天山南北前陆盆地冲断带沉积砂体对构造逆冲作用响应动力学

doi:10.11743/ogg20130217

Abstract

Abstract:

A brief analysis of vertical uplifting height and horizontal shortening on the thrust belt in foreland basins of the central and western China reveals that there are two types of forces that controlled the deposition of thrusting belt,one is the horizontal progress force and the other is the vertical uplifting force.The vertical lifting force gave birth to thrust faults.The vertical displacement by the force resulted in the uplifting of mountains and lowering of basins the thrust faults and created accommodation.The horizontal progress force generated strike-slip faults.The horizontal displacement by the force pushed mountains and provenance forward.Based on this understanding,the thrusting during the Paleogene-Neogene in southern margin of Junggar and Kuqa foreland basins can be divided into 5 stages that correspond to three sets of coarse grain deposits and two sets of fine grain deposits respectively.Among them,the conglomerate at the bottom of the Palaeogene was the product of terrigenous clastic deposition in the stage dominated by horizontal progress force (together with auxiliary vertical uplifting force) and also marks the existence of a over-thrusting in the early Himalaya movement;the conglomeratic coarse-grained deposits at the bottom of the Neogene were the result of thrusting under the dominant horizontal progress force in the early thrusting loading period and also marks the renewal activity of over-thrusting during the early-middle Himalaya orogeny;and the conglomeratic coarse-grained deposits at the bottom of the Kuqa-Dushangzi Formation at the top of Neogene were formed during the middle-late Himalaya orogeny when the base rebound and provide large amount of sediments and caused sandbody progradation under horizontal progress force.While another two sets of Paleogene and Neogene lacustrine mudstone deposits were formed in a period with vertical uplifting force predominant when mountain uplifting caused piedmont flexural subsidence being enhanced and lake level rising.

Key words: thrusting, sedimentary response, thrust belt of foreland basins, Paleogene, Neogene, southern and northern Tianshan

CLC Number:

TE121

Gao Zhiyong, Feng Jiarui, Li Xiaopei, Zhao Xuesong, Guo Meili, Mei Jialuo. Kinetics of sedimentary process response to thrusting in the thrust belts of foreland basins in southern and northern Tianshan[J]. Oil & Gas Geology, 2013, 34(2): 248-256.

