STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS

MA Bao-qi; LI De-wen

Volume 14 Issue 3

Sep. 2008

Turn off MathJax

Article Contents

Abstract

References

Article Navigation > Journal of Geomechanics > 2008 > 14(3): 201-211

XIAO Dian, LIAO Qun-an, WANG Liang-yu, et al., 2016. PETROGENESIS AND TECTONIC IMPLICATIONS OF TWO TYPES EARLY SILURIAN GRANITES IN EAST JUNGGAR. Journal of Geomechanics, 22 (4): 1049-1061.

Citation:

MA Bao-qi, LI De-wen, 2008. STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS. Journal of Geomechanics, 14 (3): 201-211.

XIAO Dian, LIAO Qun-an, WANG Liang-yu, et al., 2016. PETROGENESIS AND TECTONIC IMPLICATIONS OF TWO TYPES EARLY SILURIAN GRANITES IN EAST JUNGGAR. Journal of Geomechanics, 22 (4): 1049-1061.

Citation:

MA Bao-qi, LI De-wen, 2008. STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS. Journal of Geomechanics, 14 (3): 201-211.

PDF( 466 KB)

STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS

MA Bao-qi^1
,,
LI De-wen²

1.
Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
2.
China Earthquake Disaster Prevention Center, China Earthquake Administration, Beijing 100085, China

More Information

Abstract

Abstract

The Menyuan Basin is an intermontane basin in the central segment of the Qilian Mountains, bounded by boundary faults on the north and south.The basin is filled with the Paleogene Baiyanghe Formation and Quaternary tills and glaciofluvial deposits.The differences in rock deformation, geomorphological evolution and fault movement phases show that the Menyuan Basin underwent four stages of tectonic movements since the Cenozoic.The earliest Cenozoic tectonic movement began in the middle Oligocene (30 Ma B.P), when the I-order planation surface was disintegrated and basin was downfaulted and received sandy gravel deposits of the Baiyanghe Formation.The second stage occurred from the end of the Oligocene to the beginning of the Miocene (25 Ma to 460 ka B.P)and was characterized by the end of the basin subsidence, termination of Tertiary deposition and folding of the Baiyanghe Formation. This process continued to the initial middle Pleistocene.The third stage started in the middle part of the middle Pleistocene (460 ka B.P)and ended at 30 ka B.P.During the stage new boundary faults formed, the basin was again downfaulted and received >400 m thick tills and glaciofluvial deposits, and boundary faults were very active.This process lasted till the late part of the late Pleistocene (30 ka B.P).The latest stage began at 30 ka B.P, which was marked by the wholesale uplift of the basin and mountains at both sides of the basin and transition of the basin surface process from deposition to incision and erosion.The fault movement changed from thrusting with a strike-slip component to strike-slip movement, but the strike-slip rate decreased significantly.
- Menyuan Basin,
- tectonic deformation,
- faulting period,
- neotectonic movement stage

FullText(HTML)

致谢: Steven Wojtal, Christopher Talbot和Roberto Weinberg对本文提出了许多建设性的修改意见, 作者在此表示感谢。本文是在国家自然科学基金面上项目(Project No. 40572119)资助下完成。

References(33)

