THE LANDFORM FORMATION PROCESS OF ALPINE-GORGE IN BEISHAN, WUSHI COUNTY, SOUTHWESTERN TIANSHAN

CHEN Rui-ming; ZHA Xian-feng; GU Ping-yang; ZHUANG Yu-jun

Volume 23 Issue 2

Apr. 2017

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Article Navigation > Journal of Geomechanics > 2017 > 23(2): 264-271

CHEN Rui-ming, ZHA Xian-feng, GU Ping-yang, et al., 2017. THE LANDFORM FORMATION PROCESS OF ALPINE-GORGE IN BEISHAN, WUSHI COUNTY, SOUTHWESTERN TIANSHAN. Journal of Geomechanics, 23 (2): 264-271.

Citation:

CHEN Rui-ming, ZHA Xian-feng, GU Ping-yang, et al., 2017. THE LANDFORM FORMATION PROCESS OF ALPINE-GORGE IN BEISHAN, WUSHI COUNTY, SOUTHWESTERN TIANSHAN. Journal of Geomechanics, 23 (2): 264-271.

Citation:

CHEN Rui-ming, ZHA Xian-feng, GU Ping-yang, et al., 2017. THE LANDFORM FORMATION PROCESS OF ALPINE-GORGE IN BEISHAN, WUSHI COUNTY, SOUTHWESTERN TIANSHAN. Journal of Geomechanics, 23 (2): 264-271.

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THE LANDFORM FORMATION PROCESS OF ALPINE-GORGE IN BEISHAN, WUSHI COUNTY, SOUTHWESTERN TIANSHAN

CHEN Rui-ming^{1, 2
,},
ZHA Xian-feng^{1, 2},
GU Ping-yang^{1, 2},
ZHUANG Yu-jun¹

1.
Xi'an Center of Geological Survey, CGS, Xi'an 710054, Shannxi, China
2.
Orogen Research Center of China Geological Survey, Xi'an 710054, Shannxi, China

More Information

Received: 2016-10-27
Published: 2017-04-01

Abstract

Abstract

The geomorphological evolutionisbasically influenced by the tectonic and its regular pattern. Based on the observation of Quaternary deposit and erosional landform of Gunguntielieke river valley in Beishan, Wushi County, Southwest Tianshan, combing with the published stratigraphic chronology, the evolution of erosive geomorphic in Middle Pleistocene and Holocene are reproduced. In Middle Pleistocene, the geomorphological cutting depth is more than 1870 m, which is much deeper than 50 m in Holocene and it is believed that the alpine-gorge in this area was formed in Middle Pleistocene. Generally developed Middle Pleistocene fold thrust structure in Southwest Tianshan, resulting in the rapid and substantial mountainuplift, is the main cause of the alpine-gorge geomorphology in Beishan. The fold thrust structures extended to the basin, which led to the decrease of amplitude of the uplift of the mountain to the basin. It reveals the spatial regularity of the geomorphological evolution in Beishan. There is a close relationship between the process of Quaternary tectonic uplift and geomorphological evolution in Southwest Tianshanmountainaccording to this stuty.
- Southwest Tianshan,
- Wushi,
- Middle Pleistocene,
- alpine-gorge,
- uplift,
- geomorphological evolution

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References(32)

