出版社,183-196
97.秦克章. 新疆北部中亚型造山与成矿作用.中国科学院地质与地球物理研究所博士后研究工作报告,2000.
98.毛景文,杨建民,屈文俊,杜安道,韩春明,王志良. 新疆黄山东铜镍硫化物矿床 Re-Os 同位素测定及其地球动力学意义. 矿床地质,2002b,21(4):323-330
99.芮宗瑶,王龙生,王义天等,东天山土屋和延东斑岩铜矿床时代讨论[J],矿床地质,2002,21(1):16—22.
100.王润民,刘德权,印静泰等.新疆哈密土墩-黄山一带铜镍硫化物矿床成矿控制条件及找矿方向的研究.矿物岩石,1987(1):31-34.
101.阎文元,天山东段早石炭世岛弧火山岩特征及其矿产.新疆地质,1985,3(2):49-58
102.周济元、茅燕石、黄志勋、何大伦、王道永、消渊甫. 东天山古大陆边缘火山地质.成都:成都科技大学出版社,1994.
103.徐兴旺,马天林,孙立倩,李贵书,张学勤,徐湘康,吴继修.新疆东天山罗觉塔格韧性挤压带基本特征及动力学意义.地质科学,1998,33(2):147-156.
104.张良臣. 1995. 中国新疆板块构造与动力学特征. 见: 新疆第三届天山地质矿产学术讨论会论文选辑. 乌鲁木齐: 新疆人民出版社, 1-14
105.李锦轶,王克卓,李文铅等.东天山地区构造格架.DKD9902002 研究报告,2002
106.梁月明, 黄旭钊, 徐昆, 于学政, 王越胜, 张文志, 蔡玉梅. 2001. 新疆康古尔塔格断裂带地球物理场及深部地质特征. 中国区域地质, 20(4): 398-403
107.汪振文. 1986. 天山东部及北山区域磁场特征与深部地质构造的初步分析. 新疆地质, 4(3): 107-114
108.汪振文. 1987. 天山东部及北山区域布格重力异常特征与矿产分布关系的探讨,新疆地质,5(2): 68-75
109.王学求,迟清华,程志中等.新疆荒漠戈壁区深穿透地球化学调查与研究.内部研究报告,2001
110.刘德权,唐延龄,周汝洪. 新疆北部古生代地壳演化及成矿系列. 矿床地质,1992. 11(4):307 314.
111.陈哲夫, 梁云海. 新疆天山地质构造几个问题的探讨. 新疆地质, 1985, 3(2):1-13
112.张良臣, 吴乃元. 1985. 天山地质构造及发展史. 新疆地质, 3(3): 1-14
113.舒良树,夏飞雅克,马瑞士,1998,中天山北缘大型右旋走滑韧剪带研究,新疆地质,16/4 总 60,326-336
114.车自成, 刘洪福, 刘良. 中天山造山带的形成与演化. 北京:地质出版社, 1994, 135P
115.李锦轶. 1991. 试论新疆东准噶尔古生代板块构造演化. 见: 肖序常和汤耀庆主编, 古中亚复合巨型缝合带南缘构造演化, 北京: 北京科学技术出版社, 92-108
116.姜常义,穆艳梅,赵晓宁,白开寅,张虹波. 2001. 塔里木板块北缘活动陆缘型侵入岩带的岩石学与地球化学. 中国区域地质, 20(2):158-163
117.李锦轶, 肖序常, 汤耀庆等. 新疆北部金属矿产与板块构造. 新疆地质,1992,10(2):138—146
118.李先梓,李行等. 新疆铂族元素成矿地质条件及找矿方向.中国地质科学院西安地质矿产研究所所刊,1991,第 33号.
119.马瑞士, 叶尚夫, 王赐银. 1990. 东天山造山带构造格架和演化. 新疆地质科学, 第二辑, 21-36. 北京: 地质出版社
120.王鸿祯等,中国地理图集,1987
121.王作勋,邬继易,吕喜朝,张经国,刘成德,1990,天山多旋回构造演化及成矿. 北京: 科学出版社
122.徐兴旺,马天林,孙立倩,李贵书,张学勤,徐湘康,吴继修.新疆东天山罗觉塔格韧性挤压带基本特征及动力学意义.地质科学,1998,33(2):147-156.
123.汪振文. 1988. 中国天山区域地球物理特征及深部地壳构造,新疆地质,6(2): 29-34
124.舒良树,夏飞雅克,马瑞士,1998,中天山北缘大型右旋走滑韧剪带研究,新疆地质,16/4 总 60,326-336
125.陶维屏.中国非金属矿床的成矿系列.地质学报,1989, 63 (4) : 324-337
126.顾连兴,褚强,胡受奚.新疆卡拉麦里一哈尔里克碱性花岗岩带地质特征及成因.新疆地质科学,1990 年 2 期,47-55
127.高常林,崔可锐,钱一雄等.天山微板块与塔里木盆地.北京:地质出版社,1995, 284p
128.崔彬,成矿空间初探.地质与勘探,1999, No.3
129.崔彬.江西九瑞地区铜金成矿系列模式.矿床地质,1998, 14 (1) : 44-50
130 崔彬等.物质场-能量场-空间场综合成矿预测.现代地质,No4
131.章崇真.略论华南中生代花岗岩成矿系列.矿床地质,1983 (1) : 38-46
132.黄明渊.黄山东铜镍矿床地球化学特征及靶区优选.新疆地质,1990, 8 (2) :142-152
133.程裕淇,陈毓川,赵一鸣等,再论矿床的成矿系列问题,中国地质科学院院报,1983,总第 6 号,1-64
134.程裕淇,陈毓川,赵一鸣等,再论矿床的成矿系列问题-兼论中生代某些矿床的成矿系列,地质论评,1983, 29 (2), 127-139
135.韩发,Sedex 型矿床成矿系统,地学前缘,1999, 6 (1) 139--162
136.韩宝福,何国琦,王式光等,新疆北部后碰撞慢源岩浆活动与陆壳纵向生长.地质论评,44 (4):396-406
137.韩春明,毛景文,杨建民等.东天山晚古生代内生金属矿床成矿系列和成矿规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 65-67
138.翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999 } 1-288.