References

[1]	李吉均, 方小敏, 马海州, 等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学(D辑), 1996, 26(4):317~322. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600261329
[2]	李吉均.青藏高原的地貌演化与亚洲季风[J].海洋地质与第四纪地质.1999, 19(1):1~10. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz199901002
[3]	施雅风, 李吉均, 李炳元, 等.晚新生代青藏高原的隆升与东亚环境变化[J].地理学报, 1999, 54(1):10~21. doi: 10.3321/j.issn:0375-5444.1999.01.002
[4]	施雅风.第四纪中期青藏高原冰冻圈的演化及其与全球变化的关系[J].冰川冻土, 1998, 20(3):197~208.
[5]	李长安, 张玉芬.一次重要的第四纪构造严冬及环境效应[J].地质科技情报, 1999, 18(4):42~46.
[6]	施炜, 马寅生, 吴满路, 等.青藏高原东北缘共和盆地第四纪地层学研究[J].地质力学学报, 2006, 12(3):317~323. doi: 10.3969/j.issn.1006-6616.2006.03.005
[7]	鹿化煜, 安芷生, 王晓勇, 等.最近14Ma青藏高原东北缘阶段性隆升的地貌证据[J].中国科学(D辑), 2004, 34(9):855~864.
[8]	方小敏, 赵志军, 李吉均, 等.祁连山北缘老君庙背斜晚新生代磁性地层与高原北部隆升[J].中国科学(D辑), 2004, 34(2):97~106. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200402001
[9]	吴珍汉, 江万, 周继荣, 等.青藏高原腹地典型岩体热历史与构造—地貌演化过程的热年代学分析[J].地质学报, 2001, 75(4):468~476. doi: 10.3321/j.issn:0001-5717.2001.04.006
[10]	崔之久, 伍永秋, 刘耕年, 等.关于"昆仑—黄河"运动[J].中国科学(D辑), 1998, 28(1):53~59. doi: 10.3321/j.issn:1006-9267.1998.01.007
[11]	潘保田, 邬光剑, 王义祥, 等.祁连山东段沙沟河阶地的年代与成因[J].科学通报, 2000, 45(24):2669~2675. doi: 10.3321/j.issn:0023-074X.2000.24.019
[12]	王成善, 朱利东, 刘志飞.青藏高原北部盆地构造沉积演化与青藏高原向北生长过程[J].地球科学进展, 2004, 19(3):373~381. doi: 10.3321/j.issn:1001-8166.2004.03.005
[13]	朱利东, 王成善, 伊海生, 等.青藏高原盆地系统演化与高原形成时间[J].成都理工大学学报(自然科学版), 2004, 31(3):249~255. doi: 10.3969/j.issn.1671-9727.2004.03.006
[14]	陆洁民, 郭召杰, 赵泽辉, 等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报, 2004, 10(1):50~61. doi: 10.3969/j.issn.1006-7493.2004.01.004
[15]	陈杰, 卢演俦, 丁国瑜.祁连山西段酒西盆地区第四纪构造运动的阶段划分[J].第四纪研究, 1996, 16(3):263~271. doi: 10.3321/j.issn:1001-7410.1996.03.009
