the intrusive rock belt and the ophiolite belt of the same time together demonstrate that the tectonic system of the north qinling during the jinning movement is plate tectonic system.
北秦岭侵入巖带与同时代的蛇绿巖带有力地证明,北秦岭晋宁运动的构造体制是板块体制。
tarim land plate and caucasia - qiangtang plate was divided by kangxiwa ophiolite belt formed by multi-period subduction.
以多期俯沖形成的康西瓦蛇绿巖带将塔里木陆块与高加索—羌塘板块分开。
in addition, the authors have also processed gravity and magnetic anomalies in order to ascertain the extension of an ophiolite belt in this area.
此外,还对重、磁异常进行了处理,以确定蛇绿巖带的延展情况。