祁连山北缘佛洞庙—红崖子断裂晚第四纪滑动速率研究
|
摘要
佛洞庙—红崖子断裂是发育于祁连山北缘中段河西走廊南缘的一条重要的块体边界断裂,总体走向北西西,长约110 km。该断裂为一条全新世活动的逆-左旋走滑断裂,也是1609年红崖堡7 1/4级地震的发震断裂。断裂活动形成了一系列陡坎、断层崖以及冲沟和阶地左旋等断错地貌。我们通过详细的野外考察,选择典型断错地貌进行大比例尺差分GPS测量,结合所获相应地貌面的年代数据,得到该断裂晚第四纪平均垂直滑动速率为(0.61±0.28)mm/a,水平滑动速率为(1.27±0.58)mm/a,其结果与相邻断裂相吻合。
Fodongmiao-Hongyazi in an important margin fault which developed at the middle part of the north Qinlian Mountain and the south of Hexi-corridor,the main trending is NWW with length 110 km.The fault is a fault is a left-lateral reverse strike-slip fault during the Holocene periods,it is also the seismogenic fault of Hongyabao W7 1/4 earthquake in 1609.The activity of the fault formed a series of geomorphology like fault scarp,terrace and gully left-lateral.In this study,based on the detail field work,we choose the typical geomorphology cell carried on large scale differential GPS measure.Combined with the age dating date,we got the average vertical slip rates was(0.61±0.28 ) mm/a,and the horizontal slip rates was(1.27±0.58 ) mm/a,the result roughly same with adjacent fault
Fodongmiao-Hongyazi in an important margin fault which developed at the middle part of the north Qinlian Mountain and the south of Hexi-corridor,the main trending is NWW with length 110 km.The fault is a fault is a left-lateral reverse strike-slip fault during the Holocene periods,it is also the seismogenic fault of Hongyabao W7 1/4 earthquake in 1609.The activity of the fault formed a series of geomorphology like fault scarp,terrace and gully left-lateral.In this study,based on the detail field work,we choose the typical geomorphology cell carried on large scale differential GPS measure.Combined with the age dating date,we got the average vertical slip rates was(0.61±0.28 ) mm/a,and the horizontal slip rates was(1.27±0.58 ) mm/a,the result roughly same with adjacent fault
引文
边庆凯,张培震,苏向洲.2001.榆木山北缘断裂的构造地貌特征与断层活动性.华北地震科技,19(3):41-49. Bian Qingkai,Zhang Peizhen and Su Xiangzhou.2001.The tectonic topography feature of the faults in north Yumushan Mountain and its faulting activity.North China Earthquake Sciences,19(3):41-49.
陈杰.1995.祁连山西段第四纪构造运动的阶段、性质及其年代学研究(博士学位论文).北京:国家地震局地质研究所.1-126. Chen Jie.1995.Quaternary Tectonic Processes in the Western Portion of Qilianshan Mountain,Northwestern China(PhD Thesis).Beijing:Institute of Geology,SSB.1-126.
国家地震局地质研究所,国家地震局兰州地震研究所.1993.祁连山—河西走廊活动断裂系.北京:地震出版社.1- 340. Institute of Geology,SSB and Lanzhou Institute of Seismology,SSB.1993.The Qilian Mountain-Hexi Corridor Active Fault System.Beijing:Seismological Press.1-340.
李吉均,文世宣,张青松,王富葆,郑本兴,李炳元.1979.青藏高原隆起的时代、幅度和形式的探讨.中国科学,22(6): 608-616. Li Jijun,Wen Shixuan,Zhang Qingsong,Wang Fubao,Zheng Benxing and Li Bingyuan.1979.A discussion on the period, amplitude and type of the uplift of the Qinghai-Xizang Plateau.Scientia Sinica,22(11 ):1314-1328.
李吉均,方小敏.1998.青藏高原隆起与环境变化研究,科学通报,43(15):1569-1574. Li Jijun and Fang Xiaomin.1998.Uplift of the Tibetan Plateau and environmental changes.Chinese Science Bulletin,44(23): 2117-2124.
刘百篪.1998.青藏高原的新生代重要地质事件与构造演化.见:中国地震学研究进展—纪念谢毓寿教授八十寿辰.北京:地震出版社.299-307. Liu Baichi.1998.Main geology events and the tectonic evolution in Cenozoic are in Qinghai-Tibet Plateau.In:Progress of Seismology of China-Eighty-Birthday Commemoration of Professor Xie Yushou.Beijing:Seismological Press.299- 307.
