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A DEEP SEISMIC REFLECTION PROFILE ACROSS ALTUN FAULT BELT 被引量:3
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作者 Gao Rui 1, Liu Hongbin 2, Li Qiusheng 1,Li Pengwu 1, Yao Peiyi 1, Huang Dongding 3 (1 Lithosphere Research Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China,E\|mail: gaorui@cags.cn.net 2 Institute of Ge 《地学前缘》 EI CAS CSCD 2000年第S1期205-205,共1页
Altun fault is regarded as a large\|scale sinistral strike\|slip fault, it is composed of several faults with the different character, and there is a special geological structure in the fault belt, and they constitute... Altun fault is regarded as a large\|scale sinistral strike\|slip fault, it is composed of several faults with the different character, and there is a special geological structure in the fault belt, and they constitute the northwestern margin fault belt of the Qinghai\|Tibetan plateau. In order to investigate the deep crust structure in the Altun region, layers which Tarim lithosphere subducted beneath the Qinghai\|Tibetan plateau, the forward structure of the subduction plate and the scale of the plate subduction, a deep seismic reflection profile was designed. Data collection work of the deep seismic reflection profile across Altun fault was completed during 24/8/1999 to 25/9/1999. The profile locates in Qiemo county, Xinjiang Uygur Autonomous Region, the southern end of the profile stretches into Altun Mountains, the northern end locates in the Tarim desert margin. The profile is nearly SN trending and crosses the main Altun fault. The profile totally is 145km long, time record is 30 seconds, the smallest explosive amount is 72~100kg, the biggest explosive amount reaches 200~300kg, the explosive distance is 800m, and detectors are laid at a 50m distance. 展开更多
关键词 DEEP seismic reflection probing Altun FAULT bELT tarim b lock DEEP CRUST structure MOHO
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