STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN

LI Le; HOU Gui-ting; PAN Wen-qing; JU Yan; ZHANG Qing-lian; SHU Wu-lin; XIAO Fang-feng; JU Wei

2011 Vol. 17, No. 3

Article Contents

Article navigation > Journal of Geomechanics > 2011 > 17(3): 262-273

Next Article Previous Article

LI Le, HOU Gui-ting, PAN Wen-qing, JU Yan, ZHANG Qing-lian, SHU Wu-lin, XIAO Fang-feng, JU Wei. STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN[J]. Journal of Geomechanics, 2011, 17(3): 262-273.

Citation:

LI Le, HOU Gui-ting, PAN Wen-qing, JU Yan, ZHANG Qing-lian, SHU Wu-lin, XIAO Fang-feng, JU Wei. STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN[J]. Journal of Geomechanics, 2011, 17(3): 262-273.

STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN

1.
School of Earth and Space Science, Peking University, Beijing 100871, China
2.
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Beijing 100871, China
3.
Institute of Oil and Gas Research, Peking University, Beijing 100871
4.
Institute of Exploration and Development, Tarim Oil and Gas Branch Company, Korla 841000, Xinjiang, China

More Information

Corresponding author: LI Le, ye41lile@163.com

Received Date: 22 March 2011

Publish Date: 25 September 2011

Abstract

Abstract

Three periods of structural stress fields can be recognized since Permian in northwest of Tarim Basin and adjacent areas based on structural evolution analysis, which is the end of Permian, the Triassic to paleogene and Neogene. Based on the research of stress-response structures of dykes, joints, slickensides, folds and faults, and analysis of the comparison characters of field of stress, it is found that the direction of the maximum principal stress formed by the collision of middle Tianshan island arc and Tarim basin was NW. The direction of maximum principal stress Triassic to paleogene was NNE, which developed by repression of dextrorotary of Tarim basin. And it was N-S direction since Neogene in Bachu area as a result of the collision of Indian plate with Eurasian plate. Furthermore, the authors simulated the stress field since Neogene based on 2D finite-element method, to deeply analyze the distribution and direction of stresses in the research area.
- Tarim Basin /
- Bachu area /
- structural stress fields /
- maximum principal stress

FullText(HTML)