139.翟裕生,邓军,崔彬等.成矿系统及综合地质异常.现代地质,13 (1) : 99-103.
140.翟裕生,张湖等,大型构造与大型矿床,北京:地质出版社,1997, 173-180
141.翟裕生,姚书振,林新多.长江中下游地区铁、铜等成矿规律研究矿床地质,1992,11(1):1-12
142.翟裕生,姚书振,林新多.长江中下游地区铁铜矿床类型、形成条件和成矿演化.地球科学:地质出版社,1983, No.4
143.翟裕生,姚书振,崔彬等.成矿系列研究.武汉:中国地质大学出版社,1996, 198p
144.翟裕生.成矿系列研究问题.现代地质,1992, 6 (3):301-307
145.翟裕生.成矿系统及其演化初步实践到理论思考.地球科学,25 (4):333-339
146.翟裕生.论成矿系统.地学前缘,1999, 6 (1):13-27
147.翟裕生等.关于成矿一系列和成矿模式问题.矿床学参考书(下册).北京:地质出版社,1987:214-218
148.裴荣富,洪大伟.碰撞造山与华南花岗岩及其成矿系列研究的新进展矿床地质,1990,14(4):329-334.
149.裴荣富,邱小平,尹冰川,成矿作用爆发异常及巨量金属堆积.矿床地质,1999, 18 (4):331-340.
150.薛春纪,陈毓川,姬金生等.东天山矿床成矿系列和分布规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 60-62
151.Benning L G,Hydrosuphide complexing of gold in hydrothermal soluTion from 150℃to 5000C and 500 to 1500 bars Geochim Cosmochim Acta,1996,60:1849-1877.
152. Miler A R. High salinity in sea water. Nature, 1964, 203:590-594.
153. Ague J J, Joost L M, Van Haren. Assesing metamomTic mass and volume changes using boottrap with applicaTion to deep crustral hydrothermal alteraTion of marmble RrOnnmic GP}ln}v_199fi_91·llfi9-1189_
154.Allen M B, Windley B F and Zhang C. 1992. Paleozoic collisional tectonics and magmaTism of the Chinese Tien Shan, central Asia. tectonophysics, 220, 89-115
155.Baker A J and Fallick A E. 1989. Evidence from Lewisian limestones for isotopically heavy carbon in two-thousand-million-year-old sea water. Nature, 337: 352-354.
156.Banks D A, Yardley B W D, Campbell A R, et al. 1994. REE composiTion of an aqueous magmaTic fluid: a fluid inclusions study from the Capitan Pluton, New Mexico, U S A[J]. Chemical Geology, 113: 259-272.
157.Barley M E ,Groves D I. 1992. SuperconTinent Cycles and the distribuTion of metal deposit through Time. Geology, 20:291-294
158.Barnicocat A C, Fare R J, Groves D L, et al. 1991. Synmetamorphic lode-gold deposits in high-grade Archaean setTing[J]. Geology, 19: 921-924.
159.Baumgartner L P,Olsen S N. 1996. A least-squares approach to mass transport calculaTion using the isocon method. Economic Geology, 91:1169-1182.
160.Benning L G. 1996. Hydrosuphide complexing of gold in hydrothermal soluTion from 150℃to 500℃ and 500 to 1500 bars Geochim Cosmochim Acta, 60:1849-1877.
161.Bonnemaison M. 1991. “Filons de aurifere ”an cas parTiculiar de shear aurifer.Chron Rech Min,1986,482:55-65.
162.Bower t S.the deposiTion of gold and other metals.Geochim Cosmochim Acta, 55: 2447-2434.
163.Coleman M L, Sheppard t J, Durham, et al. 1982. ReducTion of water with zinc for hydrogen isotope analysis [J]. Anal. Chem., 54: 993-995.
164.Deines P and Gold D P. 1973. the isotopic composiTion of carbonaTite and kimberlite carbonates and their bearing on the isotopic composiTion of deep seated carbon. Geochim. Cosmochim. Acta, 37: 1709-1733.
165.Derry J M , Dipple G M . 1991. Fluid flow ,mineral reacTions, and metasomaTism.. Geology , 19: 211-214.
166.Faure G. 1986. Principles of isotope geology, 2nd ediTion[M]. New York: Wiley and Sons, 497-507.
167.Friedman I and O’Neil J R. 1977. ComplicaTion of stable isotope fracTionaTion factors of geochemical interest in data of geochemistry[M]. 6th ediTion, edited by Fleischer M. Geological Professional Paper.
168.Frietsch R, Perdahl J A. 1995. Rare earth elements in apaTite and magneTite in Kiruna-type iron ores and some otheriron ore types[J]. Ore Geol. Rev., 9: 489-510.
169.Fyfe W S,Price N J,thompson A B. 1978. Fluids in the Earth’s crust .Amsterdam,Oxford ,New York : Elserier ScienTific Publishing Company , 1-383.
170.Ghazi A M, Vanko D A, Roedder E, et al. 1993. DeterminaTion of rare earth elements in fluid inclusions by inducTively coupled plasma-mass spectrometry (ICP-MS) [J].Geochimica et Cosmochimica Acta, 57(18) : 4513-4516.
171.Glazner A F , Bartley J M. 1991. Volume loss, fluid flow and state of strain in extensional mylonites from central Mojave Desert ,Califonia . Journal of Structure Geology , 13: 587-594.
172.Grant J A. 1986. the isocon diagram a simplr soluTion to Gresens’equaTion for metasomaTic alteraTion. Economic Geology, 81:1976-1982.
173.Gresens R L. 1984. ComposiTion –volume relaTionship of metasomaTism . Chemical Geology, 2: 47-55.
174.Groves D I, Goldfarb R J, Gebre-Mriam M, et al. 1998. Orogenic gold deposits: proposed classificaTion in the context of their crustal distribuTion and relaTionship to the other gold deposit types[J]. Ore Geology Reviews, 13:7-27.
175.Groves D I. 1991. Archen lode-gold deposits :the products of crust-scale hydrothermal system .Brazil Gold, 91: 299-305.
