康西瓦
- 网络kangxiwar
康西瓦-
西昆仑康西瓦西部早古生代侵入岩的岩浆混合作用
Magma mingling of Early Paleozoic intrusive rocks in western Kangxiwar , West Kunlun , China
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西昆仑康西瓦一带早古生代石英闪长岩的地质特征及其锆石SHRIMPU-Pb测年
Geological characteristics of Early Paleozoic quartz diorite in the vicinity of Kangxiwar , West Kunlun , China and its zircon SHRIMP U-Pb dating
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以多期俯冲形成的康西瓦蛇绿岩带将塔里木陆块与高加索&羌塘板块分开。
Tarim land plate and Caucasia-Qiangtang plate was divided by Kangxiwa ophiolite belt formed by multi-period subduction .
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综合以上资料及前人的研究成果认为，康西瓦构造带是分隔古亚洲和特提斯两大构造域的右行走滑转换构造带。
Based on above data and previous study KSTB is regarded as a right-hand shove transform tectonic belt which divides the paleo-Asian tectonic domain and the Tethys domain .