References

[1]	王延欣, 侯贵廷, 李江海, 等.塔北隆起中西部新近纪末构造应力场数值模拟[J].北京大学学报:自然科学版, 2008, 44 (6):902~908. Google Scholar WANG Yan-xin, HOU Gui-ting, LI Jiang-hai, et al. Numercial simulation of tenconic stress field at the end of Neocene in the midwest of northern Tarim Basin[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2008, 44 (6):902~908. Google Scholar
[2]	杨庚, 郭华.塔里木盆地西北缘柯坪逆冲构造带与巴楚隆起的叠加关系[J].铀矿地质, 2003, 19 (1):1~7. Google Scholar YANG Geng, GUO Hua. Superposed relationship between Kalping thrust belt and Bachu uplift, northwest Tarim[J]. Uranium Geology, 2003, 19 (1):1~7. Google Scholar
[3]	杨庚, 石昕, 贾承造, 等.塔里木盆地西北缘柯坪—巴楚地区皮羌断裂与色力布亚断裂空间关系[J].铀矿地质, 2008, 24 (4):201~205. Google Scholar YANG Geng, SHI Xin, JIA Cheng~zao, et al. Spatial relationship between Piqiang fault and Selibuya fault in Keping-Bachu district, northwest Tarim basin[J]. Uranium Geology, 2008, 24 (4):201~205. Google Scholar
[4]	张臣, 郑多明, 李江海.柯坪断隆古生代的构造属性及其演化特征[J].石油与天然气地质, 2001, 22 (4):314~318. doi: 10.11743/ogg20010406 CrossRef Google Scholar ZHANG Chen, ZHENG Duo-ming, LI Jiang-hai. Attribute of Paleozoic structures and its evolution characteristics in Keping fault-uplift[J]. Oil & Gas Geology. 2001, 22 (4):314~318. doi: 10.11743/ogg20010406 CrossRef Google Scholar
[5]	陈杨. 塔里木盆地巴楚隆起构造演化与含油气关系研究[D]. 四川: 成都理工大学, 2007.http://cdmd.cnki.com.cn/article/cdmd-10616-2007138740.htm Google Scholar CHEN Yang. Analasis of Relationship between tectonic evolution and oil-gas in Bachu uplift in Tarim Basin[D]. Chengdu University of Technology, 2007. Google Scholar
[6]	万天丰.古构造应力场[M].北京:地质出版社, 1988: 4~10. Google Scholar WAN Tian-nian. Paleotectonic stress field[M]. Beijing: Geological Publishing House, 1988: 4~10. Google Scholar
[7]	肖芳锋, 侯贵廷, 王延欣, 等.准噶尔盆地及周缘二叠纪以来构造应力场解析[J].北京大学学报:自然科学版, 2010, 46 (2):224~230. Google Scholar XIAO Fang-feng, HOU Gui-ting, WANG Yan-xin, et al. Study on structural stress fields since Permian Junggar Basin and adjacent areas[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2010, 46 (2):224~230. Google Scholar
[8]	王宏强. 鄂尔多斯中生代盆地构造应力场特征及其转换与沉积-构造格局[D]. 西安: 西北大学, 2001.http://cdmd.cnki.com.cn/Article/CDMD-10697-2001011017.htm Google Scholar ANG Hong-qiang. Tectonic stress field characteristics and its transition laws and tectonic-sedimentary framework in Mesozoic Ordos Basin[D]. Xi' an: Northwest University, 2001. Google Scholar
[9]	操成杰. 川西北地区构造应力场分析与应用[D]. 北京: 中国地质科学院, 2005.http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y712742 Google Scholar CAO Cheng-jie. Tectonic Stress Field Analysis and Application in the Northwest Sichuan Basin[D]. Beijing: Chinese Academy of Geological Sciences, 2005. Google Scholar
[10]	马宗晋, 邓启东.节理力学性质的判别及其分期、配套的初步研究[M].北京:科学出版社, 1965: 15~30. Google Scholar MA Zong-jin, Deng Qi-dong. Study on judgement, major division of geological time、mating of mechanical property of joints [M]. Beijing: Science Press, 1965, 15~30. Google Scholar