References

[1] Posamentier H W,Allen G P.Siliciclastic sequence stratigraphic patterns in foreland ramp-type basins[J].Geology,1993,21:455-458.
[2] Quinlan G M,Beaumont C.Appalachian thrusting,lithospheric fle-xure and Paleozoic st ratigraphy of eastern interior of North America[J].Canadian Journal of Earth Sciences,1984,21:973-996.
[3] Beaumont C,Quinlan G M,Hamilton J.Orogeny and st ratigraphy:numeral model of the Paleozoic in the eastern interior of North American[J].Tectonics,1988,7 (3):389-416.
[4] 刘少峰.前陆盆地几种构造-沉积演化模式综述[J].地质科技情报,1991,10(4):39-44. Liu Shaofeng.Several types of tectono-depositional evolusion models of foreland basins[J].Geological Science and Technology Information,1991,10(4):39-44.
[5] 刘少峰.前陆盆地的形成机制和充填演化[J].地球科学进展,1993,8(4):30-37. Liu Shaofeng.Forming-mechanism and filling-evolution of foreland basins[J].Advance in Earth Science,1993,8(4):30-37.
[6] 刘少峰.前陆盆地挠曲过程模拟的理论模型[J].地学前缘,1995,2(3-4):69-77. Liu Shaofeng.The theoretical models for simulating the flexural process of foreland basin[J].Earth Science Frontiers,1995,2(3-4):69-77.
[7] 张明山,钱祥麟,李茂松.造山带逆冲与前陆盆地沉降和沉积平衡关系的定量讨论——以库车陆内前陆盆地为例[J].北京大学学报(自然科学版),1996,32(2):188-198. Zhang Mingshan,Qian Xianglin,Li Maosong.A quantitative discussion to the relationship between thrusting of orogenic belt andsubsi-dence and sedimentation of foreland basin-Kuche intracontinental foreland basin as an example[J].Acta Scientiarum Naturalium,1996,32(2):188-198.
[8] 王家豪,王华,陈红汉,等.一幕完整的前陆盆地构造演化的地层记录:库车坳陷下白垩统[J].地质科技情报,2006,25(6):31-36. Wang Jiahao,Wang Hua,Chen Honghan,et al,Zhao Zhongxin.Stratigraphic record in a whole episode of foreland basin tectonic evolution:the Lower Cretaceous in Kuqa Depression[J].Geological Science and Technology Information,2006,25(6):31-36.
[9] 顾家裕,张兴阳.中国西部陆内前陆盆地沉积特征与层序格架[J].沉积学报,2005,23(2):187-193. Gu Jiayu,Zhang Xingyang.Sedimentary characteristics and sequence framework of intracontinental foreland basin in the western China[J].Acta Sedimentologica Sinica,2005,23(2):187-193.
[10] 贾承造,何登发,陆洁民.中国喜马拉雅运动的期次及其动力学背景[J].石油与天然气地质,2004,25(2):121-125. Jia Chengzao,He Dengfa,Lu Jiemin.Episodes and geodynamic setting of Himalayan movement in China[J].Oil & Gas Geology,2004,25(2):121-125.
[11] 彭希龄,梁狄刚,王昌桂,等.前陆盆地理论及其在中国的应用[J].石油学报,2006,27(1):132-244. Peng Xiling,Liang Digang,Wang Changgui,et al.Discussion on the theory of foreland basin and its application in China[J].Acta Petrolei Sinica,2006,27(1):132-244.
[12] 陈新,卢华复,舒良树,等.准噶尔盆地构造演化分析新进展[J].高校地质学报,2002,8(3):257-267. Chen Xin,Lu Huafu,Shu Liangshu,et al.Study on tectonic evolution of Junggar Basin[J].Geological Journal of China Universities,2002,8(3):257-267.
[13] 贾承造.中国喜马拉雅构造运动的陆内变形特征与油气矿藏富集[J].地学前缘,2007,14(4):96-104. Jia Chengzao.The characteristics of intra-continental deformation and hydrocarbon distribution controlled by the Himalayan tectonic movements in China[J].Earth Science Frontiers,2007,14(4):96-104.
