中国西部燕山运动及其对油气成藏的控制

doi:10.11743/ogg20080401

Abstract

Abstract:

The mid-Yanshan tectonic movement had rebuilt the tectonic framework in western China.At the end of Late Jurassic,the Yarlung-Tsangbo oceanic lithosphere of the Neo-Tethys subducted northward,Bangong CoNu Jiang ocean was closed,Lasha and Qiangtang blocks collided,and the Okhotsk sea in the north was also closed.The regional tectonic compression reactivated the ancient suture and large old faults and accelerated the uplifting of the Orogenic belt in western China.It also led to the formation of angular unconformities of various scopes and types between the Jurassic and Cretaceous in the western basins,the formation of new structures at the margins of the basin and along the faults,and further reconstruction of the existing structures.Accompanying with the movement,the basins in western China entered a new evolution stage since the Cretaceous (the timing might be a little bit different in different regions).The significances of Yanshan movement to hydrocarbon accumulation and reservoir readjustment include:(1)it exerted dual influences to the underlying source rocks through speeding up thermal evolution in the relatively continuous and rapid subsidence zones at piedmont and postponing the peak of hydrocarbon generation and expulsion in zones experienced multi-stage uplifting and slow subsidence,thus providing conditions for the highly effective hydrocarbon accumulation during the Himalayan period;(2)deformation,uplifting,weathering,erosion,and leaching greatly improved the poroperm characteristics of the reservoirs underlying the unconformities,and extensive glutenite reservoirs of high quality were deposited in the lower part of the Cretaceous above the unconformities;(3)the various types of traps in combination with the paleohighs and faulted zones laid down foundation for the formation of different types of hydrocarbon accumulations in various strata.

Key words: unconformity, basin-range coupling, hydrocarbon accumulation, Yanshanian movement, western China

CLC Number:

TE121.1

He Zhiliang, Gao Shanlin. The Yanshanian movement and its control over hydrocarbon accumulation in western China[J]. Oil & Gas Geology, 2008, 29(4): 419-427.

