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论古地震断层和能动断层最新活动年代的测定
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作者 黄培华 彭青 《高原地震》 1998年第3期32-36,共5页
概述了古地震断层和能动断层活动年代测定研究的现状和进展。提出了应用多种测年方法对古地震断层和能动断层的最新活动年代的测定进行综合研究。指出了当前在断层活动年代的测定工作中存在的关键问题,同时也初步提出了今后改进的意见。
关键词 古地震断层 能动断层 最新活动的年代 年龄测定
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Marine Active Fault Exploration and Paleoearthquake Research 被引量:2
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作者 DengQidong ChaoHongtai 《Earthquake Research in China》 2002年第2期155-159,共5页
Marine active fault exploration and paleoearthquake research are still a gap in China. The paper gives a review on major research methods and new progress made abroad, including submarine survey boat, seismic reflecti... Marine active fault exploration and paleoearthquake research are still a gap in China. The paper gives a review on major research methods and new progress made abroad, including submarine survey boat, seismic reflection and acoustic reflection. Through detailed studies of offset history of 10 ka to 30 ka, it is possible to determine paleoearthquake recurrent intervals and elapsed time since last major earthquake. It is suggested that active fault exploration can be carried out by acoustic exploring method in large earthquake region of Bohai Sea. Paleoearthquake activity history can be revealed and earthquake risk in the future can be predicted. 展开更多
关键词 Sea floor geomorphology Marine active fault PALEOEARTHQUAKE Acoustic exploring
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A Preliminary Study of Palaeo-earthquakes on the Maqu Fault of East Kunlun Fault Zone
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作者 He Wengui Xiong Zhen +2 位作者 Yuan Daoyang Ge Weipeng Liu Xingwang 《Earthquake Research in China》 2006年第4期361-370,共10页
The East Kunlun active fault is an important NWW-trending boundary fault on the northeastern margin of the Qinghai-Xizang (Tibet) Plateau. The Maqu fault is the easternmost segment of the East Kunlun active fault. Bas... The East Kunlun active fault is an important NWW-trending boundary fault on the northeastern margin of the Qinghai-Xizang (Tibet) Plateau. The Maqu fault is the easternmost segment of the East Kunlun active fault. Based on three trenches, four Holocene palaeo-earthquake events are identified along the Maqu fault. The latest palaeo-earthquake event is (1730±50) ~ (1802±52) a BP, the second is (3736±57) ~ (4641±60) a BP, the third is (8590±70) a BP, and the earliest is (12200±1700) ka BP. The time of the first and second palaeo-earthquake events is more reliable than that of the third and last ones. As a result, the recurrence interval of the palaeo-earthquakes on the easternmost segment of the East Kunlun active fault is approximately 2400 a, and the palaeo-earthquake elapsed time is (1730±50) ~ (1802±52) a BP. 展开更多
关键词 The east Kunlun active fault Maqu fault Palaeo-earthquake
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Study on Holocene Paleoearthquakes in Xizhang Trench on the Jiaocheng Fault Zone,Shanxi Province
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作者 Xie Xinsheng Zhao Jinquan +8 位作者 Jiang Wali An Weiping Li Zihong Zhang Dawei Cheng Xinyuan Gao Shuyi Wang Chunhe Sun Changbin Yan Chengguo 《Earthquake Research in China》 2008年第4期428-439,共12页
Xizhang trench is located 10 km northwest of Taiyuan city, Shanxi Province, in front of a NNW-trending scarp of 4.6m height on the northern segment of the Jiaocheng fault zone. The dimensions of the trench are 108m in... Xizhang trench is located 10 km northwest of Taiyuan city, Shanxi Province, in front of a NNW-trending scarp of 4.6m height on the northern segment of the Jiaocheng fault zone. The dimensions of the trench are 108m in length, 8m in width, and 10m in depth. There are 18 horizons revealed in the trench. The upper strata are sandy loam; the upper strata of the downthrown block of the fault are gravels, the lower ones are an interbed of brown loam and sandy loam. The strata on the upthrown block of the fault are sandy loam containing gravel. The trench shows 3 fault planes, and the upper offset point on the fault plane is 1.5m below the ground surface, the newest dislocated stratum is (3.74±0.06) ka BP. The trench reveals a lot of deformation traces, such as fault planes, dislocated strata, colluvial wedges and formation tilting. The relationship between strata and faults in the trench shows that 3 paleoearthquake events have occurred at the Jiaocheng fault zone since the Early Holocene, they are about (3.74±0.06)- (3.06±0.26)ka BP, (8.35±0.09)ka- (3.74±0.06)ka BP, and( 10.66±0.85) - (8.35±0.09)ka BP. The average interval among the events is 2.6 - 3.6ka. The minimum coseismic vertical displacements of the 3 events are 3.0m, 2.5m and 3.2m, respectively. The significance of Xizhang trench is that the Jiaocheng fault used to be active thousands of years ago, though there is no M ≥ 7.0 earthquake recorded in historical documents. Evidence of new Jiaocheng fault zone activity during the Holocene is important for the earthquake safety assessment of Taiynan city in the future. 展开更多
关键词 PALEOEARTHQUAKE HOLOCENE Xizhang trench Jiaocheng fault SHANXI
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Paleoearthquake Studies along the Nalinlaka Fault of the Late Pleistocene in Lhasa,Tibet 被引量:1
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作者 Liu Jing Guan Peng +4 位作者 Shen Xuhui Xu Yueren Shen Junfeng Jing Feng Hong Shunying 《Earthquake Research in China》 2010年第4期467-477,共11页
As the most import fault of the Late Pleistocene in the Lhasa area,the Nalinlaka fault is a left-lateral thrust fault,striking NWW,dipping SSW with a high dip angle,and extending over 33km.According to studies on the ... As the most import fault of the Late Pleistocene in the Lhasa area,the Nalinlaka fault is a left-lateral thrust fault,striking NWW,dipping SSW with a high dip angle,and extending over 33km.According to studies on the latest strata on the Nalinlaka fault zone,this fault zone has been obviously active since the Late Pleistocene and the movement left behind some geomorphologic phenomena on the earth's surface,especially at the sites of the gully west of Cijiaolin and around Xiecun village.For example,some rivers,ridges and terraces are displaced,forming beheaded gullies and fault escarps.The horizontal displacements since the Late Pleistocene at the above two places are 54m ~ 87m,20m ~ 67m,respectively.Based on studies on the 4 trenches along the fault using the progressive constraining method,we conclude that there might have been 5 paleoearthquake events along the Nalinlaka fault since 70ka B.P.,the ages of each paleoearthquake are 68.53,54.40,< 41.23,21.96,9.86ka B.P.,and the average recurrence interval is 14.67ka.Because of the limits of trenches and earthquake events exposed by each trench,no single trench completely revealed all 5 events.There may therefore be some errors in determining the upper and lower limits of some events in this article. 展开更多
关键词 LHASA Active fault PALEOEARTHQUAKE
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