References

[1]	曾联波, 谭成轩, 张明利.塔里木盆地库车坳陷中新生代构造应力场及其油气运聚效应[J].中国科学D辑地球科学, 2004, 34(SI): 98~106. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2004S1010.htm ZENG Lian-bo, TAN Cheng-xuan, ZHANG Ming-li. Tectonic stress field and its effect on hydrocarbon migration and accumulation in Mesozoic and Cenozoic in Kuqa depression, Tarim basin[J]. Science in China Series D: Earth Sciences, 2004, 47(S2): 114~124. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2004S1010.htm
[2]	张明利, 谭成轩, 汤良杰, 等.塔里木盆地库车坳陷中新生代构造应力场分析[J].地球学报, 2004, 25(6): 615~619. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2004S1010.htm ZHANG Ming-li, TAN Cheng-xuan, TANG Liang-jie, et al.Ananalysis of the Mesozoic-Cenozoic tectonic stress field in Kuqa Depression, TarimBasin[J]. Acta Geoscientica Sinica, 2004, 25(6): 615~619. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2004S1010.htm
[3]	郑民, 孟自芳, 李相博, 等.新构造运动活跃的库车盆地含油气系统特征[J].中山大学学报(自然科学版), 2005, 44(S): 304~308. http://www.cnki.com.cn/Article/CJFDTOTAL-ZSDZ2005S1055.htm ZHENG Min, MENG Zi-fang, LI Xiang-bo, et al. Characteristic of the hydrocarbon system in Kuqa Basin with an active new structural movement[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2005, 44(S): 304~308. http://www.cnki.com.cn/Article/CJFDTOTAL-ZSDZ2005S1055.htm
[4]	汪新, 贾承造, 杨树锋.南天山库车褶皱冲断带构造几何学和运动学[J].地质科学, 2002, 37(3): 372~384. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200203015.htm WANG Xin, JIA Cheng-zao, YANG Shu-feng.Geometry and kinematics of the Kuqa fold-and-thrust belt in the southern Tianshan[J]. Chinese Journal of Geology, 2002, 37(3): 372~384. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200203015.htm
[5]	杨树锋, 陈汉林, 程晓敢, 等.南天山新生代隆升和去顶作用过程[J].南京大学学报(自然科学版), 2003, 39(1): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ200301001.htm YANG Shu-feng, CHEN Han-lin, CHENG Xiao-gan, et al. Cenozoic uplifting and unroofing of southern TienShan, China[J]. Journal of Nanjing University(NaturalSciences), 2003, 39 (1): 1~8. http://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ200301001.htm
[6]	周兴熙.塔里木盆地库车油气系统新生代构造演化及油气成藏作用[J].古地理学报, 2002, 4(1): 75~82. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200201011.htm ZHOU Xing-xi.Oil and gas pool-forming process and tectonic evolution of Cenozoic in Kuqa petroleum system of TarimBasin[J]. Journal of Palaeogeography, 2002, 4(1): 75~82. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200201011.htm
[7]	马德明, 陈江力, 曾昌民, 等.塔里木盆地西北缘柯坪冲断带的构造变形特征[J].地质力学学报, 2007, 13(4): 340~347. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070444&journal_id=dzlxxb MA De-ming, CHEN Jiang-li, ZENG Chang-min, et al. Structural deformation characteristics of the Kalpin thrust belt on the northwestern margin of the Tarimbasin[J]. Journal of Geomechanics, 2007, 13(4): 340~347. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20070444&journal_id=dzlxxb
[8]	Allen M B, Vincent S J, Wheeler P J. Late Cenozoic tectonics of the Kepingtage thrust zone: interactions of the TienShan and Tarim basin, Northwest China[J]. Tectonics, 1999, 18(4): 639~654. doi: 10.1029/1999TC900019
[9]	Jia D, Lu H L, Jia C Z, et al. Structural features of northern Tarim Basin: implications for regional tectonics and petroleum traps: reply[J]. AAPG Bulletin, 1999, 83(8): 1284~1286. http://aapgbull.geoscienceworld.org/content/83/8/1284
[10]	Allen M B, Vincent S J. Structural features of northern Tarim Basin: implications for regional tectonics and petroleum traps: Discussion[J]. AAPG Bulletin, 1999, 83(8): 1279~1283. http://aapgbull.geoscienceworld.org/content/83/8/1284
[11]	Yin A, Nie P, Craig P, et al. Late Cenozoic tectonic evolution of the Southern Chinese TianShan[J]. Tectonics, 1998, 17(1): 1~27. doi: 10.1029/97TC03140