[14] 彭天令,阎桂华,陈伟,等.准噶尔盆地南缘霍玛吐构造带特征[J].新疆石油地质,2008,29(2):191-194. Peng Tianling,Yan Guihua,Chen Wei,et al.Characteristics of Huoer-guosi-Manasi-Tugulu structural belt inJunggar Basin[J].Xinjiang Petroleum Geology,2008,29(2):191-194.
[15] 万里皋,刘登明,侯六根.准噶尔盆地南缘前陆冲断带构造特征研究[J].石油地球物理勘探,2005,40(增刊):40-45. Wan Ligao,Liu Dengming,Hou Liugen.Structure feature of foreland thrust-fold belts in the southern edge of Junggar Basin[J].Oil Geophysical Prospecting,2005,40(S1):40-45.
[16] 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):1081-1101. Du Zhili,Wang Qingchen.Mesozoic and Cenozoic uplifting history of the Tianshan region: insight from apatite fission track[J].Acta Geologica Sinica,2007,81(8):1081-1101.
[17] 王清晨,张仲培,林伟.库车盆地-天山边界的晚第三纪断层活动性质与应力状态[J].科学通报,2003,48(24):2553-2559. Wang Qingchen,Zhang Zhongpei,Lin Wei.The Paleogene fault acti-vities and stress in the Kuqa Basin to the boundary of Tianshan[J].Chinese Science Bulletin,2003,48(24):2553-2559.
[18] 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. Xu Zhiqin,Yang Jingsui,Jiang Mei,et al.Continental subduction and uplifting of the orogenic belts at the margin of the Qinghai-Tibet pla-teau[J].Earth Science Frontiers,1999,6(3):139-151.
[19] 漆家福,雷刚林,李明刚,等.库车坳陷克拉苏构造带的结构模型及其形成机制[J].大地构造与成矿学,2009,33(1):49-56. Qi Jiafu,Lei Ganglin,Li Minggang,et al.Analysis ofstructure model and formation mechanism of Kelasu sructure zone,Kuqa depression[J].Geotecton ica et Metallogenia,2009,33(1):49-56.
[20] 张锐,郭召杰,张志诚,等.天山北麓晚新生代独山子-安集海褶皱冲断带构造分析及其对河流改道的影响[J].新疆地质,2005,23(3):215-219. Zhang Rui,Guo Zhaojie,Zhang Zhicheng,et al.Structural analysis of the Dushanzi-Anjihai late Cenozoic fold-thrust belt and its influence on river channels,North Tianshan[J].Xinjiang Geology,2005,23(3):215-219.
[21] 方世虎,郭召杰,张志诚,等.中新生代天山及其两侧盆地性质与演化[J].北京大学学报(自然科学版),2004,40(6):886-897. Fang Shihu,Guo Zhaojie,Zhang Zhicheng,et al.Discussion on Mesozoic-Cenozoic evolution of Tian Shan and its adjacent basins[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2004,40(6):886-897.
[22] 杨晓平,陈立春,李安,等.西南天山阿图什背斜晚第四纪的阶段性隆升[J].地学前缘,2009,16(3):160-170. Yang Xiaoping,Chen Lichun,Li An,et al.The uplifting of Artux anticline by stages in the Late Quaternary,Southwest Tianshan[J]. Earth Science Frontiers,2009,16(3):160-170.
[23] 李海兵,王宗秀,付小芳,等.2008年5月12日汶川地震(Ms8.0)地表破裂带的分布特征[J].中国地质,2008,35(5):803-813. Li Haibing,Wang Zongxiu,Fu Xiaofang,et al.The surface rupture zone distribution of the Wenchuan earthquake (Ms 8.0) happened on May 12^th,2008[J].Geology of China,2008,35(5):803-813.
[24] Gao Zhiyong,Guo Hongli,Zhu Rukai,et al.Sedimentary response of different fan types to the Paleogene-Neogene basin transformation in the Kuqa depression,Tarim basin,Xinjiang Province[J].Acta Geologica Sinica,2009,83(2):411-424.
