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论新疆深大断裂特征与地震的关系(2)
引用本文:宋和平.论新疆深大断裂特征与地震的关系(2)[J].内陆地震,2006,20(1):1-9.
作者姓名:宋和平
作者单位:新疆维吾尔自治区地震局,新疆,乌鲁木齐,830011
摘    要:新疆独有的地貌形态及展布特征反映了地壳岩石圈深部物质运移变化的结果。由于地理位置和所处的构造部位的不同,中部天山山脉、北部阿尔泰山脉、西南部昆仑—阿尔金山脉在地壳岩石圈深部特征都有很大差异,它们有整体共性的必然联系,也有区域个性的特殊面貌。了解和认识岩石圈结构及其变化特征,对于分析研究该区域构造环境、应力场和地震的发生等有重要意义。

关 键 词:地壳  岩石圈  深部构造  新疆
文章编号:1001-8956(2006)01-0001-09
收稿时间:2005-07-19
修稿时间:2005-12-22

RELATION BETWEEN CHARACTER OF XINJINAG DEEP AND HUGE FRACTURE AND EARTHQUAKE
SONG He-ping.RELATION BETWEEN CHARACTER OF XINJINAG DEEP AND HUGE FRACTURE AND EARTHQUAKE[J].Inland Earthquake,2006,20(1):1-9.
Authors:SONG He-ping
Institution:Seismological Bureau of Xinjiang Uygur Autonomous Region, Urumqi 830011, Xinjiang, China
Abstract:Special shape and distributing feature of Xinjiang geomorphy reflect change of deep material motion of crust and lithosphere.With different geographic position and tectonic section,the deep character of crust and lithosphere in the middle Tienshan mountain,the northern Altai mountain and southwestern Kunlun-Alkin mountain are very different,which have a common necessary relation as a whole,and also special regional feature.It is significant to know changing character of lithosphere structure in order to analyze and study regional tectonic conditions,stress field and earthquake occurrence.
Keywords:Crust  Lithosphere  Deep tectonic  Xinjiang
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