西昆仑山前柯东构造带变形特征、机制及物理模拟

龚艳萍; 尹宏伟; 汪新; 梁瀚

doi:10.11781/sysydz201403299

西昆仑山前柯东构造带变形特征、机制及物理模拟

doi: 10.11781/sysydz201403299

1.
南京大学地球科学与工程学院, 南京 210093
2. 中海石油有限公司深圳分公司, 广州 510220
3. 浙江大学地球科学系, 杭州 310027

基金项目: 国家自然科学基金项目（40872134，41272227）和国家油气专项（2011ZX05009-001）资助。

详细信息

作者简介:
龚艳萍（1989—）,女,硕士,从事构造地质与应用地球物理研究。E-mail: gongyp123@163.com。

中图分类号: TE121.2
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- 被引次数: 0
出版历程
- 收稿日期: 2013-02-01
- 修回日期: 2014-03-28
- 刊出日期: 2014-05-28

Structural deformation characteristics, mechanics and physical modeling of Kedong structure in piedmont of western Kunlun Mountain

1.
School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210093, China
2. CNOOC Shenzhen Branch Company, Guangzhou, Guangdong 510220, China
3. Department of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China

摘要

摘要: 柯东构造带地处西昆仑造山带前缘，构造演化受到西昆仑山隆升的重要影响，变形主要发生在新近纪—第四纪。地震资料显示，该区深部变形以逆冲叠瓦断层的发育为特点，浅部为一套北倾新生界地层为主的单斜层。采用构造物理模拟方法对柯东构造带的构造变形演化过程和变形机制进行了分析，研究结果表明，柯东构造带变形主要受由南往北的区域挤压、剥蚀作用、同构造沉积作用等因素影响。古近系膏岩层和侏罗系煤系地层组成的区域上的复合滑脱层，控制了该区深浅构造脱耦与差异性演化。
- 物理模拟 /
- 变形机制 /
- 柯东构造带 /
- 西昆仑山
Abstract: The Kedong structure locates in the front of the western Kunlun orogenic belt and was impacted signi-ficantly by the uplift of the western Kunlun Mountain. Deformations took place mainly in Neogene and Quaternary. Seismic data showed that the deformations in deep series were featured by thrust and imbricate faults, while in the shallow series a set of Cenozoic monoclines inclined to the north developed. The structural deformation process and mechanism of the Kedong structure were analyzed with physical simulation. It was concluded that the Kedong structure was mainly controlled by compression from south to north, erosion and synkinematic sedimentation. Paleogene evaporate bed and Jurassic coal-series stratum worked as regional composite detachment and controlled the decoupling and differential evolution of the upper and lower structures.
- physical modeling /
- deformation mechanics /
- Kedong structure /
- western Kunlun Mountain

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参考文献(15)