[16]	谭利华, 杨景春, 段锋军.河西走廊新生代构造运动的阶段划分[J].北京大学学报(自然科学版), 1998, 34(4):523~532. doi: 10.3321/j.issn:0479-8023.1998.04.017
[17]	杨景春.祁连山北麓河流阶地与新构造演化[J].第四纪研究, 1998, (3):229~237. doi: 10.3321/j.issn:1001-7410.1998.03.006
[18]	郑文涛, 杨景春, 段锋军.武威盆地晚更新世河流阶地变形与新构造运动[J].地震地质, 2000, 22(3):318~328. doi: 10.3969/j.issn.0253-4967.2000.03.012
[19]	国家地震局地质研究所, 国家地震局兰州地震研究所.祁连山—河西走廊活动断裂系[M].北京:地震出版社, 1993.95~104.
[20]	国家地震局兰州地震研究所.昌马活动断裂带[M].北京:地震出版社, 1992.
[21]	何文贵, 刘百篪, 袁道阳, 等.冷龙岭活动断裂的滑动速率研究[J].西北地震学报, 2000, 22(1):90~97. doi: 10.3969/j.issn.1000-0844.2000.01.017
[22]	康建成, 朱俊杰, 陈宏凯.祁连山冷龙岭南坡晚第四纪冰川演化序列[J].冰川冻土, 1992, 14(4):352~359. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049842
[23]	郭宏伟, 陈晔, 李吉均.祁连山冷龙岭南麓的冰川序列、黄土记录和阶地系列的初步研究[J].兰州大学学报(自然科学版), 1995, 31(1):102~110. doi: 10.3321/j.issn:0455-2059.1995.01.019
[24]	史正涛, 张世强, 周尚哲, 等.祁连山第四纪冰碛物的ESR测年[J].冰川冻土, 2000, 22(4):353~357. doi: 10.3969/j.issn.1000-0240.2000.04.010
[25]	赵井东, 周尚哲, 史正涛, 等.祁连山东段冷龙岭南麓白水河冰碛物ESR测年研究[J].兰州大学学报(自然科学版), 2001, 37(4):110~117. doi: 10.3321/j.issn:0455-2059.2001.04.022
[26]	赵井东, 周尚哲, 崔建新, 等.摆浪河流域的ESR年代学与祁连山第四纪冰期新认识[J].山地学报, 2001, 19(6):481~488. doi: 10.3969/j.issn.1008-2786.2001.06.001
[27]	周尚哲, 李吉均, 张世强, 等.祁连山摆浪河谷地的冰川地貌与冰期[J].冰川冻土, 2001, 23(2):131~138. doi: 10.3969/j.issn.1000-0240.2001.02.005
[28]	周尚哲, 李吉均.第四纪冰川测年研究新进展[J].冰川冻土, 2003, 25(6):660~666. doi: 10.3969/j.issn.1000-0240.2003.06.011
[29]	侯元才, 许伟林, 俞建, 等.青藏高原北缘1.2MaB.P.以来各阶段古气候演变[J].青海地质, 2001, B12:10~16.
[30]	黄华芳, 彭作林, 卢伟, 等.酒西盆地、酒东盆地第三系磁性地层的划分与对比[J].甘肃地质学报, 1993, 2(1):6~16. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000005227462
[31]	尹泽生, 徐叔鹰.祁连山区域地貌与制图研究[M].北京:科学出版社, 1992, 32~38.
[32]	陈柏林, 刘建生, 张永双, 等.嘉峪关断裂晚第四纪新构造活动特征[J].地质力学学报, 2007, 13(1):78~85. doi: 10.3969/j.issn.1006-6616.2007.01.010
[33]	申旭辉, 汪一鹏. 川滇地区最新构造变形基本特征初步研究[C]. 新构造与环境, 地震出版社, 2001, 430~439.