176.Haynes D W. 1995. Olympic dam ore genesis : a fluid-mixing model. Economic Geology,.90-281.
177.Houseman G. 1996. From moutain to basin .Nature, 379:771-772.
178.Huang t K. 1945. On Major tectonic Forms of China., Ser. A, No.20, 165pp., 8pls. (with Chinese summary of 11pages)
179.Hudchison C S. 1994. Economic deposit and their tectonic setTing.New York:Macmillan, 1-391.
180.Hudchison C S.Mackenzie D P.,Molnar P. 1981. Convergent instabolity of thickened evoluTion of convergent belts Journal of Geophysics Review, 86: 6135-6155.
181.Hudson J D. 1977. Stable isotopes and limestone lithificaton. J. Geol. Soc. Lond., 133: 637-660.
182.Irvine t N. et al. 1971. A guide to the chemical classificaTion of the common volcanic rocks. Canadian J. Earth Sci. No.5.
183.Jia Y, Kerrich R. 1999. Nitrogen isotope systemaTics of mesothermal lode deposits: Metamorphic, graniTic, meteoric water, or mantle origin? [J] Geology, 27:1051-1054.
184.Jia Y, Kerrich R. 2000. Giant quartz vein systems in accreTionary orogenic belts: the evidence for a metamorphic fluids origin from δ15N and δ13C studies[J]. Earth and Planetary Sciences Letters, 184: 211-224.
185.Keith M L, Weber J N. 1964. Carbon and oxygen isotopic composiTion of selected limestones and fossils[J]. Geochim. Cosmochim. Acta, 28: 1787-1816.
186.Keller J, Hoefs J. 1995. Stable isotope characterisTics of recent natrocarbonaTites from Oldoinyo Lengai, In: Bell K, Keller J eds. 187.CarbonaTite volcanism: Oldoinyo Lengai and the petrogenesis of natrocarbonaTites. Springer Berlin, 113-123.
188.Kerrich D M., Cladeira K. 1998. Metamorphic CO2 degassing from orogenic belts[J]. Chemical Geology, 45: 213-232.
189.Kerrich R, Goldfarb R, Groves D, et al. 2001. the characterisTics, origins and geodynamic setTings of supergiant gold metallogenic provincs [J]. Science in China(series D), 43(supp.): 1-68.
190.Lowenstern J B. 1994. Dissolved volaTile concentraTions in an ore-forming magma[J]. Geology, 22: 893-896.
191.Lowenstern J B. 2001. Carbaon dioxide in magmas and implicaTions for hydrothermal systems[J]. Mineralium Deposita, 36: 490-502.
192.Lowenstern J B. Clynne M A, Bullen t D. 1997. ComagmaTic A-type granophyre and rhyolite from the Alid volcanic center, Eritrrea, northeast Africa[J]. J. Petrol, 38: 1707-1721.
193.Lu H Z, Chi G X. 1996. Geochemical characterisTics of ore forming fluids in shear zone hosted archean gold deposits [J]. 地学前缘, 3(3-4):19-38.
194.Mao J W, Goldfarb R, Zhang Z W, et al. 2002a. Gold deposits in the Xiaoqinling-Xiong'ershan region, Qinling Mountains, central China[J]. Mineralium Deposita, 37(3):306-325.
195.Mao J W, Kerrich R, Li H Y, et al. 2002b. High 3He/4He raTios in the Wangu gold deposit , Hunan province ,China: ImplicaTions for mantle fluids along the tanlu deep fault zone [J]. Geochemical Journal, 36(3): 197-208.
196.Mao J W, Wang Y t, Ding t P, et al. 2002c. Dashuigou tellurium Deposit in Sichuan Province, China: S, C, O, and H Isotope 197.Data and their ImplicaTions on Hydrothermal MineralizaTion [J]. Resource Geology, 52(1): 15-23.
198.Marinelli P, Metrich N, Sbrana A. 1999. Shallow and deep reservoirs involved in magma supply of the 1994 erupTion of Vesuvius[J]. Bull Volcanol, 61: 48-63.
199.McCrea M. 1950. the isotopic chemistry of carbonates and a paleotemperayure scale[J]. J. Chem. Phys., 18: 849-857.
200.Meissner K, Wever R. 1992. the possible role of fluids for the structuring of the conTinental crust ,Earth Science Reviews, 32: 19-32.
201.Miler A R. 1964. High salinity in sea water. Nature, 203: 590-594. Moore J G, Batchelder J N, Cunningham C G. 1977. CO2-filled vesicles in mid-ocean basalt[J]. J. Volcanol Geotherm Res. , 2: 309-327.
202.Murray R W, Brink M R , Jones D L, et al. 1990. REE as indicators of different marine deposiTional environment in chert and shale. Geology, 18: 268-271.
203.Newton RC. 1990. Fluids and shear zones in the deep crust. tectonophysics, 182: 21-27.
204.Newton RC. 1990. 深部地壳中的变质流体,国外科技地质,8:1-90
205.Norman D I, Philip R K and Charles B. 1989. Analysis of trace elements including rare earth elements in fluid inclusion liquids[J]. Economic Geology, 84: 162-166.
206.O’Hara K D. 1988. Fluid flow and volume loss dyring myloniTizaTion:An orogion for phyllonite in an overthuat,North Carolina,USA. tectonphysics , 156: 21-36.
207.O’Hara K. 1990. State of strain in mylonites from the western Blue Ridge province ,southern Appalachians:the role of volume loss . Journal of Structure Geology. 12: 419-430.
208.O’Hara K,Blackbura W H. 1989. Volume loss model for trace element enrichment in mylonite. Geology, 17: 524-527.
2.马天林,杨建民,孙立倩等.土屋铜矿成矿过程与东天山矿产分布.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 129-131
3. 马瑞士,舒良树,孙家齐.东天山构造演化与成矿作.1997.北京:地质出版社,202P.
4. 毛景文,宋叔和,陈毓川.桂北地区成岩系列和锡多金属矿床成矿系列.北京:北京科学技术地质出版社,1988, P 196
5. 毛景文,杨建民,韩春明等.东天山金铜成矿系统和成矿动力学研究.地球科学,2002
6.毛景文,华仁民,李晓波.浅议大规模成矿作用与大型矿集区.矿床地质,1999, 18(4):291-299.