References

[1] 翁文灏.中国东部中生代以来之地壳运动及火山活动[J].中国地质学会志,1927,6(1),9～36
[2] 黄汲清.中国地质构造基本特征的初步总结[J].地质学报,1960,40(1):1～37
[3] 任纪瞬,陈廷愚,牛宝贵,等.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京:科学出版社,1990.90～91
[4] 赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319～328
[5] 翟明国,朱日祥,刘建明.华北东部中生代构造体制转折的关键时限[J].中国科学(D辑),2003,33(10):913～920
[6] 何登发,贾承造,李德生,等.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64～77
[7] 周良仁,蔡厚维.中国西北地区的燕山运动[J].西北地质科学,1990,30(1):64～78
[8] Hendrix M S,Graham S A,Carrol A R,et al.Sedimentary record and climatic implication of recurrent deformation of the Tian Shan:evidence from Mesozoic strata of the north Tarim,south Junggar and Turpan basins[J].Geological Society of America Bulletin,1992,104:53-79
[9] 卢华复,王胜利,罗俊成,等.塔里木盆地东部断裂系统及其构造演化[J].石油与天然气地质,2006,27(4):433～441
[10] 何治亮,罗传容,龚铭,等.塔里木多旋回叠加盆地与复式成藏系统[M].武汉:中国地质大学出版社,2001.5～17
[11] 贾承造,陈汉林,杨树锋,等.库车坳陷晚白垩世隆升过程及其地质响应[J].石油学报,2003,24(3):1～14
[12] 卢华复,陈楚铭,刘志宏,等.库车再生前陆逆冲带的构造特征与成因[J].石油学报,2000,21(3):19～24
[13] 赵白.燕山、喜马拉雅构造运动在准噶尔盆地油气运聚中的作用[J].新疆石油地质,2004,25(5):465～490
[14] 贾承造,魏国齐,李本亮.中国中西部燕山期构造特征及其油气地质意义[J].石油与天然气地质,2005,26(1):9～15
[15] 曲晓明,辛洪波.藏西班公湖斑岩铜矿带的形成时代与成矿构造环境[J].地质通报,2006,5(7):792～799
[16] 陈奇,谢琳,肖志坚.青藏高原西部班公湖蛇绿混杂岩带的基本特征与构造演化[J].华东理工学院学报,2007,30(2):107～ 112
[17] 张志诚,郭召杰,韩作振.敦煌盆地中侏罗世火山岩的地球化学特征及其地质意义[J].北京大学学报(自然科学版),1998,34(1):72～79
[18] 崔俊,陈登钱,姚熙海.柴达木冷湖地区侏罗纪火山活动浅析[J].青海石油,2004,22(1):17～20
[19] 罗金海,车自成,周新源,等.塔里木盆地西部中生代早期伸展作用的辉绿岩证据[J].中国地质,2006,33(3):566～571
[20] 王根厚,梁定益,张维杰,等.藏东北构造古地理特征及冈瓦纳北界的时空转换[J].地质通报,2007,26(8):921～928
[21] 卢书炜,任建德,白国典,等.西藏尼玛县南部中晚侏罗世松木果强过铝花岗岩带的发现及其意义[J].中国地质,2006,33(2):332～339
[22] 钟华明,童劲松,鲁如魁,等.西藏日土北部松西-胜利山一带燕山期高钾钙碱性花岗岩的地球化学特征及构造环境[J].地质通报,2007,26(6):730～738
[23] 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(1):223～227
[24] 周路,郑金云,雷德文,等.准噶尔盆地车莫古隆起侏罗系剥蚀厚度恢复[J].古地理学报,2007,9(3):243～252
[25] 张传恒,刘典波,张传林,等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1):294～302
[26] 李忠,郭宏,王道轩,等.库车坳陷-天山中、新生代构造转折的砂岩碎屑与地球化学记录[J].中国科学(D辑),2005,35(1):15～28
[27] 方世虎,郭召杰,贾承造,等.准噶尔盆地南缘中-新生界沉积物重矿物分析与盆山格局演化[J].地质科学,2006,41(4):648～662
[28] 沈传波,梅廉夫,刘麟,等.新疆博格达山中新生代隆升-热历史的裂变径迹记录[J].海洋地质与第四纪地质,2006,26(3):87～92
[29] 杜治利,王清晨.中新生代天山地区隆升历史的裂变径迹证据[J].地质学报,2007,81(8):1 081～1 101
[30] 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
[31] 柳益群,吴涛.新疆吐鲁番-哈密盆地的古地温梯度及地质热历史[J].中国科学(D辑),1997,27(5):431～436
[32] 雷刚林,谢会文,张敬洲,等.库车坳陷克拉苏构造带构造特征及天然气勘探[J].石油与天然气地质,2007,28(6):816～820,835
[33] 丁道桂,刘伟新,崔可锐,等.塔里木中-新生代前陆盆地构造分析与油气领域[J].石油实验地质,1997,19(2):97～107
[34] 何光玉,卢华复,李树新.库车盆地秋里塔格构造带构造圈闭及油气勘探方向[J].地质科学,2003,38(4):506～513
[35] 姚亚明,刘池阳,何明喜,等.焉耆盆地博湖坳陷油气成藏的主控因素及成藏模式[J].新疆石油天然气,2005,1(3):1～6
[36] 李平平,邹华耀,郝芳.准噶尔盆地腹部侏罗系顶部风化壳的发育机制及其油气成藏效应[J].沉积学报,2006,24(6):889～ 895
[37] 万桂梅,汤良杰,金文正,等.库车坳陷西部构造圈闭形成期与烃源岩生烃期匹配关系探讨[J].地质学报,2007,81(2):187～ 196
[38] 李洪铎,艾华国.不整合面上下部的储盖组合——塔里木盆地油气成藏的关键因素[J].中国西部油气地质,2006,2(4):390～394
[39] 洪太元,蔡希源,何治亮,等.准噶尔盆地腹部白垩系底部不整合的控油作用[J].新疆地质,2007,25(1):87～91

The Yanshanian movement and its control over hydrocarbon accumulation in western China

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