[1]	陈杰,卢演俦,丁国瑜.塔里木西缘晚新生代造山过程的记录:磨拉石建造及生长地层和生长不整合[J].第四纪研究,2001,21(6):528-539. Chen Jie,Lu Yanchou,Ding Guoyu.Records of late Cenozoic mountain building western Tarim Basin:molasses,growth strata and growth unconformity[J].Quaternary Sciences,2001,21(6):528-539.
[2]	Zheng H,Powell C,An Z,et al.Pliocene uplift of the northern Tibetan Plateau[J].Geology,2000,28(8):715-718.
[3]	刘函,王国灿,曹凯,等.西昆仑及邻区区域构造演化的碎屑锆石裂变径迹年龄纪录[J].地学前缘,2010,17(3):64-78. Liu Han,Wang Guocan,Cao Kai,et al.The detrital zircon fission-track ages constraint to tectonic processes in west Kunlun and adjacent regions[J].Earth Science Frontiers,2010,17(3):64-78.
[4]	伍秀芳,刘胜,汪新,等.帕米尔—西昆仑北麓新生代前陆褶皱冲断带构造剖面分析[J].地质科学,2004,39(2):260-271. Wu Xiufang,Liu Sheng,Wang Xin,et al.Analysis on structural sections in the Cenozoic Pamir-western Kunlun foreland fold-and-thrust belt[J].Chinese Journal of Geology,2004,39(2):260-271.
[5]	杨海军,王步清,杨芝林,等.塔里木盆地西南坳陷柯东构造建模与油气勘探[J].地质科学,2011,46(2):456-465. Yang Haijun,Wang Buqing,Yang Zhilin,et al.Structure modeling and hydrocarbon exploration of Kedong structural belt in southwestern Tarim Basin[J].Chinese Journal of Geology,2011,46(2):456-465.
[6]	程晓敢,雷刚林,陈汉林,等.西昆仑山前甫沙—克里阳地区新生代变形特征及油气控制作用[J].石油学报,2011,32(1):83-89. Cheng Xiaogan,Lei Ganglin,Chen Hanlin,et al.Cenozoic structural deformation of the Fusha-Keliyang area in the piedmont of the western Kunlun Mountains and its control on hydrocarbon accumulation[J].Acta Petrolei Sinica,2011,32(1):83-89.
[7]	张玮,漆家福,雷刚林,等.塔西南拗陷甫沙构造带结构模型及形成机制[J].西南石油大学学报:自然科学版,2011,33(1):42-48. Zhang Wei,Qi Jiafu,Lei Ganglin,et al.Analysis of structure model and formation mechanism of Fusha structure zone in south-western depression of Tarim Basin[J].Journal of Southwest Petroleum University:Science & Technology Edition,2011,33(1):42-48.
[8]	张国清,吴晓智,唐勇.塔西南甫沙—克里阳地区盆山接触带构造特征及油气勘探有利区带[J].新疆石油地质,2000,21(6):459-461,486. Zhang Guoqing,Wu Xiaozhi,Tang Yong.Basin-mountain structural features and favorable play in the Fusha-Keliyang area in southwestern Tarim Basin[J].Xinjiang Petroleum Geology,2000,21(6):459-461,486.
[9]	梁瀚,杜治利,王宇,等.西昆仑山前东段新生代褶皱冲断带及其锥形楔机制[J].地质科学,2012,47(3):808-823. Liang Han,Du Zhili,Wang Yu,et al.Cenozoic fold and thrust belt in eastern section of the piedmount of west Kunlun and its taper wedge mechanics[J].Chinese Journal of Geology,2012,47(3):808-823.
[10]	邢厚松,李君,孙海云,等.塔里木盆地塔西南与库车山前带油气成藏差异性研究及勘探建议[J].天然气地质科学,2012,23(1):36-45. Xing Housong,Li Jun,Sun Haiyun,et al.Differences of hydrocarbon reservoir forming between Southwestern Tarim Basin and Kuche Mountain Front[J].Natural Gas Geoscience,2012,23(1):36-45.
[11]	Vendeville B C,Jackson M P A.The fall of diapirs during thin-skinned extension[J].Marine and Petroleum Geology,1992,9(8):354-371
[12]	Vendeville B C,Jackson M P A.The rise of diapirs during thin-skinned extension[J].Marine and Petroleum Geology,1992,9(4):331-353.
[13]	Hubert M K.Theory of scale models as applied to the study of geologic structures[J].Bulletin of the Geological Society of America,1937,48(10):1459-1520.
[14]	何登发,Suppe J,贾承造.断层相关褶皱理论与应用研究新进展[J].地学前缘,2005,12(4):353-364. He Dengfa,Suppe J,Jia Chengzao.New advances in theory and application of fault-related folding[J].Earth Science Frontiers,2005,12(4):353-364.
[15]	刘玉萍,尹宏伟,张洁,等.褶皱—冲断体系双层滑脱构造变形物理模拟实验[J].石油实验地质,2008,30(4):424-428. Liu Yuping,Yin Hongwei,Zhang Jie,et al.Physical modeling on double decollements structure in fold-and-thrust belt[J].Petroleum Geology & Experiment,2008,30(4):424-428.