塔里木盆地显生宙古隆起的分布及迁移
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摘要
塔里木盆地属于多期叠合盆地,存在多期不整合与古隆起构造,二者的形成及发育密切相关。利用钻井、地震、野外露头等综合资料,开展了盆地尺度的构造层、不整合结构构造、累积最小生长指数分析,进一步了解盆地内多个古隆起的分布、成因及隆升过程,特别是和田、塔中、塔北、巴楚、塔东古隆起及其内部的形成演化。发现盆地内不同时期古隆起构造变形和展布与盆地周缘造山带构造作用相响应。早古生代以来盆地内古隆起经历了6次大的迁移,每次迁移的动力来源于该时期盆地周缘的板块边缘或造山带的构造活动。根据隆起形成的主控因素,塔里木盆地古隆起主要可分为4种成因类型,包括断控隆起、继承性隆起、前陆盆地前缘隆起和构造古地理隆起等。古隆起隆升的差异还体现在隆起区内不同部位上,对油气成藏有重要意义。
The Tarim Basin is the largest superimposed basin in NW China,in which the multiple regional unconformities and palaeo-uplifts developed in the Phanerozoic,and both of them are closely related in their formation and evolution.In this paper,based on the seismic,drilling and outcrop data,the tectonic sequences,the structural architectures of unconformities and the accumulation minimum growth factor in basin-scale are analyzed.The distribution,formation and uplifting process of palaeo-uplifts are better understood,especially in the Hotian,Tazhong,Tabei,Bachu,and Tadong palaeo-uplifts.The results suggest that the structural deformations and distributions of palaeo-uplifts during the main tectonic movement phases in the Tarim Basin are coordinated with the tectonism of the peripheral orogenic belts.From the Early Paleozoic to present,six times of migrations of the palaeo-uplifts had occurred.And each migration had changed and responded to the tectonism of the peripheral basin orogens in the same phase.According to the controlling factors of palaeouplift formation,the uplifts in this basin can be divided into four genetic types,including the fault controlled uplift,the inheritance uplift,the forebulge of the foreland basin and the tectonic palaeo-geography uplift.The differential uplifting of the palaeo-uplifts occurring in their different parts may be significant for the oil and gas accumulation.
引文
[1]刘和甫,李晓清,刘立群.盆山耦合与前陆盆地成藏区带分析[J].现代地质,2004,18(4):389-403.
    [2]刘池洋,赵红格,张参.青藏—喜马拉雅构造域演化的转折时期[J].地学前缘,2009,16(4):1-12.
    [3]李德威,夏义平,徐礼贵.大陆板内盆山耦合及盆山成因:以青藏高原及周边盆地为例[J].地学前缘,2009,16(3):110-119.
    [4]Mattauer M.地壳变形(1980)[M].孙坦,张道安,译.北京:地质出版社,1984:1-339.
    [5]许志琴.地壳变形与显微构造[M].北京:地质出版社,1984:1-133.
    [6]许志琴,杨经绥,李海兵,等.造山的高原:青藏高原的地体拼合、碰撞造山及隆升机制[M].北京:地质出版社,2007:1-458.
    [7]Levorsen A I.Geology of Petroleum[M].2nd ed.Tulsa:The American Association of Petroleum Geologist Foundation,2001:1-700.
    [8]何登发.塔里木盆地的地层不整合面与油气聚集[J].石油学报,1995,16(3):14-21.
    [9]贾承造,魏国齐,姚慧君,等.塔里木盆地油气勘探丛书:盆地构造演化与区域构造地质[M].北京:石油工业出版社,1995:1-70.
    [10]贾承造,孙德龙,周新源,等.塔里木盆地板块构造与大陆动力学[M].北京:石油工业出版社,2004:1-202.
    [11]金之钧,张一伟,陈书平.塔里木盆地构造-沉积波动过程[J].中国科学:D辑,2005,35(6):530-539.
    [12]何登发,李德生,童晓光,等.多期叠加盆地古隆起控油规律[J].石油学报,2008,29(4):475-488.
    [13]许效松,门玉澎,张海全.古陆、古隆与古地理[J].沉积与特提斯地质,2010,30(3):1-10.
    [14]何碧竹,许志琴,焦存礼,等.塔里木盆地构造不整合成因及对油气成藏的影响[J].岩石学报,2011,27(1):253-265.
    [15]何碧竹,焦存礼,许志琴,等.阿尔金—西昆仑早古生代构造作用在塔里木盆地塘古兹巴斯凹陷中的响应[J].岩石学报,2011,27(11):3435-3448.
    [16]何碧竹,焦存礼,许志琴,等.不整合结构构造与构造古地理环境:以加里东中期青藏高原北缘及塔里木盆地为例[J].岩石学报,2013,29(6):2184-2198.
    [17]刘池洋.叠合盆地特征及油气赋存条件[J].石油学报,2007,28(1):1-7.