7. 王之田,秦克章.中国铜矿床类型、成矿环境及其时、空分布特点地质学报,1988,62 (3):257-267
8 毛景文,张招崇,任丰寿等.北祁连西段金属矿床时分布规律与成矿环境.地质学报,1999. 73(1):73-82.
9. 陈毓川,毛景文,王平安.桂北地区矿床成矿系列和成矿历史演化轨迹.广西:科学技术出版社,1995
10. 陈毓川,毛景文,王平安.桂北地区矿床成矿系列和成矿多旋回性.第五届全国矿床会议论文集,北京:地质出版社,91-93
11.陈毓川,王登红,林文蔚.中国岩金矿床成矿系列.矿床地质[J] , 1998 增刊:87-92
12.陈毓川,黄民智,徐压等.大厂锡石一硫化物多金属矿带地质特征及成矿系列.地质学报,1985, 59 (3): 228-240
13 陈毓川,裴荣富,宋天锐等,中国矿床成矿系列.第五届全国矿床会议论文集.北京:地质出版社,1993, 89-91
14.陈毓川,裴荣富,宋天锐等,中国矿床成矿系列初论.北京二地质出版社,1998, P 104
15 王元龙,成守德.新疆大地构造四个阶段的演化及其基本特征.见陈海乱等主编,中国碰撞造山带研究.1999,北京:地质出版社,122131.
16 王元龙.成矿系列研究及其应用.新疆地质,1993, 11(4) :332-338
17.王作勋,乌牡继易,吕喜超等.天山多旋回演化与成矿.北京:科学技术出版社,1990,83-130
18.王登红,陈毓川,李红阳等.新疆阿尔泰造山带成矿规律成矿系列研究进展.地质论评,1998, 44(1):62
19.王福同,玛京,胡建卫等.新疆土屋大型斑岩铜矿床特征及发现意义.中国地质,2001 年 1 月,第 28 卷 1 期,36-39.
20.王福同,庄道泽,胡建卫等.物探在新疆土屋地区铜矿床找矿中的应用.中国地质,2001,28 (3):40-X16.
21 车自成,刘洪福,刘良.中大山造山带的形成与演化.北京:地质出版社,1994, 135P
22.邓万明,壳一慢过渡带及其在岩石圈构造演化中的地质意义,科学通报,1997, 42 (23):2474-24820
23. 王龙生,丙宗瑶.超大型斑岩型铜矿形成的必要条件.第六届全国矿床会议论文集北京:地质出版社,1998 , 15-18.
24.叶庆同,石桂华,川一锦华等.怒江、澜仓 l1. ,金沙江地区铅锌矿床成矿特征和成矿系列,北京:科学技术出版社,161p
25.田培仁.新疆北部主要矿产成矿区带划分新疆地质,1994, 12 (1 ): 67-74
26 田培仁.新疆北部主要矿产成矿规律.新疆地质,1994, 12 ( 1): 83-87
27.白云来.新疆东部梧桐窝子群的大地构造背景及其地球化学论证.新疆地质,1994,12(2):106-114
28.王登红,陈毓川.阿尔泰成矿省的成矿系列及成矿规律.北京,原子能出版社.2002,16-410
29 王登红,陈毓川.与海相火山作用有关的铁-铜-铅-锌矿床系列类型及成因初探.矿床地质, 2001, 20 (1)
30.陈毓川,刘德权等.2006 新疆国家紧缺矿产大型矿集区预测评价研究报告.305 项目专题研究报告.代号: 2003BA612A-06-07-18A
31.胡旺亮等.东准噶尔成矿区成矿条件与矿产资源评价研究.305 项目专题研究报告.代号:85-902-03
32.刘德权,唐延龄,周汝洪,中亚古生代造山带成矿作用基本特征.西北地质,2001, 34(2):1-10
33.刘德权,唐延龄,周汝洪,新疆斑岩铜矿的成矿条件和远景新疆地质,2001, 19 (1):43-18.
34.刘德权,唐延龄,周汝洪.中国新疆矿床系列类型.矿床地质,1996. 15 (3 ): 207215.
35.刘德权,唐延龄,周汝洪.新疆北部古生代地壳演化及成矿系列.矿床地质,1992. 11(4):307314.
36.孙宝生.中国天山东部矿床组合和矿床分布模式的大地构造意义.第五届全国矿床会议论文集,1993,北京:地质出版社,68-70
37.毛景文,杨建民等.东天山铜金成矿地质背景和成矿过程研究.2002.国土资源大调查项目研究报告:编号:DKD9902001
38. 成守德,李耀增,王元龙.新疆矿产资源成矿特征与分布规律.矿床地质,1993, 12 (1) : 1-9
39. 朱裕生.论矿床成矿模式.地质论评,1993,39 (3):216-222
40.李华芹,陈富文.2004.中国新疆区域成矿作用年代学.北京:地质出版社,59-83,103-169
41.李锦轶,肖序常,汤耀庆等.新疆北部金属矿产与板块构造.新疆地质,1992, 10 ( 2 ):138-146
42.祁思敬,李英,南秦岭晚古生带海底喷气-沉积成矿系统,地学前缘,1999 6(1)171 一 180
43.何国琦,刘德权,李茂松等.中国新疆古生代地壳演化及成矿.乌鲁木齐:新疆人民出版社,1994
44 何国琦,刘德权,李茂松等新疆土要造山带地壳发展的五阶段模式及成矿系列,新疆地质,1995 年 2 期
45.宋天锐.沉积成矿系列研究的新进展.地质论评,42 (4):357-- 363
46.宋叔和.中国一些主要金属矿床类型及其时空分布规律.矿床地质,1991, 10 (1) :10---18
47.张文淮,成矿流体与成矿机制,地学前缘,1996, 3 (4 ): 245-2520
48.张连昌,曾章仁,杨兴科等,康古尔韧性剪切带型金矿构造地球化学特征.贵金属地质, 1997,6: 13-21.
