佳木斯-伊通断裂带大型逆冲构造带的发现及形成时代

doi:10.11743/ogg20060508

Abstract

Abstract:

The newly discovered major thrustbelt in the Jiamusi-Yitong fault zone in Siping city of Jilin province has well developed thrusts,cataclasite,and folds.In areas near the eastern and western main boundary faults, secondary faults are distributed intensively,and folds are dominated by closed vertical bends,while in the central part of the thrustbelt,the strata occurrence is gentle with few faults and folds,indicating that the main boundary faults are the area of compressive stress concentration.Most of the faults thrust towards the 110°-130° irection.According to the relationship of cutting and overlaying between the thrusts and the Mesozoic-Cenozoic strata,the Jiamusi-Yitong fault zone is considered to have experienced at least two periods of strong obduction since the Cretaceous:the first occurred in late Late Cretaceous,when the major thrustbelt was formed;and the second occurred at the end of Oligocene.According to field survey results and basin data,the formation and evolution of Jiamusi-Yitong fault zone can be divided into five stages:namely sinistral strike-slip(early K₁),regional stretch(later K₁-early K₂),compressive and thrusting(late K₂),fault depression(E),and compressive inversion(the end of E₃).

Key words: thrust fault, Late Cretaceous, Jiamusi-Yitong fault zone, northeastern China

CLC Number:

TE111.2

Sun Xiaomeng, Long Shengxiang, Zhang Meisheng, Liu Xiaoyan, Hao Fujiang. Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone[J]. Oil & Gas Geology, 2006, 27(5): 637-643.

References

[1] 万天丰.郯-庐断裂带的演化与古应力场[J].地球科学--中国地质大学学报.1995.20(5):526～534 Wan Tianfeng.Evolution of Tancheng-Lujiang fault zone and paleostress flelds[J].Earth Science-Journal of China University of Geosciences,1995,20(5):526-534
[2] 王小风,李中坚,陈柏林郯庐断裂带[M].北京:地质出版社,2000.1～180 Wang Xiaofeng,Li Zhongjian,Chen Bolin.Tancheng-Lujiang fault zone[M].Beijing:Geological Publishing House,2000.1-180
[3] 朱光,王道轩,刘国生,等.郯庐断裂带的演化及其对西太平洋板块的响应[J] 地质科学,2004,39(1):36～49 Zhu Guang,Wang Daoxuan,Liu Guosheng,et al.Evolution of the Tan-Lu fault zone and its responses to plate movements in West Pacific basin[J].Scientia Geologica Sinica,2004,39(1):36-49
[4] 朱光,王道轩,刘国生,等.郯庐断裂带的伸展活动及其动力学背景[J].地质科学,2001,36(3):269～278 Zhu Guang,Wang Daoxuan,Liu Guosheng,et al.Extensional activities along the Tan-Lu fault zone and its geodynamic setting[J].Scientia Geologica Sinica,2001,36(3):269-278
[5] 张庆龙,王良书,谢国爱,等.郯庐断裂带北延及中新生代构造体制转换问题的探讨[J].高校地质学报,2005,11(40):577～584 Zhang Qinglong,Wang Liangshu,Xie Guoai,et al.Discussion on northward extension of Tan-Lu fault zone and its tectonic regime transformation[J].Geological Journal of China Universities,2005,11(40):577-584
[6] 刘茂强,杨丙中,邓俊国,等.伊通-舒兰地堑地质构造特征及其演化[M].北京:地质出版社,1993.42～103 Liu Maoqiang,Yang Bingzhong,Deng Junguo,et al.The feature of geological structure and its evolution of Yitong-Shulan graben[M].Beijing:Geological Publishing House,1993.42-82
[7] 王永春.伊通地堑含油气系统与油气成藏[M].北京:石油工业出版社,2001.10～50 Wang Yongchun.Oil-gas-beating system and oil-gas accumulation of Yitong graben[M].Beijing:Petroleum Industry Press,2001.10-50
[8] 任建业,陆永潮,李思田,等.伊舒地堑构造演化的沉积充填响应[J].地质科学,1999,34(2):196～203 Ren Jianye,Lu Yongchao,Li Sitian,et al.The tectonic evolution of the Yi-Shu Graben and its depositional filling response[J].Scientia Geologica Sinica,1999,34(2):196-203
[9] 田在艺,韩屏.中国东北地区中新生代沉积盆地构造形成演化及其油气展望[J].石油地震地质,1992,4(2):1～23 Tian Zaiyi,Han Ping.Tectonic evolution and hydrocarbon prospect of Meso-Cenozoic sedimentary basins in NE China[J].Petroleum Seismogeology,1992,4(2):1-23
[10] 陈发景,赵海玲,陈昭年,等.中国东部中、新生代伸展盆地构造特征及地球动力学背景[J].地球科学--中国地质大学学报,1996,21(4):357～365 Chen Fajing,Zhao Hailing,Chen Zhaonian,et al.Structural characteristics and geodynamic setting of Mesozoic and Cenozoic extensional basins in eastern China[J].Earth Science-Journal of China University of Geosciences,1996,21(4):357-365
[11] 陈守田,张克民,王青海,等.伊-舒地堑下第三系层序地层分析[J].石油与天然气地质,2002,23(2):150～153 Chen Shoutian,Zhang Kemin,Wang Qinghai,et al.Analysis of sequence stratigraphy of Eogene system in Yi-Shu graben[J].Oil & Gas Geology,2002,23(2):150-153
[12] 侯贵廷,冯大晨,王文明,等.松辽盆地的反转构造作用及其对油气成藏的影响[J].石油与天然气地质,2004,25(1):49～53 Hou Guiting,Feng Dachen,Wang Wenming,等.Reverse structures and their impacts on hydrocarbon accumulation in Songliao basin[J].Oil & Gas Geology,2004,25(1):49-53
[13] 窦立荣,宋建国,王瑜.郯庐断裂带北段形成的年代学及其意义[J].地质论评,1996,42(6):508～512 Dou Lirong,Song Jianguo,Wan Yu.Chronology and its significance of the north segment in Tan-Lu fault zone[J].Geological Review,1996,42(6):508-512
[14] 殷长建,彭玉鲸,王彦生,等.伊舒断裂带年代学新证据[J].吉林地质,2005,24(1):6～15 Yin Changjian,Peng Yujing,Wang Yansheng,et al.New evidences of chronology of rift belt of Yitong-Shulan[J].Jilin Geology,2005,24(1):6-15
[15] 朱光,牛漫兰,刘国生,等.郯庐断裂带肥东段走滑运动的⁴⁰Ar/³⁹Ar法定年[J].地质学报,2005,79(3):303～316 Zhu Guang,Niu Manlan,Liu Guosheng,et al.⁴⁰Ar/³⁹Ar dating for the strike-slip movement on the Feidong part of the Tan-Lu fault belt[J].Acta Geologica Sinica,2005,79(3):303-316
[16] Maruyama S,Seno T.Orogeny and relative plate motions:example of the Japanese Islands[J].Tectonophysics,1986,127(3-4):305-329
[17] Maruyama S,Isozaki Y,Kimura Gand Terabayashi M C.Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from 750 Ma to the present[J].Island Arc,1997,6:121-142
[18] 任延广,陈均亮,冯志强,等.喜山运动对松辽盆地含油气系统的影响[J].石油与天然气地质,2004,25(2):185～190 Ren Yanguang,Chen Junliang,Feng Zhiqiang,et al.Impacts of Himalaya movement on petroleum system in Songliao basin[J].Oil & Gas Geology,2004,25(2):185-190
[19] 徐旭辉,高长林,黄泽光,等.中国盆地形成的三大活动构造历史阶段[J].石油与天然气地质,2005,26(2):155～162 Xu Xuhui,Gao Changlin,Huang Zeguang,et al.Three stages of tectonic movements in formation of petroliferous basins in China[J].Oil & Gas Geology,2005,26(2):155-162
[1] 张宏,王小风.郯庐断裂系北段地质特征及中生代演化.中国地质科学院-沈阳地质矿产研究所,1995,(4):50～778

Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone

PDF (PC)

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 8

Recommended Articles

Metrics

[1]	Lin Peng, Wu Shenghe, Zhang Jiajia, Hu Guangyi, Xia Qinyu, Fan Hongjun, Wang Nansu. Distribution of submarine fans in the thrust fault zone of continental slope, Niger Delta Basin [J]. Oil & Gas Geology, 2018, 39(5): 1073-1086.
[2]	Yang Geng, Li Wei, Chen Zhuxin, Shi Xin, Lei Yongliang, Wang Xiaobo. Mazatage detachment anticline in Hetianhe gas field, Tarim Basin, western China [J]. Oil & Gas Geology, 2015, 36(4): 563-572.
[3]	Yao Wenqian, Tang Liangjie, Xie Daqing, Yang Yong, Jiang Huashan, Zhang Yuhang, Yu Tengxiao, Cao Zicheng. Deformation and tectonic evolution of the Selibuya fault zone in Tarim Basin [J]. Oil & Gas Geology, 2013, 34(4): 522-527.
[4]	Wang Xinguo, Wang Pu, He Jiankun, Li Dongan. A study of structure styles between double thrust faults——taking the area between Yuejin-2 and Yuedong thrust faults in the Qaidam Basin as an example [J]. Oil & Gas Geology, 2010, 31(1): 114-118.
[5]	Luo Jinhai, Che Zicheng, Guo Anlin, Cheng Shunyou, Pei Xianzhi. Late Cretaceous lithospheric extension in the Nandan-Hechi tectonic zone of northern Guangxi Province and its influence on hydrocarbon accumulation conditions [J]. Oil & Gas Geology, 2009, 30(5): 619-625.
[6]	Cheng Xiaogan, Zheng Dewen, Yang Shufeng, Xiao Ancheng, Chen Hanlin. A study on characteristics of the Late Cretaceous-Paleocene structures in Jiuquan Basin [J]. Oil & Gas Geology, 2006, 27(4): 522-527.
[7]	Zhang Hong, He Shunli, Pang Xiongqi, Gu Daihong, Jiang Zhenxue. Physical simulation of reservoiring process of Kela 2 gas field [J]. Oil & Gas Geology, 2006, 27(1): 23-26.
[8]	Chen Zhaonian, Chen Fajing, Su Junqing, Sun Xiaoming. CONTROL OF FAULTING OVER OIL-GAS POOLS OF BURIED HILLS IN BEIDAGANG STRUCTURAL BELT [J]. Oil & Gas Geology, 2002, 23(1): 92-95.