New Progress in Paleoearthquake Studies of the East Sertengshan Piedmont Fault, Inner Mongolia, China
New Progress in Paleoearthquake Studies of the East Sertengshan Piedmont Fault, Inner Mongolia, China
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内蒙古色尔腾山东前断裂古地震研究新进展
DOI:
10.1007/s12583-017-0937-z
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发表时间:
2018-04
影响因子:
3.3
通讯作者:
Zhang Hao
中科院分区:
文献类型:
--
作者:
He Zhongtai;Ma Baoqi;Long Jianyu;Wang Jinyan;Zhang Hao
The two eastern segments of the Sertengshan piedmont fault have moved considerably since the Holocene. Several paleoseismic events have occurred along the fault since 30 ka BP. Paleoearthquake studies have been advanced by digging new trenches and combining the results with the findings of previous studies. Comprehensive analyses of the trenches revealed that 6 paleoseismic events have occurred on the Kuoluebulong segment since approximately 30 ka BP within the following successive time periods: 19.01–37.56, 18.73, 15.03–15.86, 10.96, 5.77–6.48, and 2.32 ka BP. The analyses also revealed that 6 paleoseismic events have occurred on the Dashetai segment since approximately 30 ka BP, and the successive occurrence times are 29.07, 19.12–28.23, 13.92–15.22, 9.38–9.83, 6.08–8.36, and 3.59 ka BP. The results indicate that quasi-periodic recurrences occurred along the two segments with an approximate 4 000 a mean recurrence interval. The consistent timing of the 6 events between the two segments indicates that the segments might conform to the cascade rupturing model between the two segments. As recorded by a large number of Chinese historical texts, the latest event on the Kuoluebulong segment is the historicalM8.0 earthquake occurred on November 11, 7 BC.
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影响因子:
1.7
作者:
M. Brady;D. Coleman
通讯作者:
M. Brady;D. Coleman
影响因子:
3.3
作者:
P. Nulay;C. Chonglakmani;Q. Feng
通讯作者:
P. Nulay;C. Chonglakmani;Q. Feng
影响因子:
3
作者:
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通讯作者:
Zhongtai He;Baoqi Ma
影响因子:
3
作者:
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通讯作者:
Wenliang Jiang;Xin Wang;T. Tian;Jingfa Zhang;Donglei Wang
影响因子:
2
作者:
Murray, AS;Wintle, AG
通讯作者:
Wintle, AG