[12]	郑民, 雷刚林, 黄少英, 等.南天山西段南缘断裂构造特征及对乌什凹陷发育的控制[J].地质科学, 2007, 42(4): 639~655. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200704003.htm ZHENG Min, LEI Gang-lin, HUANG Shao-ying, et al. Features of fault structure in Southern margin of west segment of the South Tianshan, and its control to evolution of the Wushi sag[J]. Chinese Journal of Geology, 2007, 42(4): 639~655. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200704003.htm
[13]	付碧宏, 贾营营.南天山乌什前陆逆冲褶皱构造带的晚新生代构造地貌特征与地震活动[J].地质科学, 2010, 45(4): 917~929. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201004001.htm FU Bi-hong, JIA Ying-ying.Late Cenozoic tectono-geomorphology and seismicities of the Wushi thrust-and-fold belt, southern TianShan[J]. Chinese Journal of Geology, 2010, 45(4): 917~929. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201004001.htm
[14]	陈建波, 沈军, 张同良, 等.库车坳陷区西段拱拜孜活动逆断裂-背斜变形特征[J].新疆地质, 2011, 29(1): 32~36. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201101008.htm CHEN Jian-bo, SHEN Jun, ZHANG Tong-liang, et al. Deformation feature of Gongbaizi reverse fault anticline in west segment of Kuqadepression[J]. Xinjiang Geology, 2011, 29(1): 32~36. http://www.cnki.com.cn/Article/CJFDTOTAL-XJDI201101008.htm
[15]	滕志宏, 岳乐平, 何登发, 等.南疆库车河新生界剖面磁性地层研究[J].地层学杂志, 1997, 21(1): 55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ701.005.htm TENG Zhi-hong, YUE Le-ping, HE Deng-fa, et al. Magnetostratigraphic research of Cenozoic section of Kuche River area, South Xinjiang[J]. Journal of Stratigraphy, 1997, 21(1): 55~62. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ701.005.htm
[16]	游长江.壳体地貌沉积过程初论[J].大地构造与成矿学, 1997, 21(1): 83~88. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK199701010.htm YOU Chang-jiang.On the sedimentary processes of crustobodygeomorphology[J]. GeotectonicaetMetallogenia, 1997, 21(1): 83~88. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK199701010.htm
[17]	陈杰, 丁国瑜, Burbank D W, 等.中国西南天山山前的晚新生代构造与地震活动[J].中国地震, 2001, 17(2): 134~155. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200102003.htm CHEN Jie, DING Guo-yu, Burbank D W, et al. Late Cenozoic tectonics and seismicity in the Southwestern Tianshan, China[J]. Earthquake Research in China, 2001, 17(2): 134~155. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGZD200102003.htm
[18]	田勤俭, 丁国瑜, 郝平.南天山及塔里木北缘构造带西段地震构造研究[J].地震地质, 2006, 28(2): 213~223. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200602004.htm TIAN Qin-jian, DING Guo-yu, HAO Ping.Seismotectonic study on west part of the interaction zone between Southern Tianshan and Northern Tarim[J]. Seismology and Geology, 2006, 28(2): 213~223. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ200602004.htm
[19]	杨成荣, 吴传勇, 聂晓红. 2009年4月19日新疆阿合奇5.4级地震[J].内陆地震, 2010, 24(4): 315~322. http://www.cnki.com.cn/Article/CJFDTOTAL-LLDZ201004003.htm YANG Cheng-rong, WU Chuan-yong, NIE Xiao-hong.Study on Aheqi5.4 Earthquake in Xinjiang on APR. 19, 2009[J]. Inland Earthquake, 2010, 24(4): 315~322. http://www.cnki.com.cn/Article/CJFDTOTAL-LLDZ201004003.htm
[20]	贾启超, 吴传勇, 沈军, 等.西南天山迈丹断裂阿合奇段左旋走滑的证据及其最新活动[J].地震工程学报, 2015, 37(1): 222~227. http://www.cnki.com.cn/Article/CJFDTOTAL-ZBDZ201501035.htm JIA Qi-chao, WU Chuan-yong, SHEN Jun, et al. Evidence of left-lateral strike-slip along the Aheqi segment of Maidan fault in southwest Tianshan mountains, China and its latest activity[J]. China Earthquake Engineering Journal, 2015, 37(1): 222~227. http://www.cnki.com.cn/Article/CJFDTOTAL-ZBDZ201501035.htm
[21]	陈杰, Heermance R V, Burbank D W, 等.中国西南天山西域砾岩的磁性地层年代与地质意义[J].第四纪研究, 2007, 27(4): 576~587. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200704013.htm CHEN Jie, Heermance R V, Burbank D W, et al. Magnetochronology and its implications of the Xiyu conglomerate in the southwestern Chinese TianShan foreland[J]. Quaternary Sciences, 2007, 27(4): 576~587. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200704013.htm