刘兴旺,袁道阳,雷中生,曹娜.2011.1609年甘肃红崖堡71/4级地震考证.西北地震学报,33(2):143-148. Liu Xingwang,Yuan Daoyang,Lei Zhongsheng and Cao Na.2011.Textual Research on the Hongyapu M7.25 Earthquake in 1609.Northwestern Seismological Journal,33(2):143-148.
闵伟,张培震,何文贵,李传友,毛凤英,张淑萍.2002.酒西盆地断层活动特征及古地震研究.地震地质,24(1): 35-44. Min Wei,Zhang Peizhen,He Wengui,Li Chuanyou,Mao Fengying and Zhang Shuping.2002.Research on the active faults and paleoearthquakes in the western Jiuquan Basin.Seismology and Geology,24(1 ):35-44.
张培震,李传友,毛凤英.2008.河流阶地演化与走滑断裂滑动速率.地震地质,30(1):44-57. Zhang Peizhen,Li Chuanyou and Mao Fengying.2008.Strath terrace formation and strike-slip faulting.Seismology and Geology,30(1):44-57.
郑文俊.2009.河西走廊及其邻区活动构造图像及构造变形模式(博士学位论文).北京:中国地震局地质研究所.1- 126. Zheng Wenjun.2009.Geometric Pattern and Active Tectonics of the Hexi Corridor and Its Adjacent Regions(Ph D Thesis). Beijing:Institute of Geology,China Earthquake Administration.1-126.
Cowgill E.2007.Impact of riser reconstructions on estimation of secular variation in rates of strike slip faulting:Revisiting the Cherchen River site along the Altyn Tagh fault,NW China.Earth and Planetary Science Letters,254(3 - 4):239- 255.
Kirby E,Harkins N,Wang E,Shi X,Fan C and Burbank D.2007.Slip rate gradients along the eastern Kunlun fault.Tectonics, 26:TC2010,doi:10.1029/2006TC002033.
Gaudemer Y,Tapponnier P,Meyer B,Peltzer G,Guo S M,Chen Z T,Dai H G and Cifuentes I.1995.Partitioning of crustal slip between linked,active faults in the eastern Qilian Shan,and evidence for a major seismic gap,the Tianzhu gap', on the western Haiyuan Fault,Gansu(China).Geophysical journal International,120(3):599-645.
Hetzel R,Niedermann S,Tao M X,Kubik P W,Ivy-Ochs S,Gao B and Strecker M R.2002.Low slip rates and long-term preservation of geomorphic features in Central Asia.Nature,417:428-432.
Hetzel R,Tao M X,Stokes S,Niedermann S,Ivy-Ochs S,Gao B,Strecker M R and Kubik P W.2004.Late Pleistocene/ Holocene slip rate of the Zhangye thrust(Qilian Shan,China) and implications for the active growth of the northeastern Tibetan Plateau,Tectonics.23(6):TC6006,doi:10.1029/2004TC001653.
Tapponnier P,Meyer B,Avouac J P,Peltzer G,Gaudemer Y,Guo S M,Xiang H F,Yin K L,Chen Z T,Cai S H and Dai H G. 1990.Active thrusting and folding in the Qilian Shan,and decoupling between upper crust and mantle in northeastern Tibet.Earth and Planetary Science Letters,97(3-4):382-403.
Zhang P Z,Molnar P and Xu X W.2007.Late Quaternary and present-day rates of slip along the Altyn Tagh fault,northern margin of the Tibetan Plateau.Tectonics,26(5):TC5010,doi:10.1029/2006TC002014.
Zheng D W,Clark M K,Zhang P Z,Zheng W J and Farley K A.2010.Erosion,fault initiation and topographic growth of the North Qilian Shan(northern Tibetan Plateau).Geosphere,6(6):937-941.
陈杰.1995.祁连山西段第四纪构造运动的阶段、性质及其年代学研究(博士学位论文).北京:国家地震局地质研究所.1-126. Chen Jie.1995.Quaternary Tectonic Processes in the Western Portion of Qilianshan Mountain,Northwestern China(PhD Thesis).Beijing:Institute of Geology,SSB.1-126.
国家地震局地质研究所,国家地震局兰州地震研究所.1993.祁连山—河西走廊活动断裂系.北京:地震出版社.1- 340. Institute of Geology,SSB and Lanzhou Institute of Seismology,SSB.1993.The Qilian Mountain-Hexi Corridor Active Fault System.Beijing:Seismological Press.1-340.
李吉均,文世宣,张青松,王富葆,郑本兴,李炳元.1979.青藏高原隆起的时代、幅度和形式的探讨.中国科学,22(6): 608-616. Li Jijun,Wen Shixuan,Zhang Qingsong,Wang Fubao,Zheng Benxing and Li Bingyuan.1979.A discussion on the period, amplitude and type of the uplift of the Qinghai-Xizang Plateau.Scientia Sinica,22(11 ):1314-1328.