[25] 徐纪人,赵志新.汶川8.0级大地震震源机制与构造运动特征[J].中国地质.2010,37(4):967-977. Xu Jiren,Zhao Zhixin.Causative mechanism and related tectonic movement of the 2008 Wenchuan M8 Earthquake[J].Geology of China,2010,37(4):967-977.
[26] 史兴民,李有利,杨景春,等.新疆玛纳斯河山前地貌对构造活动的响应[J].地质学报,2008,82(2):281-288. Shi Xingmin,Li Youli,Yang Jingchun,et al.Response of the Foreland of the Manas River to the tectonic movement in Xinjiang uygu rautonomous region[J].Acta Geologica Sinica,2008,82(2):281-288.
[27] 何光玉,卢华复,杨树锋,等.库车中新生代盆地沉降特征[J].浙江大学学报(理学版),2004,31(1):110-113. He Guangyu,Lu Huafu,Yang Shufeng,et al.Subsiding features of the Mesozoic and Cenozoic Kuqa Basin,Northwestern China[J].Journal of Zhejiang University (Science Edition),2004,31(1):110-113.
[28] 彭守涛,宋海明.库车坳陷北部白垩系沉积速率分析[J].沉积学报,2006,24(5):641-649. Peng Shoutao,Song Haiming.The sedimentation rates analysis of cretaceous depositional succession in the Northern Kuqa depression,Northwest China[J].Acta Sedimentologica Sinica,2006,24(5):641-649.
[29] 阎福礼,卢华复,贾东,等.塔里木盆地库车坳陷中、新生代沉降特征探讨[J].南京大学学报(自然科学),2003,39(1):31-39. Yan Fuli,Lu Huafu,Jia Dong,et al.The Meso-Cenozoic Subsidence Features of Kuqa Depression,Tarim Basin[J].Journal of Nanjing University(Nateural Sciences),2003,39(1):31-39.
[30] 张明山.陆内挤压造山带与陆内前陆盆地关系——以塔里木盆地北部与南天山为例[J].现代地质,1997,11(4):461-469. Zhang Mingshan.Relationship between intracontinental compressional orogenic belts and intracontinental foreland basins—a example of northern tarim and southern Tianshan[J].Geosciences,1997,11(4):461-469.
[31] 吕嵘,汪新文,沈勇伟.准噶尔盆地南缘中新生代构造沉降史分析[J].石油天然气学报(江汉石油学院学报),2006,28(5):10-12. Lü Rong,Wang Xinwen,Shen Yongwei.Analysis oftectonic subsi-dence evolution of Mesozoic-Cenozoic in southern margin of Junggar Basin[J].Journal of Oil and Gas Technology,2006,28(5):10-12.
[32] 高志勇,韩国猛,朱如凯,等.准噶尔盆地南缘古近纪—新近纪前陆盆地沉积格局与演变[J].古地理学报,2009,11(5):491-502. Gao Zhiyong,Han Guomeng,Zhu Rukai,et al.Depositional setting and evolution of the Paleogene-Neogene foreland basin of southern margin of Junggar Basin[J].Journal of Palaeogeography,2009,11(5):491-502.
[33] 高志勇,胡永军,张莉华,等.准噶尔南缘前陆盆地白垩纪—新近纪构造挤压作用与储层关系的新表征:镜质体反射率与颗粒填集密度[J].中国地质,2010,37(5):1336-1352. Gao Zhiyong,Hu Yongjun,Zhang Lihua,et al.The interpretation of the controlling action of Cretaceous to Tertiary tectonic compression on the reservoir in the southern margin of Junggar Basin:vitrinite reflectance and grain packing density[J].Geology in China,2010,37(5):1336-1352.
[34] 高志勇,郭宏莉,安海亭,等.库车坳陷东部山前带古近系不同体系域内扇三角洲沉积砂体的对比研究[J].地质科学,2008,43(4): 758-776. Gao Zhiyong,Guo Hongli,An Haiting,et al.Paleogene fan-delta sandbodies of different system tracts in foreland of the eastern Kuqa Depression: a comparative study[J].Chinese Journal of Geology,2008,43(4): 758-776.
[35] 刘贻军.前陆盆地层序地层学研究中的几个问题[J].地球学报.1998,19(1):90-96. Liu Yijun.Sequence stratigraphy discussions for research foreland basins[J].Acta Geoscientia Sinica,1998,19(1):90-96.

