中国南天山西部冲断褶皱系前缘区的运动学特征

肖安成; 贾承造; 杨树锋; 魏国齐; 陈汉林; 张春生

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中国南天山西部冲断褶皱系前缘区的运动学特征

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生

文章导航 > 沉积学报 > 2000 > 18(3): 439-444

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

引用本文:

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

XIAO An cheng, JIA Cheng zao, YANG Shu feng, WEI Guo qi, CHEN Han ling, ZHANG Chun sheng. The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China[J]. Acta Sedimentologica Sinica, 2000, 18(3): 439-444.

Citation:

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

引用本文:

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

Citation:

中国南天山西部冲断褶皱系前缘区的运动学特征

1 浙江大学地球科学系杭州 310027;
2 中国石油天然气股份公司塔里木油田分公司新疆库尔勒 841000;
3中国石油天然气股份公司石油科学研究院廊坊分院河北廊坊 102800;
4 江汉石油学院石油地质系湖北荆州 434102

详细信息

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

中图分类号: P542⁺.2

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文章访问数: 603
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The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

1 Zhejiang University Geoscience Department Hangzhou 310037;
2 Tarim Oilfield Company CNPC Korla Xinjiang 841000;
3 Langfang Peirolewrt Science Research Institute CNPC Langfang Hebei 102800;
4 Jianghan Petroleum Insliluie Geology Department Jingzhou HuBei 434102

摘要

摘要: 南天山冲断褶皱系是中—上新世以来形成的以薄皮滑脱为主的冲断构造,冲断作用导致了盆地内及周缘区古—新生界的碎屑岩和碳酸盐岩地层发主形变。本文对该冲断系前缘区 (巴音库鲁提北部至喀什地区 )的运动学特征进行了研究。南天山冲断褶皱系从平面上分出了六个冲断褶皱带。从剖面上划分出两种不同的冲断体系。冲断系的前锋为盲冲结构的构造三角带。冲断作用导致前锋区中新世以来层系变形、抬升并出露地表,本区有两个区域性的主滑脱面,冲断作用及断层相关褶皱的形成是冲断层沿主滑脱面向前陆方向逐渐推进的结果。同时发育的次级冲断层导致冲断褶皱带的复杂化。文章同时指出,南天山冲断褶皱系的冲断扩展顺序为逆序。这与塔里木盆地南缘西昆仑山前冲断带的活动方式相反,暗示着南天山构造带的运动学特征是独特的。利用平衡地质剖面的方法,在综合地质和地球物理资料的基础上,作出本区的构造横剖面图并进行了平衡恢复,从而得出南天山冲断褶皱系前缘区上新世以来的南北缩短率为30 %,缩短量为 5 0km,缩短速率为 9— 10mm/a。
- 南天山 /
- 冲断带 /
- 运动学特征 /
- 平衡剖面
Abstract: The Southern Tianshan thrust-fold systems are thin skin thrust structural belts formed after Miocene and Pliocene. Thrusting resulted in Palaozoic-Cenozoic clastic and carbonate rocks deforming in basin and margins regions. The kinematics characters of thrust front regions (Northern Bainkuluti and Kashi) were discussedThe Southern Tianshan thrust-fold systems were divided into six structural belts on plane and two tectonic layers in section. The blind thrust structural deltas were formed in thrust belts front.Thrusting made for Miocene strata deformation, uplift and denudation. There were two detachment surfaces. Thrusting on detachment surfaces gradually spreaded toward foreland and formed fault-related folds. That embranchment faults formed during structure activity made thrust belts more complication.The author indicated that thrust propagating of the Southern Tianshan thrust-fold systems were inverted sequence. The results were different from sequence of thrust-fold belts in Western Kunlun Mountain. It implicated that the Southern Tianshan thrust-fold systems were provided with unique kinematics characters. Using method of the balanced section, the structural crossing section was made and restored on the based of geology and geophysical data. Sequentially these were got that shorting percentage of the Southern Tianshan thrust-fold systems was 30%、that shorting amount was 50km and that shorting velocity was 9-10mm/a.
- southern Tianshan /
- thrust-fold belts /
- kinematics characters /
- balanced section

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参考文献(27)