[11]	侯贵廷, 张臣, 钱祥麟, 等.华北克拉通中元古代基性岩墙群形成机制及构造应力场[J].地质论评, 1998, 44 (3):309~314. Google Scholar HOU Gui-ting, ZHANG Chen, QIAN Xiang-lin, et, al. The formation mechanism and tectonic stress field of the Mesoproterozoic mafic dike swarms in the North China Craton[J]. Geological Review, 1998, 44 (3):309~314. Google Scholar
[12]	侯贵廷, 李江海, 金爱文, 等.鲁西前寒武纪基性岩墙群[J].地质学报, 2005, 79 (2):190~200. Google Scholar HOU Gui-ting, LI Jiang-hai, JIN Ai-wen, et al. The Precambrian basic dyke swarms in the western Shandong Province [J]. Acta Geologica Sinica, 2005, 79 (2):190~200. Google Scholar
[13]	Hou, Guiting, Liu, Yulin, Li, Jianghai, Qian, Xianglin. The evidence of 1. 8 Ga extension of North China Craton from the mafic dyke in Shandong Province, Eastern Block[J]. Journal of Asian Earth Science, 2006, 27 (4):392~401. doi: 10.1016/j.jseaes.2005.05.001 CrossRef Google Scholar
[14]	邵济安, 张履桥, 魏春景, 等.北京南口中生代双峰式岩墙群的组成及其特征[J].地质学报, 2001, 75 (2):205~212. Google Scholar SHAO Ji-an, ZHANG Lu-qiao, WEI Chun-jing, et al. Composition and features of the Mesozoic bimodal dike swarm in Nankou area, Beijing[J]. Acta Geologica Sinica, 2001, 75 (2):205~212. Google Scholar
[15]	张自力, 秦其明, 田伟, 等.塔里木麻扎尔塔格基性岩墙群的侵位特征和空间分布规律研究[J].岩石学报, 2008, 24 (10):2273~2280. Google Scholar ZHANG Zi-li, QIN Qi-ming, TIAN Wei, et al. Emplacement characteristics and spatial distribution of Permian Mazhartager basic dike swarms in Bachu area, Tarim basin[J]. Acta Petrologica Sinica, 2008, 24 (10):2273~2280. Google Scholar
[16]	杨树锋, 厉子龙, 陈汉林, 等.塔里木二叠纪石英正长斑岩岩墙的发现及其构造意义[J].岩石学报, 2006, 22 (5):1405~1412. Google Scholar YANG Shu-feng, LI Zi-long, CHEN Han-lin, et al. Discovery of a Permian quartz syenitic porphyritic dyke from the Tarim Basin and its tectonic implications[J]. Acta Petrologica Sinica, 2006, 22 (5):1405~1412. Google Scholar
[17]	李勇, 苏文, 孔屏, 等.塔里木盆地塔中-巴楚地区早二叠世岩浆岩的LA-ICP-MS锆石U-Pb年龄[J].岩石学报, 2007, 23 (5):1097~1107. Google Scholar LI Yong, SU Wen, KONG Ping, et al. Zircon U-Pb ages of the Early Permian magmatic rocks in the Tazhong-Bachu region, Tarim Basin by LA-ICP-MS[J]. Acta Petrologica Sinica, 2007, 23 (5):1097~1107. Google Scholar
[18]	孙林华, 王岳军, 范蔚茗, 等.新疆巴楚辉绿岩岩脉的岩石成因和大地构造意义[J].岩石学报, 2007, 23 (6):1369~1380. Google Scholar SUN Lin-hua, WANG Yue-jun, FAN Wei-ming, et al. Petrogenesis and tectonic significances of the diabase dikes in the Bachu area, Xinjiang[J]. Acta Petrologica Sinica, 2007, 23 (6):1369~1380. Google Scholar
[19]	ZHANG Zhi-cheng, GUO Zhao-jie, LIU Shu-wen. Age and tectonic significance of the mafic dyke swarm in the Kuruktag region, Xinjiang[J]. Acta Geologica Sinica, 1998, 72 (1):29~36. doi: 10.1111/acgs.1998.72.issue-1 CrossRef Google Scholar
[20]	刘玉琳, 张志诚, 郭召杰, 等.库鲁克塔格基性岩墙群K-Ar等时年龄测定及其有关问题讨论[J].高校地质学报, 1999, 5 (1):54~58. Google Scholar LIU Yu-lin, ZHANG Zhi-cheng, GUO Zhao-jie, et al. K-Ar isochron dating of Kuluktag mafic dykes, Xinjiang Autonomous region, and discussion on some related questions[J]. Geological Journal of China Universities, 1999, 5 (1):54~58. Google Scholar