    [18]贾承造.环青藏高原巨型盆山体系构造与塔里木盆地油气分布规律[J].大地构造与成矿学,2009,33(1):1-9.
    [19]许志琴,李思田,张建新,等.塔里木地块与古亚洲/特提斯构造体系的对接[J].岩石学报,2011,27(1):1-22.
    [20]万天丰.论构造地质学和大地构造学的几个重要问题[J].地学前缘,2014,21(1):132-149.
    [21]万天丰.中国大地构造学纲要[M].北京:地质出版社,2004:1-387.
    [22]汤良杰,金之钧,庞雄奇.多期叠合盆地油气运聚模式[J].石油大学学报:自然科学版,2000,24(4):67-70.
    [23]Xu Z Q,He B Z,Zhang C L,et al.Tectonic framework and crustal evolution of the Precambrian basement of the Tarim Block in NW China:New geo-chronological evidence from deep drilling samples[J].Precambrian Research,2013,235:150-162.
    [24]Tapponnier P,Xu Z Q,Roger F O,et al.Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2001,294(23):1671-1677.
    [25]刘训.天山—西昆仑地区沉积-构造演化史:新疆地学断面走廊域及邻区不同地体的沉积-构造演化[J].古地理学报,2001,3(3):21-31.
    [26]冯增昭,鲍志东,吴茂炳,等.塔里木地区寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2005:1-186.
    [27]陈景山,王振宇,代宗仰,等.塔中地区中、上奥陶统台地镶边体系分析[J].古地理学报,1999,1(2):8-17.
    [28]赵文智,张光亚,等.被动大陆边缘演化与油气地质:以塔里木盆地西南地区为例[M].北京:石油工业出版社,2007:1-234.
    [29]何登发,孙方原,何金有,等.温宿北—野云沟断裂的构造几何学与运动学特征及塔北隆起的成因机制[J].中国地质,2011,38(4):917-934.
    [30]王国林,李曰俊,孙建华,等.塔里木盆地西北缘柯坪冲断带构造变形特征[J].地质科学,2009,44(1):50-62.
    [31]焦存礼,何碧竹,邢秀娟,等.塔中地区奥陶系加里东中期Ⅰ幕古岩溶特征及控制因素研究[J].中国石油勘探,2010,15(1):21-26.
    [32]赵宗举,赵治信,黄智斌.塔里木盆地奥陶系牙形石带及沉积层序[J].地层学杂志,2006,30(3):193-201.
    [33]蔡习尧,钱一雄,陈跃,等.塔中地区中、下奥陶统划分与对比[J].新疆石油地质,2007,28(3):292-295.
    [34]Riba O.Syntectonic unconformities of the Acto Cardener,Spanish Pyrenees:A genetic interpretation[J].Sedimentary Geology,1976,15:213-233.
    [35]陈发景,张光亚,陈昭年.不整合分析及其在陆相盆地构造研究中的意义[J].现代地质,2004,18(3):269-275.
    [36]何登发,李德生,何金有,等.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示[J].石油学报,2013,34(2):201-218.
    [37]陈汉林,罗俊成,郭群英,等.塔里木盆地东南缘中新生代变形史与构造演化[J].大地构造与成矿学,2009,33(1):38-45.
    [38]张传林,陆松年,于海峰,等.青藏高原北缘西昆仑造山带构造演化:来自锆石SHRIMP及LA-ICP-MS测年的证据[J].中国科学:D辑,2007,27(2):145-154.
    [39]王超,刘良,车自成,等.塔里木南缘铁克里克构造带东段前寒武纪地层时代的新限定和新元古代地壳再造:锆石定年和Hf同位素的约束[J].地质学报,2009,83(11):1647-1656.
    [40]张建新,李怀坤,孟繁聪,等.塔里木盆地东南缘(阿尔金山)“变质基底”记录的多期构造热事件:锆石U-Pb年代学的制约[J].岩石学报,2011,27(1):23-46.
    [41]Matte P H,Tapponnier P,Arnaud N,et al.Tectonics of Western Tibet,between the Tarim and the Indus[J].Earth and Planetary Science Letters,1996,142(3/4):311-330.
    [42]杨经绥,宋曙光,许志琴,等.柴达木盆地北缘早古生代高压-超高压变质带中发现典型超高压矿物:柯石英[J].地质学报,2001,75(2):175-179.
    [43]Zhang J X,Mattinson C G,Meng F C,et al.An Early Palaeozoic HP/HT granulite-garnet peridotite association in the south Altyn Tagh,NW China:p-T history and U-Pb geochronology[J].Journal of Metamorphic Geology,2005,23:491-510.