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[3]	曲国胜,陈杰,陈新安等.西昆仑-帕米尔造山带及其北缘盆地板内变形构造[J] .地质论评,1998,44(4)：417～429
[4]	刘训.GrahamS,ChangE等.塔里木板块周缘晚古生代以来的构造演化[J] .地球化学,19(6)：715～725
[5]	刘和甫,梁慧社,蔡立国等.天山两侧前陆冲断系构造样式与前陆盆地演化[J] .地球科学,1994,19(6)：727～741
[6]	汤良杰.塔里木盆地构造演化与构造样式[J] .地球科学,1994,19(6)：742～754
[7]	Burtman V S,Skobelev S F,Molnar. Late Conozoic slip on the Talas-Ferghana fault, The Tian Shah, Central Asia[J] . Geol. Soc. Am.Bull. 1996,108:1 004～1 021
[8]	Neil E A, Houseman G A. Geodynamies of the Tarim Basin and theTian Shan in Central Asia[J] . Tectonics. 1997,16(4) :571～584
[9]	Harrision T M P,Copeland W R, Kidd W S F et al. Raising Tibet[J] .Science, 1992,255:1 663～1 670
[10]	Hendrix M S, Dumitru T A, Graham S A. Late Oligocene - Early444 沉积学报第18卷Miocene unroofing in the Chinese Tian Shan: An early effect of theIndia - Asia collision [J] . Geology, 1994,22: 487～490
[11]	Sobel E R, Dumitru T A. Thrusting and exhumation around the mar-gins of the western Tarim basin during the India - Asia collision[J] .J. Geophys. Res. 1997,102(b3):5 043～5 063
[12]	Thomas J C,Cobbold P R,Uright A. Cenozoic tectonics of the Tadzhikdepression Central Asia[A] . In: Yin A, Harision T M, eds. TectonicEvolution of Asia[C] . New York:Cambridge Univ. Press, 1996.191～207
[13]	Yin A, Nie S, Harrison T M, et al. Late Cenozoic tectonic Evolution ofhe Southern Chinese Tian Shan[J] . Tectonics, 1998, 17(1): 1～27
[14]	肖安成,张春生,李景义.中国南天山西部冲断褶皱系前缘区的结构,中国碰撞造山带研究[M] .北京：海洋出版社,1999.80～91
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[26]	肖安成.塔里木盆地西南缘的构造特征和油气聚集规律[J] .江汉石油学院学报,1997,19(2)：1～6
[27]	伍德华特N B,博耶SE,萨普J.平衡地质剖面[M] .贾维民等译.武汉：中国地质大学出版社,1991

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中国南天山西部冲断褶皱系前缘区的运动学特征

1 浙江大学地球科学系杭州 310027;

2 中国石油天然气股份公司塔里木油田分公司新疆库尔勒 841000;

3中国石油天然气股份公司石油科学研究院廊坊分院河北廊坊 102800;

4 江汉石油学院石油地质系湖北荆州 434102

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

收稿日期: 1998-12-31
修回日期: 2000-01-02
刊出日期: 2000-09-10

中图分类号: P542⁺.2

关键词:

南天山 /

冲断带 /

运动学特征 /

平衡剖面

摘要: 南天山冲断褶皱系是中—上新世以来形成的以薄皮滑脱为主的冲断构造,冲断作用导致了盆地内及周缘区古—新生界的碎屑岩和碳酸盐岩地层发主形变。本文对该冲断系前缘区 (巴音库鲁提北部至喀什地区 )的运动学特征进行了研究。南天山冲断褶皱系从平面上分出了六个冲断褶皱带。从剖面上划分出两种不同的冲断体系。冲断系的前锋为盲冲结构的构造三角带。冲断作用导致前锋区中新世以来层系变形、抬升并出露地表,本区有两个区域性的主滑脱面,冲断作用及断层相关褶皱的形成是冲断层沿主滑脱面向前陆方向逐渐推进的结果。同时发育的次级冲断层导致冲断褶皱带的复杂化。文章同时指出,南天山冲断褶皱系的冲断扩展顺序为逆序。这与塔里木盆地南缘西昆仑山前冲断带的活动方式相反,暗示着南天山构造带的运动学特征是独特的。利用平衡地质剖面的方法,在综合地质和地球物理资料的基础上,作出本区的构造横剖面图并进行了平衡恢复,从而得出南天山冲断褶皱系前缘区上新世以来的南北缩短率为30 %,缩短量为 5 0km,缩短速率为 9— 10mm/a。

