新疆阜康断裂带甘河子段晚第四纪活动特征

吴传勇; 陈建波; 沈军; 宋和平; 吴国栋; 罗福忠

doi:10.3799/dqkx.2013.064

Volume 38 Issue 3

May 2013

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Article Navigation > Earth Science > 2013 > 38(3): 632-640

WU Chuan-yong, CHEN Jian-bo, SHEN Jun, SONG He-ping, WU Guo-dong, LUO Fu-zhong, 2013. Late-Quaternary Activity Characteristics of the Ganhezi Segment of the Fukang Fault Belt, in Xinjiang. Earth Science, 38(3): 632-640. doi: 10.3799/dqkx.2013.064

Citation:

WU Chuan-yong, CHEN Jian-bo, SHEN Jun, SONG He-ping, WU Guo-dong, LUO Fu-zhong, 2013. Late-Quaternary Activity Characteristics of the Ganhezi Segment of the Fukang Fault Belt, in Xinjiang. Earth Science, 38(3): 632-640. doi: 10.3799/dqkx.2013.064

Citation:

WU Chuan-yong, CHEN Jian-bo, SHEN Jun, SONG He-ping, WU Guo-dong, LUO Fu-zhong, 2013. Late-Quaternary Activity Characteristics of the Ganhezi Segment of the Fukang Fault Belt, in Xinjiang. Earth Science, 38(3): 632-640. doi: 10.3799/dqkx.2013.064

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Late-Quaternary Activity Characteristics of the Ganhezi Segment of the Fukang Fault Belt, in Xinjiang

doi: 10.3799/dqkx.2013.064

Seismological Bureau of Xinjiang Uygur Autonomous Region, Urumqi 830011, China

Received Date: 2012-07-15
Publish Date: 2013-05-15

Abstract

Abstract

In order to understand the activity characteristics of the Fukang fault in Late-Quaternary, and accurately estimate the seismic hazard of the fault, a geological survey has been conducted along the Fukang fault. By surveying the deformation micro-topography, excavating two large paleoearthquake trenches, and dating a series of samples of thermoluminescence, the quantity activity characteristics of the Ganhezi fault segment of the Fukang fault belt are revealed. The Ganhezi fault segment is a Holocene active fault, with a total length about 33 km. The fault activity is obvious, generating a series of apparent geomorphic traces on the surface. Since the Late-Quaternary, the average vertical slip rate of fault is about 0.34-0.43 mm/a. Since the Mid-Holocene, there were two paleoearthquake events; the strong earthquake recurrence period of the fualt segment is about 2 100-3 750 a. The vertical surface displacement is about 1.5 m and the elapsed time is 4.11 ka of the latest paleoearthquake, corresponding to the paleoearthquake magnitude of between Ms7.2-7.4. The fault has accumulated a high energy so far.
- Fukang fault belt,
- tectonic landform,
- Late-Quaternary,
- deformation characteristics,
- paleoearthquake

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References(46)

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Late-Quaternary Activity Characteristics of the Ganhezi Segment of the Fukang Fault Belt, in Xinjiang

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