    [44]Zhang J X,Mattinson C G,Yu S Y,et al.U-Pb zircon geochronology of coesite-bearing eclogites from the southern Dulan area of the North Qaidam UHP terrane,northwestern China:Spatially and temporally extensive UHP metamorphism during continental subduction[J].Journal of Metamorphic Geology,2010,28:955-978.
    [45]Song S G,Zhang L F,Niu Y L.Zircon U-Pb SHRIMP ages of eclogites in the North Qilian Mountains and their tectonic implications[J].Chinese Science Bulletin,2004,49:848-852.
    [46]杨海波,高鹏,李兵,等.新疆西天山达鲁巴依蛇绿岩地质特征[J].新疆地质,2005,23(2):123-126.
    [47]肖序常,汤耀庆,王军,等.中国南天山造山带蓝片岩及其构造意义[J].地球学报,1994,15(增刊1):54-64.
    [48]汤耀庆,高俊,赵民,等.西南天山蛇绿岩和蓝片岩[M].北京:地质出版社,1995:1-133.
    [49]高俊,钱青,龙灵利,等.西天山的增生造山过程[J].地质通报,2009,28(12):1804-1816.
    [50]Lin W,Chu Y,Ji W B,et al.Geochronological and geochemical constraints for a Middle Paleozoic continental arc on the northern margin of the Tarim block:Implications for the Paleozoic tectonic evolution of the South Chinese Tianshan[J].Lithosphere,2013,5(4):355-381.
    [51]郭召杰,张志诚,吴朝东,等.中、新生代天山隆升过程及其与准噶尔、阿尔泰山比较研究[J].地质学报,2006,80(1):1-15.
    [52]周鼎武,苏犁,简平,等.南天山榆树沟蛇绿岩地体中高压麻粒岩SHRIMP锆石U-Pb年龄及构造意义[J].科学通报,2004,49(14):1411-1415.
    [53]高俊,龙灵利,钱青,等.南天山:晚古生代还是三叠纪碰撞造山带[J].岩石学报,2006,22(5):1049-1061.
    [54]许志琴,杨经绥,戚学祥,等.印度/亚洲碰撞:南北向和东西向拆离构造与喜马拉雅造山机制的再讨论[J].地质通报,2006,25(1/2):1-14.
    [55]肖文交,周辉,Windley B F,等.西昆仑造山带复式增生楔的构造特征与演化[J].新疆地质,2003,21(1):31-36.
    [56]陈正乐,万景林,刘健,等.西天山山脉多期次隆升-剥露的裂变径迹证据[J].地球学报,2006,27(2):97-106.
    [57]李海兵,Liou J G.阿尔金断裂带印支期走滑活动的地质及年代学证据[J].科学通报,2001,46(16):1333-1338.
    [58]肖序常,李廷栋.青藏高原的构造演化与隆升机制[M].广州:广东科技出版社,2000:1-122.
    [59]史仁灯.班公湖SSZ型蛇绿岩年龄对班-怒洋时限的制约[J].科学通报,2007,52(2):223-227.
    [60]刘池洋,杨兴科,任战利,等.藏北羌塘盆地查桑地区构造格局与演化[J].中国科学:D辑,2001,31(增刊1):14-19.
    [61]Monlar P,Tapponnier P.Cenozoic tectonics of Asia:Effects of a continental collision[J].Science,1975,189:419-426.
    [62]Tapponnier P,Peltzer G,Armijo R.On the mechanics of the collision between India and Asia[M]∥Coward M P,Riess A C.Collision Tectonics.London:Geological Society,Special Publication,1986,19:115-157.
    [63]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-151.
    [64]梁狄刚,张水昌,张宝民,等.从塔里木盆地看中国海相生油问题[J].地学前缘,2000,7(4):534-547.
    [65]庞雄奇,高剑波,孟庆洋.塔里木盆地台盆区构造变动与油气聚散关系[J].石油与天然气地质,2006,27(5):594-603.
    [66]王招明,王清华,赵孟军,等.塔里木盆地和田河气田天然气地球化学特征及成藏过程[J].中国科学:D辑,2007,37(增刊2):69-79.
    [67]赵宗举,贾承造,周新源,等.塔里木盆地塔中地区奥陶系油气成藏主控因素及勘探选区[J].中国石油勘探,2006,11(4):6-15.
    [68]康玉柱,康志宏.塔里木古生代海相大油气田形成条件及勘探方向[J].海相油气地质,2002,7(3):28-33.
    [69]汤良杰,贾承造.塔里木叠合盆地构造解析和应力场分析(精)/中国典型叠合盆地油气形成富集与分布预测丛书[M].北京:科学出版社,2007:1-149.
    [70]林畅松,李思田,刘景彦,等.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化[J].岩石学报,2011,27(1):210-218.
    [71]云金表,周波,金之钧.断裂带对油气运聚控制作用探讨:以塔里木台盆区阿克库勒凸起与塔中低隆为例[J].地学前缘,2013,20(5):126-131.

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