49.张德润.新疆东部地区大地构造问题探讨.新疆地质,1990, 18 (2) :99-106
50.杨兴科,程宏宾,姬金生等.东天山金铜成矿背景与成矿系统分析.西安工程学院学报,2000, 22 (2):7-14
51.杨兴科,姬金生,张连昌.东天山金矿带区域成矿规律解析.矿床地质,1998 17(增刊):131-134.
52.杨树德.浅议古板块构造的划分原则.新疆地质,新疆地质,1994, 12 (1): 175-179
53.杨树德.新疆北部的古板块构造.新疆地质,新疆地质,1994, 12 (1): 1-8
54.肖序常,汤耀庆,冯益民等.新疆北部及邻区大地构造.北京:地质出版社,1992, 169p
55.芮宗瑶,王龙生,王义大,东大山大地构造格局与成矿动力学探讨.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 3-4
56.芮宗瑶,王龙生,王义天等,东天山土屋和延东斑岩铜矿床时代讨论,矿床地质,2002,21(1):16-22.
57.芮宗瑶,王福同,李恒海.新疆东大山斑岩铜矿带的新进展.中国地质,2001.第 28 卷 2 期,1623.
58.芮宗瑶,刘玉琳,王龙生等,新疆东天山斑岩铜矿带及其大地构造格局.地质学报,2002,76(1):83-93.
59.陈从喜,蔡克勤.矿床成矿系列的若干问题与方向-兼论非金属矿床成矿系列研究的有关问题.地质论评,1998,44 (6) : 596-602
60.陈文明.论东天山土屋一延东铜矿的容矿岩.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 65-67
61.陈陶成.新疆哈密黄山一镜儿泉铜镍矿带成矿地质背景及矿例介绍.西北地质,1990,1:20-250
62.陈毓川矿床成矿系列.地学前缘,1994, 1 (3) :90-94
63.陈毓川主编,中国矿床成矿系列图(附说明书 ).北京:地质出版社,1999
64.郎智君,师波,李大德.新疆二岔口铜矿一戍因探讨.新疆地质,1992, 10(3): 244-252
65.姜立丰,李凤鸣,姬厚贵等,哈密县 885-846 高地 1: 50000 区调报告,1994, 138--151
66.姜立丰,姬厚贵,郑勇.新疆东天山区域构造演化与矿产资源潜力分析.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 73-77
67.姬金生,杨兴科,屈文军.东天山觉罗塔格金、铜成矿带成矿规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 10-1
68.姬金生,李华琴,张连昌等,东天山康古尔金矿磁铁矿绿泥石建造年代学.科学通报,1999(5),439-442
69.姬金生等,东天山康古尔塔格金矿带地质与成矿.北京:地质出版社,1999 , 1-20.
70.桑少杰.东天山地球动力学演化与成矿,东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 78-87
71.涂光炽.初议中亚成矿域地质科学,1990, 34 (4) : 397-404
72.秦克章,方同辉,王书来等,吐哈盆地南缘古生代“天窗”卡拉塔格铜金矿化区的发现及其成矿潜力.中国地质,2001年 3 月,28 (3):16-23
73.秦克章,方同辉,王书来等.东天山古生代板块构造分区、演化与成矿规律研究及勘查应用.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议, 2001,68-72
74.秦克章,孙枢,陈海泄.新疆北部金属矿床时空分布格局-古生代多岛海型碰撞造山带的标志.中国碰撞造山带研究.1999.北京:地质出版社,183-196.
75.秦克章,汪东坡,王之田.中国东部铜矿床类型、成矿集中区与成矿系统.矿床地质,1999. 18(4):359-371.
76.秦克章.新疆中亚型造山带与成矿作用.中国科学院地质与地球物理研究所,2000, 71-157.
77.恩环金川铜镍硫化物矿床成矿模式和成矿系列.地质论评,32 (3) : 276-286
78.郭召杰,马瑞士,郭令智等.新疆东部三条蛇绿棍杂岩带的比较研究.地质论评,1993,139 (3):236-247
79.郭召杰,马瑞士.东天山晚古生代康古尔弧间盆地研究.南京大学学报(地球科学), 1990 (3):103-113
80.贾跃明,流体成矿系统与成矿作用研究,地学前缘,1996, 3 (4): 253-2580
81.车自成, 刘洪福, 刘良. 中天山造山带的形成与演化. 北京:地质出版社, 1994, 135P
82.胡霭琴等. 1985. 天山东段中天山隆起带前寒武纪变质岩系时代及演化—据 U-Pb 年代学研究. 地球化学, 10(3): 285-290
83. 胡受奚,郭继春,顾连兴,周顺之,严正富,杨浩,王金珠,刘延东,1990,加里东造山带在东天山(E85°-95°)构造格架中的重要地位及其地质特征,新疆地质科学(第 1 辑), 32-46
84.姬金生,杨兴科,刘光海,觉罗塔格金、铜成矿带成矿系列分布规律研究与矿床定位预测.新疆国家 305 项目办公室内部报告,2000.
85.李华芹,谢才富,常海亮. 新疆北部有色金属贵金属矿床成矿作用年代学[M]. 北京:地质出版社,1998,202—220.
86. 李锦轶, 肖序常, 汤耀庆等. 新疆北部金属矿产与板块构造. 新疆地质,1992,10(2):138—146
87. Huang t K. On Major tectonic Forms of China.
88.Windley B F, Allen M B, Zhang C, Zhao Z Y, and Wang G R. 1990. Paleozoic accreTion and Cenozoic redeformaTion of Chinese Tien Shan rang, central Asia. Geology, 18: 128-131
89.马瑞士, 舒良树, 孙家齐. 1997. 东天山构造演化与成矿. 地质出版社, 北京
90.马瑞士, 王赐银, 叶尚夫等. 1993. 东天山构造格架及地壳演化
91.姬金生,陶洪祥,曾章仁,杨兴科,张连昌等. 1994. 东天山康古尔塔格金矿带地质与成矿. 北京:地质出版社
92.李锦轶. 1991. 试论新疆东准噶尔古生代板块构造演化. 见: 肖序常和汤耀庆主编, 古中亚复合巨型缝合带南缘构造演化, 北京: 北京科学技术出版社, 92-108
93.李先梓,李行等. 新疆铂族元素成矿地质条件及找矿方向.中国地质科学院西安地质矿产研究所所刊,1991,第 33号.