Kinetics of sedimentary process response to thrusting in the thrust belts of foreland basins in southern and northern Tianshan

PDF (PC)

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 15

Recommended Articles

Metrics

[1]	Ying Chen, Yinxue Han, Lizeng Bian, Qingbo Zeng, Shuai Guo, Mo Ji, Dongsheng Yang, Longying Wang. Difference between eastern and western Paleogene sedimentary systems in deep waters off the northern South China Sea continental margin and its effect on source rock distribution [J]. Oil & Gas Geology, 2020, 41(5): 1028-1037.
[2]	Youlu Jiang, Shengmin Su, Hua Liu, Yongshi Wang, Xiaojun Cui. Differential hydrocarbon enrichment of the Paleogene and its main controlling factors in the Bohai Bay Basin [J]. Oil & Gas Geology, 2020, 41(2): 248-258.
[3]	Haifeng Yang, Changgui Xu, Chengmin Niu, Geng Qian, Zhengyu Li, Yanfei Gao, Zhen Huang. Quantitative evaluation of hydrocarbon accumulation pattern and the controlling factors in the Neogene of Huanghekou Sag, Bohai Bay Basin [J]. Oil & Gas Geology, 2020, 41(2): 259-269.
[4]	Zhang Zhengtao, Lin Changsong, Li Huiyong, Huang Zhi, Zhang Guokun. Characteristics of the Neogene strike-slip faults and their controls on hydrocarbon accumulation in Shaleitian uplift, Bohai Bay Basin [J]. Oil & Gas Geology, 2019, 40(4): 778-788.
[5]	Pang Xiaojun, Wang Qingbin, Dai Liming, Li Huan, Chen Jing. Paleogene fault activities and their control over sedimentation at southeastern margin of Qinnan Sag,northern Bohai Sea [J]. Oil & Gas Geology, 2017, 38(6): 1059-1067.
[6]	Zhong Yijiang, Chen Hongde, Xu Changgui, Wang Jun, Zou Hao, Wei Peng, Du Xiaofeng, Huang Xiaobo. Discovery of shallow-water delta in the Neogene Guantao Formation in the Liaodong Bay Depression and its significance for oil and gas exploration [J]. Oil & Gas Geology, 2017, 38(3): 499-507.
[7]	She Xiaoyu, Chen Jie, Zhang Shiwan, Shu Zhiguo, Yu Fei, Li Dongdong, Gong Xiaoxing. Tectonic characteristics and their shale gas geological significance of the Mesozoic-Paleozoic in Jiaoshiba area,the Sichuan Basin [J]. Oil & Gas Geology, 2016, 37(6): 828-837.
[8]	Zhang Yukun, Wang Hui, Hu Xiaoqing, Zhang Xianwen, Bu Fanqing, Gao Yufei, Fan Tingen. Reservoir modeling of complex lithologies with sparse wells: A case from A oilfield in Shijiutuo uplift,Bohai Bay Basin [J]. Oil & Gas Geology, 2016, 37(3): 450-456.
[9]	Jiang Youlu, Liu Pei, Song Guoqi, Liu Hua, Wang Yongshi, Zhao Kai. Late Cenozoic Faulting activities and their influence upon hydrocarbon accumulations in the Neogene in Bohai Bay Basin [J]. Oil & Gas Geology, 2015, 36(4): 525-533.
[10]	Fan Xiaojun, Pan Lei, Li Feng, Li Jixuan, Hou Donglin, Hao Jingyu. Hydrocarbon accumulation mechanism and play fairways of the Paleogene in Lunpola Basin,Tibet [J]. Oil & Gas Geology, 2015, 36(3): 362-369,377.
[11]	Song Guoqi, Xu Xingyou, Li Zheng, Wang Xiuhong. Factors controlling oil production from Paleogene shale in Jiyang depression [J]. Oil & Gas Geology, 2015, 36(3): 463-471.
[12]	Huang Taizhu. Analysis on the fault system of Yubei region, Tarim Basin [J]. Oil & Gas Geology, 2014, 35(1): 98-106.
[13]	Tan Xianfeng, Tian Jingchun, Huang Jianhong, Lin Xiaobing, Ma Jianwei. Material responses and accumulation patterns in cyclic sediment records of continental clastic rocks：taking the Paleogene Kongdian Formation of Wangjiagang area in Jiyang Depression as an example [J]. Oil & Gas Geology, 2013, 34(3): 332-341.
[14]	Shi Wenlong, Zhang Zhiqiang, Peng Wenxu, Wang Baoquan, Guo Tao. Tectonic evolution and hydrocarbon accumulation in the east part of Shaleitian Sailent,western Bohai Sea [J]. Oil & Gas Geology, 2013, 34(2): 242-247.
[15]	Wang Guanmin, Pang Xiaojun, Zhang Xuefang, Liu Zhanbo, Liu Boao. Activity of Shinan fault and its control on hydrocarbon accumulation in the Paleogene in Bozhong Depression [J]. Oil & Gas Geology, 2012, 33(6): 859-866.