English Abstract

The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

1 Zhejiang University Geoscience Department Hangzhou 310037;

2 Tarim Oilfield Company CNPC Korla Xinjiang 841000;

3 Langfang Peirolewrt Science Research Institute CNPC Langfang Hebei 102800;

4 Jianghan Petroleum Insliluie Geology Department Jingzhou HuBei 434102

Received Date: 1998-12-31
Rev Recd Date: 2000-01-02
Publish Date: 2000-09-10

Keywords:

Abstract: The Southern Tianshan thrust-fold systems are thin skin thrust structural belts formed after Miocene and Pliocene. Thrusting resulted in Palaozoic-Cenozoic clastic and carbonate rocks deforming in basin and margins regions. The kinematics characters of thrust front regions (Northern Bainkuluti and Kashi) were discussedThe Southern Tianshan thrust-fold systems were divided into six structural belts on plane and two tectonic layers in section. The blind thrust structural deltas were formed in thrust belts front.Thrusting made for Miocene strata deformation, uplift and denudation. There were two detachment surfaces. Thrusting on detachment surfaces gradually spreaded toward foreland and formed fault-related folds. That embranchment faults formed during structure activity made thrust belts more complication.The author indicated that thrust propagating of the Southern Tianshan thrust-fold systems were inverted sequence. The results were different from sequence of thrust-fold belts in Western Kunlun Mountain. It implicated that the Southern Tianshan thrust-fold systems were provided with unique kinematics characters. Using method of the balanced section, the structural crossing section was made and restored on the based of geology and geophysical data. Sequentially these were got that shorting percentage of the Southern Tianshan thrust-fold systems was 30%、that shorting amount was 50km and that shorting velocity was 9-10mm/a.

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

引用本文:

肖安成, 贾承造, 杨树锋, 魏国齐, 陈汉林, 张春生. 中国南天山西部冲断褶皱系前缘区的运动学特征[J]. 沉积学报, 2000, 18(3): 439-444.

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中国南天山西部冲断褶皱系前缘区的运动学特征

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

计量

The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

计量

目录

中国南天山西部冲断褶皱系前缘区的运动学特征

1 浙江大学地球科学系杭州 310027;

2 中国石油天然气股份公司塔里木油田分公司新疆库尔勒 841000;

3中国石油天然气股份公司石油科学研究院廊坊分院河北廊坊 102800;

4 江汉石油学院石油地质系湖北荆州 434102

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

English Abstract

The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

1 Zhejiang University Geoscience Department Hangzhou 310037;

2 Tarim Oilfield Company CNPC Korla Xinjiang 841000;

3 Langfang Peirolewrt Science Research Institute CNPC Langfang Hebei 102800;

4 Jianghan Petroleum Insliluie Geology Department Jingzhou HuBei 434102

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[1]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
[2]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.

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中国南天山西部冲断褶皱系前缘区的运动学特征

作者简介: 肖安成,1958年出生,副教授,博士,构造地质学

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The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

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出版历程

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中国南天山西部冲断褶皱系前缘区的运动学特征

1 浙江大学地球科学系 杭州 310027; 2 中国石油天然气股份公司塔里木油田分公司 新疆库尔勒 841000; 3中国石油天然气股份公司石油科学研究院廊坊分院 河北廊坊 102800; 4 江汉石油学院石油地质系 湖北荆州 434102

作者简介: 肖安成,1958年出生,副教授,博士,构造地质学

English Abstract

The Kinematics Characters of The Thrust- foldBelts Western Front Regions in Southern Tianshan, China

1 Zhejiang University Geoscience Department Hangzhou 310037; 2 Tarim Oilfield Company CNPC Korla Xinjiang 841000; 3 Langfang Peirolewrt Science Research Institute CNPC Langfang Hebei 102800; 4 Jianghan Petroleum Insliluie Geology Department Jingzhou HuBei 434102

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目录

友情链接

期刊在线

联系我们

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

1 浙江大学地球科学系杭州 310027;

2 中国石油天然气股份公司塔里木油田分公司新疆库尔勒 841000;

3中国石油天然气股份公司石油科学研究院廊坊分院河北廊坊 102800;

4 江汉石油学院石油地质系湖北荆州 434102

作者简介:
肖安成,1958年出生,副教授,博士,构造地质学

1 Zhejiang University Geoscience Department Hangzhou 310037;

2 Tarim Oilfield Company CNPC Korla Xinjiang 841000;

3 Langfang Peirolewrt Science Research Institute CNPC Langfang Hebei 102800;

4 Jianghan Petroleum Insliluie Geology Department Jingzhou HuBei 434102