94.刘德权,唐延龄,周汝洪. 中国新疆矿床系列类型. 矿床地质,1996.15(3):207 2 15.
95.马瑞士,叶尚夫,王赐银等.东天山造山带构造格架与演化.新疆地质科学,1990(2):21-36
96. 秦克章,孙枢,陈海泓.新疆北部金属矿床时空分布格局—古生代多岛海型碰撞造山带的标志[C]. 见陈海泓主编,中国碰撞造山带研究. 1999.北京:地质出版社,183-196
97.秦克章. 新疆北部中亚型造山与成矿作用.中国科学院地质与地球物理研究所博士后研究工作报告,2000.
98.毛景文,杨建民,屈文俊,杜安道,韩春明,王志良. 新疆黄山东铜镍硫化物矿床 Re-Os 同位素测定及其地球动力学意义. 矿床地质,2002b,21(4):323-330
99.芮宗瑶,王龙生,王义天等,东天山土屋和延东斑岩铜矿床时代讨论[J],矿床地质,2002,21(1):16—22.
100.王润民,刘德权,印静泰等.新疆哈密土墩-黄山一带铜镍硫化物矿床成矿控制条件及找矿方向的研究.矿物岩石,1987(1):31-34.
101.阎文元,天山东段早石炭世岛弧火山岩特征及其矿产.新疆地质,1985,3(2):49-58
102.周济元、茅燕石、黄志勋、何大伦、王道永、消渊甫. 东天山古大陆边缘火山地质.成都:成都科技大学出版社,1994.
103.徐兴旺,马天林,孙立倩,李贵书,张学勤,徐湘康,吴继修.新疆东天山罗觉塔格韧性挤压带基本特征及动力学意义.地质科学,1998,33(2):147-156.
104.张良臣. 1995. 中国新疆板块构造与动力学特征. 见: 新疆第三届天山地质矿产学术讨论会论文选辑. 乌鲁木齐: 新疆人民出版社, 1-14
105.李锦轶,王克卓,李文铅等.东天山地区构造格架.DKD9902002 研究报告,2002
106.梁月明, 黄旭钊, 徐昆, 于学政, 王越胜, 张文志, 蔡玉梅. 2001. 新疆康古尔塔格断裂带地球物理场及深部地质特征. 中国区域地质, 20(4): 398-403
107.汪振文. 1986. 天山东部及北山区域磁场特征与深部地质构造的初步分析. 新疆地质, 4(3): 107-114
108.汪振文. 1987. 天山东部及北山区域布格重力异常特征与矿产分布关系的探讨,新疆地质,5(2): 68-75
109.王学求,迟清华,程志中等.新疆荒漠戈壁区深穿透地球化学调查与研究.内部研究报告,2001
110.刘德权,唐延龄,周汝洪. 新疆北部古生代地壳演化及成矿系列. 矿床地质,1992. 11(4):307 314.
111.陈哲夫, 梁云海. 新疆天山地质构造几个问题的探讨. 新疆地质, 1985, 3(2):1-13
112.张良臣, 吴乃元. 1985. 天山地质构造及发展史. 新疆地质, 3(3): 1-14
113.舒良树,夏飞雅克,马瑞士,1998,中天山北缘大型右旋走滑韧剪带研究,新疆地质,16/4 总 60,326-336
114.车自成, 刘洪福, 刘良. 中天山造山带的形成与演化. 北京:地质出版社, 1994, 135P
115.李锦轶. 1991. 试论新疆东准噶尔古生代板块构造演化. 见: 肖序常和汤耀庆主编, 古中亚复合巨型缝合带南缘构造演化, 北京: 北京科学技术出版社, 92-108
116.姜常义,穆艳梅,赵晓宁,白开寅,张虹波. 2001. 塔里木板块北缘活动陆缘型侵入岩带的岩石学与地球化学. 中国区域地质, 20(2):158-163
117.李锦轶, 肖序常, 汤耀庆等. 新疆北部金属矿产与板块构造. 新疆地质,1992,10(2):138—146
118.李先梓,李行等. 新疆铂族元素成矿地质条件及找矿方向.中国地质科学院西安地质矿产研究所所刊,1991,第 33号.
119.马瑞士, 叶尚夫, 王赐银. 1990. 东天山造山带构造格架和演化. 新疆地质科学, 第二辑, 21-36. 北京: 地质出版社
120.王鸿祯等,中国地理图集,1987
121.王作勋,邬继易,吕喜朝,张经国,刘成德,1990,天山多旋回构造演化及成矿. 北京: 科学出版社
122.徐兴旺,马天林,孙立倩,李贵书,张学勤,徐湘康,吴继修.新疆东天山罗觉塔格韧性挤压带基本特征及动力学意义.地质科学,1998,33(2):147-156.
123.汪振文. 1988. 中国天山区域地球物理特征及深部地壳构造,新疆地质,6(2): 29-34
124.舒良树,夏飞雅克,马瑞士,1998,中天山北缘大型右旋走滑韧剪带研究,新疆地质,16/4 总 60,326-336
125.陶维屏.中国非金属矿床的成矿系列.地质学报,1989, 63 (4) : 324-337
126.顾连兴,褚强,胡受奚.新疆卡拉麦里一哈尔里克碱性花岗岩带地质特征及成因.新疆地质科学,1990 年 2 期,47-55
127.高常林,崔可锐,钱一雄等.天山微板块与塔里木盆地.北京:地质出版社,1995, 284p
128.崔彬,成矿空间初探.地质与勘探,1999, No.3
129.崔彬.江西九瑞地区铜金成矿系列模式.矿床地质,1998, 14 (1) : 44-50
130 崔彬等.物质场-能量场-空间场综合成矿预测.现代地质,No4
131.章崇真.略论华南中生代花岗岩成矿系列.矿床地质,1983 (1) : 38-46
132.黄明渊.黄山东铜镍矿床地球化学特征及靶区优选.新疆地质,1990, 8 (2) :142-152
133.程裕淇,陈毓川,赵一鸣等,再论矿床的成矿系列问题,中国地质科学院院报,1983,总第 6 号,1-64
134.程裕淇,陈毓川,赵一鸣等,再论矿床的成矿系列问题-兼论中生代某些矿床的成矿系列,地质论评,1983, 29 (2), 127-139
135.韩发,Sedex 型矿床成矿系统,地学前缘,1999, 6 (1) 139--162
136.韩宝福,何国琦,王式光等,新疆北部后碰撞慢源岩浆活动与陆壳纵向生长.地质论评,44 (4):396-406
137.韩春明,毛景文,杨建民等.东天山晚古生代内生金属矿床成矿系列和成矿规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 65-67
138.翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999 } 1-288.