Relative Articles

	GAO Chenyang, ZHAO Fuhai, GAO Lianfeng, LI Bingxi, LEI Maosheng, DING Kai. 2023: The methods of fracture prediction based on structural strain analysis and its application. Journal of Geomechanics, 29(1): 21-33. doi: 10.12090/j.issn.1006-6616.2022089
	ZHAO Yuanfang, SHI Wei, ZHANG Yu. 2023: Study on the reconstruction of the paleo-tectonic stress field and its evolution in the Jinchuan mining district, Gansu Province, China. Journal of Geomechanics, 29(6): 770-785. doi: 10.12090/j.issn.1006-6616.2023161
	CHANG Zu-feng, ZHANG Yan-feng, LI Jian-lin. 2017: THE SEISMOGENIC MECHANISM OF STRONG EARTHQUAKES IN DAYAO-YAOAN AREA:STRUCTURE STRENGTHENING AND ACTIVITY OF THE NW STRIKE FOLD JOINTS. Journal of Geomechanics, 23(1): 161-172.
	ZHAO Jiyong, ZHOU Xingui, LEI Qihong, ZHAO Guoxi, HE You'an, SHI Jianchao, ZHANG Linyan. 2017: STUDY ON PALEO-TECTONIC AND PRESENT TECTONIC STRESS IN CHANG 7 TIGHT RESERVOIR OF MALING OILFIELD, ORDOS BASIN. Journal of Geomechanics, 23(6): 810-820.
	ZHANG Dan-dan, DAI Jun-sheng, FU Xiao-long. 2015: NUMERICAL SIMULATION OF STRUCTURAL STRESS FIELD IN THE LATE SEDIMENTARY PERIOD OF Es₄ AND PREDICTION OF THE LOWER-ORDER FAULTS IN LANGGU SAG. Journal of Geomechanics, (1): 38-46.
	CUI Min, CAI Jia. 2014: AUTOMATIC FINITE STRAIN DETERMINATION OF QUARTZ SANDSTONE IN WEAK STRUCTURAL DEFORMATION REGION. Journal of Geomechanics, 20(2): 159-164.
	WANG Ming-liang, ZHANG Jia-gui, WANG Xin-wen, LUAN Qiu-lei. 2014: CHARACTERISTICS OF PALEOTECTONIC STRESS FILED ON THE AILAOSHAN STRUCTURAL BELT. Journal of Geomechanics, 20(1): 82-93.
	CHEN Long, SHI Wei. 2014: SUPERPOSED FOLD: AN OVERVIEW. Journal of Geomechanics, 20(4): 455-468.
	DAI Jun-sheng, ZHANG Ji-biao, FENG Jian-wei, TIAN Teng-fei, MAO Cheng-dong. 2012: DEVELOPMENT LAW AND PREDICTION OF THE LOWER-ORDER FAULTS IN THE WEST OF ZHENWU FAULT ZONE IN GAOYOU SAG. Journal of Geomechanics, 18(1): 11-21.
	WANG Ji-lin, JIANG Bo, WANG Chao-yong. 2007: SIMULATION STUDY OF THE TECTONIC STRESS FIELD IN MINES———A CASE STUDY OF THE BAODIAN COAL MINE. Journal of Geomechanics, 13(3): 239-246.
	WANG Lian-jie, WU Zhen-han, WANG Wei, SUN Dong-sheng. 2006: NUMERICAL MODELING OF THE PRESENT TECTONIC STRESS FIELD IN THE CENTRAL QINGHAI-TIBET PLATEAU. Journal of Geomechanics, 12(2): 140-149.
	ZHAO Shu-yue, SUN Guang-rui, ZHAO Jie, LI Kai, ZHU Chun-yan. 2001: STUDY OF MESOZOIC PALAEOTECTONIC STRESS FIELD IN THE VOLCAMIC ROCK AREA OF HUZHONG,THE NORTHERN PART OF DAHINGANLING VOLCANIC ZONE. Journal of Geomechanics, 7(4): 359-367.
	HUANG Ji-jun. 2001: STRUCTURAL FEATURES, STRESS FIELDS AND STRAIN FIELDS IN FENGHUANGSHAN SILVER MINE AREA, GUANGXI, CHINA. Journal of Geomechanics, 7(1): 9-21.
	XU Zenghe, XU Xiaohe. 1999: LIQUID-SOLID COUPLED PROBLEM OF RADIAL FLOW THROUGH POROUS MEDIA UNDER GENERAL PLAIN STRESSCODITION. Journal of Geomechanics, 5(1): 14-18.
	Zhang Da, Li Dongxu. 1998: MODELING OF STRESS FIELD OF FENGHUANGSHAN OREFIELD DURING MINERALIZATION. Journal of Geomechanics, 4(2): 91-96.
	Tan Chengxuan, Wang Lianjie, Sun Baoshan, Hu Daogong, Xu Shouli. 1997: AN APPROACH TO NUMERICAL SIMULATION OF 3-D TECTONIC STRESS FIELD OF THE OIL-GAS-BEARING BASIN. Journal of Geomechanics, 3(1): 71-80.
	Ding Yuanchen, Sun Baoshen, Wang Xihai, Shao Zhaogang, Zhou Xingui. 1996: PALEOSTRESS IN NORTHERN TARIM OIL FIELD ESTIMATED BY AE. Journal of Geomechanics, 2(2): 18-25.

Supplements(0)

Cited By

Proportional views

Proportional views

Figures(5)

Get Citation

PDF

XML

Article Metrics

Article views (292) PDF downloads(23)

STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS

Abstract

References

Relative Articles

Proportional views

Catalog

Article Metrics

Proportional views

Related

STAGES OF THE NEOTECTONIC MOVEMENT OF THE MENYUAN BASIN IN THE MIDDLE SEGMENT OF THE QILIAN MOUNTAINS

Abstract

References

Relative Articles

Proportional views

Catalog

Article Metrics

Proportional views

Related

Export File

Citation

Format

Content