[21]	肖序常.新疆北部及其邻区大地构造[M].北京:地质出版社, 1992. Google Scholar XIAO Xu-chang. Tectonic evolution of northern Xinjiang and its adjacent regions[M]. Beijing: Geological Publishing House, 1992. Google Scholar
[22]	戴俊生.构造地质学及大地构造[M].北京:石油工业出版社, 2006. Google Scholar DAI Jun-sheng. Structural geology and tectonics[M]. Beijing: Petroleum Industry Press, 2006. Google Scholar
[23]	王喜双, 李晋超, 王邵民, 等.塔里木盆地构造应力场与油气聚集[J].石油学报, 1997, 3: 77~82. Google Scholar WANG Xi-shuang, LI Jin-chao, WANG Shao-min, et al. Oil and gas accumulation and structural stress field in Tarim basin [J]. Acta Petrolei Sinica.. 1997, 3: 77~82. Google Scholar
[24]	马宗晋, 邓启东.节理力学性质的判别及其分期、配套初步研究[M].北京:科学出版社, 1965: 15~30.划分. Google Scholar MA Jin-chao, DENG Qi-dong. Preliminary study on mechanical property discrimination, stage division and system division of joints[M]. Beijing: Science Press, 1965: 15~30. Google Scholar
[25]	何绍勋.构造地质学中的赤平极射投影[M].北京:地质出版社, 1997. Google Scholar HE Shao-xun. Stereographic projection in structural geology[M]. Beijing: Geological Publishing House, 1997. Google Scholar
[26]	曲国胜, 李亦纲, 陈杰, 等.柯坪塔格推覆构造几何学、运动学及其构造演化[J].地学前缘, 2003, 10 (特):142~152. Google Scholar QU Guo-sheng, LI Yi-gang, CHEN Jie, et al. Geometry, Kinematics and tectonic evolution of Kepingtage thrust system [J]. Earth Science Frontiers. 2003, 10 (Supp.):142~152. Google Scholar
[27]	马德明, 陈江力, 曾昌民, 等.塔里木盆地西北缘柯坪冲断带的构造变形特征[J].地质力学学报, 2007, 13 (4):340~347. Google Scholar MA De-ming, CHEN Jiang-li, ZENG Chang-min, et al. Structural deformation characteristics of the Kalpin thrust belt on the northwestern margin of the Tarim basin[J]. Journal of Geomechanics, 2007, 13 (4):340~347. Google Scholar
[28]	何文渊, 李江海, 钱祥麟, 等.塔里木盆地巴楚断隆中新生代的构造演化[J].北京大学学报:自然科学版, 2000, 36 (4):539~546. Google Scholar HE Wen-yuan, LI Jiang-hai, Qian Xiang-lin, et al. The Meso-Cenozoic evolution of Bachu fault-uplift in Tarim Basin[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2000, 36 (4):539~546. Google Scholar
[29]	高国英, 温和平.帕米尔东北侧现代构造应力场与地震活动特征研究[J].中国地震, 2000, 16 (2):176~184. Google Scholar GAO Guo-ying, WEN He-ping. Recent tectonic stress field and seismicity of northeast Pamir[J]. Earthquake Research in China, 2000, 16 (2):176~184. Google Scholar
[30]	崔效锋.伽师及周围地区现代构造应力场特征研究[J].地震学报, 2006, 28 (4):347~356. Google Scholar CUI Xiao-feng. Characteristics of recent tectonic stress field in Jiashi, Xinjiang and adjacent regions[J]. Acta Seismologica Sinica, 2006, 28 (4):347~356. Google Scholar
[31]	王盛泽, 高国英.新疆及其邻近地区现代构造应力场的区域特征[J].地震学报, 1992, 14 (增):612~620. Google Scholar WANG Sheng-ze, GAO Guo-ying. Regional characteristics of recent tectonic stress field in Xinjiang and adjacent regions [J]. Acta Seismologica Sinica, 1992, 14 (Supp.):612~620. Google Scholar
[32]	赵明, 孙兆于, 岳勇, 等.巴楚隆起西段色力布亚断裂演化及其封闭性研究[J].石油天然气学报, 2008, 30 (4):28~32. Google Scholar ZHAO Ming, SUN Zhao-yu, YUE Yong, et al. Evolution and sealing research of Selibuya Fault in the west of Bachu uplift [J]. Journal of Oil and Gas Technology, 2008, 30 (4):28~32. Google Scholar