139.翟裕生,邓军,崔彬等.成矿系统及综合地质异常.现代地质,13 (1) : 99-103.
140.翟裕生,张湖等,大型构造与大型矿床,北京:地质出版社,1997, 173-180
141.翟裕生,姚书振,林新多.长江中下游地区铁、铜等成矿规律研究矿床地质,1992,11(1):1-12
142.翟裕生,姚书振,林新多.长江中下游地区铁铜矿床类型、形成条件和成矿演化.地球科学:地质出版社,1983, No.4
143.翟裕生,姚书振,崔彬等.成矿系列研究.武汉:中国地质大学出版社,1996, 198p
144.翟裕生.成矿系列研究问题.现代地质,1992, 6 (3):301-307
145.翟裕生.成矿系统及其演化初步实践到理论思考.地球科学,25 (4):333-339
146.翟裕生.论成矿系统.地学前缘,1999, 6 (1):13-27
147.翟裕生等.关于成矿一系列和成矿模式问题.矿床学参考书(下册).北京:地质出版社,1987:214-218
148.裴荣富,洪大伟.碰撞造山与华南花岗岩及其成矿系列研究的新进展矿床地质,1990,14(4):329-334.
149.裴荣富,邱小平,尹冰川,成矿作用爆发异常及巨量金属堆积.矿床地质,1999, 18 (4):331-340.
150.薛春纪,陈毓川,姬金生等.东天山矿床成矿系列和分布规律.东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001, 60-62
151.Benning L G,Hydrosuphide complexing of gold in hydrothermal soluTion from 150℃to 5000C and 500 to 1500 bars Geochim Cosmochim Acta,1996,60:1849-1877.
152. Miler A R. High salinity in sea water. Nature, 1964, 203:590-594.
153. Ague J J, Joost L M, Van Haren. Assesing metamomTic mass and volume changes using boottrap with applicaTion to deep crustral hydrothermal alteraTion of marmble RrOnnmic GP}ln}v_199fi_91·llfi9-1189_
154.Allen M B, Windley B F and Zhang C. 1992. Paleozoic collisional tectonics and magmaTism of the Chinese Tien Shan, central Asia. tectonophysics, 220, 89-115
155.Baker A J and Fallick A E. 1989. Evidence from Lewisian limestones for isotopically heavy carbon in two-thousand-million-year-old sea water. Nature, 337: 352-354.
156.Banks D A, Yardley B W D, Campbell A R, et al. 1994. REE composiTion of an aqueous magmaTic fluid: a fluid inclusions study from the Capitan Pluton, New Mexico, U S A[J]. Chemical Geology, 113: 259-272.
157.Barley M E ,Groves D I. 1992. SuperconTinent Cycles and the distribuTion of metal deposit through Time. Geology, 20:291-294
158.Barnicocat A C, Fare R J, Groves D L, et al. 1991. Synmetamorphic lode-gold deposits in high-grade Archaean setTing[J]. Geology, 19: 921-924.
159.Baumgartner L P,Olsen S N. 1996. A least-squares approach to mass transport calculaTion using the isocon method. Economic Geology, 91:1169-1182.
160.Benning L G. 1996. Hydrosuphide complexing of gold in hydrothermal soluTion from 150℃to 500℃ and 500 to 1500 bars Geochim Cosmochim Acta, 60:1849-1877.
161.Bonnemaison M. 1991. “Filons de aurifere ”an cas parTiculiar de shear aurifer.Chron Rech Min,1986,482:55-65.
162.Bower t S.the deposiTion of gold and other metals.Geochim Cosmochim Acta, 55: 2447-2434.
163.Coleman M L, Sheppard t J, Durham, et al. 1982. ReducTion of water with zinc for hydrogen isotope analysis [J]. Anal. Chem., 54: 993-995.
164.Deines P and Gold D P. 1973. the isotopic composiTion of carbonaTite and kimberlite carbonates and their bearing on the isotopic composiTion of deep seated carbon. Geochim. Cosmochim. Acta, 37: 1709-1733.
165.Derry J M , Dipple G M . 1991. Fluid flow ,mineral reacTions, and metasomaTism.. Geology , 19: 211-214.
166.Faure G. 1986. Principles of isotope geology, 2nd ediTion[M]. New York: Wiley and Sons, 497-507.
167.Friedman I and O’Neil J R. 1977. ComplicaTion of stable isotope fracTionaTion factors of geochemical interest in data of geochemistry[M]. 6th ediTion, edited by Fleischer M. Geological Professional Paper.
168.Frietsch R, Perdahl J A. 1995. Rare earth elements in apaTite and magneTite in Kiruna-type iron ores and some otheriron ore types[J]. Ore Geol. Rev., 9: 489-510.
169.Fyfe W S,Price N J,thompson A B. 1978. Fluids in the Earth’s crust .Amsterdam,Oxford ,New York : Elserier ScienTific Publishing Company , 1-383.
170.Ghazi A M, Vanko D A, Roedder E, et al. 1993. DeterminaTion of rare earth elements in fluid inclusions by inducTively coupled plasma-mass spectrometry (ICP-MS) [J].Geochimica et Cosmochimica Acta, 57(18) : 4513-4516.
171.Glazner A F , Bartley J M. 1991. Volume loss, fluid flow and state of strain in extensional mylonites from central Mojave Desert ,Califonia . Journal of Structure Geology , 13: 587-594.
172.Grant J A. 1986. the isocon diagram a simplr soluTion to Gresens’equaTion for metasomaTic alteraTion. Economic Geology, 81:1976-1982.