[22]	陈杰, 尹金辉, 曲国胜, 等.塔里木盆地西缘西域组的底界、时代、成因与变形过程的初步研究[J].地震地质, 2000, 22(S): 104~116. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ2000S1014.htm CHEN Jie, YIN Jin-hui, QU Guo-sheng, et al. Timing, lowerboundary, genesis, and defrormation of Xiyu Formation around the western margins of the Tarimbasin[J]. Seismology and Geology, 2000, 22 (S): 104~116. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ2000S1014.htm
[23]	郑洪波, 陈惠忠, 靳鹤龄, 等.上新世—早更新世青藏高原北缘隆升的磁性地层学证据[J].海洋地质与第四纪地质, 2002, 22(2): 57~62. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200202010.htm ZHENG Hong-bo, CHEN Hui-zhong, JIN He-ling, etal. Magnetostratigraphic evidence for the Pliocene-early Pleistocene uplift of the northern Tibetan Plateau[J]. Marine Geology & Quaternary Geology, 2002, 22(2): 57~62. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200202010.htm
[24]	孙继敏, 朱日祥.天山北麓晚新生代沉积及其新构造与古环境指示意义[J].第四纪研究, 2006, 26(1): 14~19. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601002.htm SUN Ji-min, ZHU Ri-xiang.Cenozoic deposits in the Northern Tianshan mountains and its implications for neotectonics and environmental changes[J]. Quaternary Sciences, 2006, 26(1): 14~19. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ200601002.htm
[25]	Fang X M, Zhao Z J, Li JJ, et al. Magnetostratigraphy of the Late Cenozoic Laojunmiao anticline in the northern Qilian Mountains and its implications for the northern Tibetan Plateau uplift[J]. Science in China Series D: Earth Sciences, 2005, 48(7): 1040~1051. doi: 10.1360/03yd0188
[26]	赵希涛, 胡道功, 吴中海, 等.青海格尔木早更新世昆仑河砾岩的发现及其地质意义[J].地质力学学报, 2010, 16(1): 1~10. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100101&journal_id=dzlxxb ZHAO Xi-tao, HU Dao-gong, WU Zhong-hai, et al. Discovery of the early Pleistocene Kunlunhe Conglomerate in Golmud of Qinghai province and its geological significance[J]. Journal of Geomechanics, 2010, 16(1): 1~10. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100101&journal_id=dzlxxb
[27]	崔之久, 伍永秋, 刘耕年.昆仑—黄河运动的发现及其性质[J].科学通报, 1997, 42(18): 1986~1989. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199718018.htm CUI Zhi-jiu, WU Yong-qiu, LIU Geng-nian.Discovery and character of the Kunlun-Yellow river movement[J]. Chinese Science Bulletin, 1998, 43(10): 833~836. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199718018.htm
[28]	Cui Z J, Wu Y Q, Liu G N, et al. On Kunlun-Yellow river tectonic movement[J]. Science in China Series D: Earth Sciences, 1998, 41(6): 592~600.
[29]	Wu Y Q, Cui Z J, Liu G N, et al. Quaternary geomorphological evolution of the Kunlun pass area and uplift of the Qinghai-Xizang (Tibet) plateau[J]. Geomorphology, 2001, 36(3/4): 203~216.
[30]	江樟焰, 伍永秋, 崔之久. "昆仑-黄河运动"与我国自然地理格局的形成[J].北京师范大学学报(自然科学版), 2005, 41(1): 85~88. http://www.cnki.com.cn/Article/CJFDTOTAL-BSDZ20050100S.htm JIANG Zhang-yan, WU Yong-qiu, CUI Zhi-jiu.Kunlun-Yellow river tectonic motion and formation of modern physical geography pattern of China[J]. Journal of Beijing Normal University (Natural Science), 2005, 41(1): 85~88. http://www.cnki.com.cn/Article/CJFDTOTAL-BSDZ20050100S.htm
[31]	王国灿, 侯光久, 张克信, 等.东昆仑东段中更新世以来的成山作用及其动力转换[J].地球科学——中国地质大学学报, 2002, 27(1): 4~12. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200201001.htm WANG Guo-can, HOU Guang-jiu, ZHANG Ke-xin, et al. Mountain building and its dynamic transition since middle Pleistocene in east of eastern Kunlun, northeast Tibet Plateau[J]. Earth Science—Journal of China University of Geosciences, 2002, 27(1): 4~12. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200201001.htm
[32]	王国灿, 吴燕玲, 向树元, 等.东昆仑东段第四纪成山作用过程与地貌变迁[J].地球科学——中国地质大学学报, 2003, 28(6): 583~592. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200306001.htm WANG Guo-can, WU Yan-ling, XIANG Shu-yuan, et al. Mountain building process and geomorphic migration of eastern Kunlun mountains during Quaternary[J]. Earth Science—Journal of China University of Geosciences, 2003, 28(6): 583~592. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200306001.htm