李吉均,方小敏.1998.青藏高原隆起与环境变化研究,科学通报,43(15):1569-1574. Li Jijun and Fang Xiaomin.1998.Uplift of the Tibetan Plateau and environmental changes.Chinese Science Bulletin,44(23): 2117-2124.
刘百篪.1998.青藏高原的新生代重要地质事件与构造演化.见:中国地震学研究进展—纪念谢毓寿教授八十寿辰.北京:地震出版社.299-307. Liu Baichi.1998.Main geology events and the tectonic evolution in Cenozoic are in Qinghai-Tibet Plateau.In:Progress of Seismology of China-Eighty-Birthday Commemoration of Professor Xie Yushou.Beijing:Seismological Press.299- 307.
刘兴旺,袁道阳,雷中生,曹娜.2011.1609年甘肃红崖堡71/4级地震考证.西北地震学报,33(2):143-148. Liu Xingwang,Yuan Daoyang,Lei Zhongsheng and Cao Na.2011.Textual Research on the Hongyapu M7.25 Earthquake in 1609.Northwestern Seismological Journal,33(2):143-148.
闵伟,张培震,何文贵,李传友,毛凤英,张淑萍.2002.酒西盆地断层活动特征及古地震研究.地震地质,24(1): 35-44. Min Wei,Zhang Peizhen,He Wengui,Li Chuanyou,Mao Fengying and Zhang Shuping.2002.Research on the active faults and paleoearthquakes in the western Jiuquan Basin.Seismology and Geology,24(1 ):35-44.
张培震,李传友,毛凤英.2008.河流阶地演化与走滑断裂滑动速率.地震地质,30(1):44-57. Zhang Peizhen,Li Chuanyou and Mao Fengying.2008.Strath terrace formation and strike-slip faulting.Seismology and Geology,30(1):44-57.
郑文俊.2009.河西走廊及其邻区活动构造图像及构造变形模式(博士学位论文).北京:中国地震局地质研究所.1- 126. Zheng Wenjun.2009.Geometric Pattern and Active Tectonics of the Hexi Corridor and Its Adjacent Regions(Ph D Thesis). Beijing:Institute of Geology,China Earthquake Administration.1-126.
Cowgill E.2007.Impact of riser reconstructions on estimation of secular variation in rates of strike slip faulting:Revisiting the Cherchen River site along the Altyn Tagh fault,NW China.Earth and Planetary Science Letters,254(3 - 4):239- 255.
Kirby E,Harkins N,Wang E,Shi X,Fan C and Burbank D.2007.Slip rate gradients along the eastern Kunlun fault.Tectonics, 26:TC2010,doi:10.1029/2006TC002033.
Gaudemer Y,Tapponnier P,Meyer B,Peltzer G,Guo S M,Chen Z T,Dai H G and Cifuentes I.1995.Partitioning of crustal slip between linked,active faults in the eastern Qilian Shan,and evidence for a major seismic gap,the Tianzhu gap', on the western Haiyuan Fault,Gansu(China).Geophysical journal International,120(3):599-645.
Hetzel R,Niedermann S,Tao M X,Kubik P W,Ivy-Ochs S,Gao B and Strecker M R.2002.Low slip rates and long-term preservation of geomorphic features in Central Asia.Nature,417:428-432.
Hetzel R,Tao M X,Stokes S,Niedermann S,Ivy-Ochs S,Gao B,Strecker M R and Kubik P W.2004.Late Pleistocene/ Holocene slip rate of the Zhangye thrust(Qilian Shan,China) and implications for the active growth of the northeastern Tibetan Plateau,Tectonics.23(6):TC6006,doi:10.1029/2004TC001653.
Tapponnier P,Meyer B,Avouac J P,Peltzer G,Gaudemer Y,Guo S M,Xiang H F,Yin K L,Chen Z T,Cai S H and Dai H G. 1990.Active thrusting and folding in the Qilian Shan,and decoupling between upper crust and mantle in northeastern Tibet.Earth and Planetary Science Letters,97(3-4):382-403.
Zhang P Z,Molnar P and Xu X W.2007.Late Quaternary and present-day rates of slip along the Altyn Tagh fault,northern margin of the Tibetan Plateau.Tectonics,26(5):TC5010,doi:10.1029/2006TC002014.
Zheng D W,Clark M K,Zhang P Z,Zheng W J and Farley K A.2010.Erosion,fault initiation and topographic growth of the North Qilian Shan(northern Tibetan Plateau).Geosphere,6(6):937-941.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心