173.Gresens R L. 1984. ComposiTion –volume relaTionship of metasomaTism . Chemical Geology, 2: 47-55.
174.Groves D I, Goldfarb R J, Gebre-Mriam M, et al. 1998. Orogenic gold deposits: proposed classificaTion in the context of their crustal distribuTion and relaTionship to the other gold deposit types[J]. Ore Geology Reviews, 13:7-27.
175.Groves D I. 1991. Archen lode-gold deposits :the products of crust-scale hydrothermal system .Brazil Gold, 91: 299-305.
176.Haynes D W. 1995. Olympic dam ore genesis : a fluid-mixing model. Economic Geology,.90-281.
177.Houseman G. 1996. From moutain to basin .Nature, 379:771-772.
178.Huang t K. 1945. On Major tectonic Forms of China.
179.Hudchison C S. 1994. Economic deposit and their tectonic setTing.New York:Macmillan, 1-391.
180.Hudchison C S.Mackenzie D P.,Molnar P. 1981. Convergent instabolity of thickened evoluTion of convergent belts Journal of Geophysics Review, 86: 6135-6155.
181.Hudson J D. 1977. Stable isotopes and limestone lithificaton. J. Geol. Soc. Lond., 133: 637-660.
182.Irvine t N. et al. 1971. A guide to the chemical classificaTion of the common volcanic rocks. Canadian J. Earth Sci. No.5.
183.Jia Y, Kerrich R. 1999. Nitrogen isotope systemaTics of mesothermal lode deposits: Metamorphic, graniTic, meteoric water, or mantle origin? [J] Geology, 27:1051-1054.
184.Jia Y, Kerrich R. 2000. Giant quartz vein systems in accreTionary orogenic belts: the evidence for a metamorphic fluids origin from δ15N and δ13C studies[J]. Earth and Planetary Sciences Letters, 184: 211-224.
185.Keith M L, Weber J N. 1964. Carbon and oxygen isotopic composiTion of selected limestones and fossils[J]. Geochim. Cosmochim. Acta, 28: 1787-1816.
186.Keller J, Hoefs J. 1995. Stable isotope characterisTics of recent natrocarbonaTites from Oldoinyo Lengai, In: Bell K, Keller J eds. 187.CarbonaTite volcanism: Oldoinyo Lengai and the petrogenesis of natrocarbonaTites. Springer Berlin, 113-123.
188.Kerrich D M., Cladeira K. 1998. Metamorphic CO2 degassing from orogenic belts[J]. Chemical Geology, 45: 213-232.
189.Kerrich R, Goldfarb R, Groves D, et al. 2001. the characterisTics, origins and geodynamic setTings of supergiant gold metallogenic provincs [J]. Science in China(series D), 43(supp.): 1-68.
190.Lowenstern J B. 1994. Dissolved volaTile concentraTions in an ore-forming magma[J]. Geology, 22: 893-896.
191.Lowenstern J B. 2001. Carbaon dioxide in magmas and implicaTions for hydrothermal systems[J]. Mineralium Deposita, 36: 490-502.
192.Lowenstern J B. Clynne M A, Bullen t D. 1997. ComagmaTic A-type granophyre and rhyolite from the Alid volcanic center, Eritrrea, northeast Africa[J]. J. Petrol, 38: 1707-1721.
193.Lu H Z, Chi G X. 1996. Geochemical characterisTics of ore forming fluids in shear zone hosted archean gold deposits [J]. 地学前缘, 3(3-4):19-38.
194.Mao J W, Goldfarb R, Zhang Z W, et al. 2002a. Gold deposits in the Xiaoqinling-Xiong'ershan region, Qinling Mountains, central China[J]. Mineralium Deposita, 37(3):306-325.
195.Mao J W, Kerrich R, Li H Y, et al. 2002b. High 3He/4He raTios in the Wangu gold deposit , Hunan province ,China: ImplicaTions for mantle fluids along the tanlu deep fault zone [J]. Geochemical Journal, 36(3): 197-208.
196.Mao J W, Wang Y t, Ding t P, et al. 2002c. Dashuigou tellurium Deposit in Sichuan Province, China: S, C, O, and H Isotope 197.Data and their ImplicaTions on Hydrothermal MineralizaTion [J]. Resource Geology, 52(1): 15-23.
198.Marinelli P, Metrich N, Sbrana A. 1999. Shallow and deep reservoirs involved in magma supply of the 1994 erupTion of Vesuvius[J]. Bull Volcanol, 61: 48-63.
199.McCrea M. 1950. the isotopic chemistry of carbonates and a paleotemperayure scale[J]. J. Chem. Phys., 18: 849-857.
200.Meissner K, Wever R. 1992. the possible role of fluids for the structuring of the conTinental crust ,Earth Science Reviews, 32: 19-32.
201.Miler A R. 1964. High salinity in sea water. Nature, 203: 590-594. Moore J G, Batchelder J N, Cunningham C G. 1977. CO2-filled vesicles in mid-ocean basalt[J]. J. Volcanol Geotherm Res. , 2: 309-327.
202.Murray R W, Brink M R , Jones D L, et al. 1990. REE as indicators of different marine deposiTional environment in chert and shale. Geology, 18: 268-271.
203.Newton RC. 1990. Fluids and shear zones in the deep crust. tectonophysics, 182: 21-27.
204.Newton RC. 1990. 深部地壳中的变质流体,国外科技地质,8:1-90
205.Norman D I, Philip R K and Charles B. 1989. Analysis of trace elements including rare earth elements in fluid inclusion liquids[J]. Economic Geology, 84: 162-166.
206.O’Hara K D. 1988. Fluid flow and volume loss dyring myloniTizaTion:An orogion for phyllonite in an overthuat,North Carolina,USA. tectonphysics , 156: 21-36.
207.O’Hara K. 1990. State of strain in mylonites from the western Blue Ridge province ,southern Appalachians:the role of volume loss . Journal of Structure Geology. 12: 419-430.
208.O’Hara K,Blackbura W H. 1989. Volume loss model for trace element enrichment in mylonite. Geology, 17: 524-527.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |