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surface trace中文是什么意思

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  • Tian shan extends east - west in central asia , the tian shan range was formed in later paleozoic , and a few intramontan basins appeared in mesozoic . it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision , so many active structures can be found in tian shan . active tectonics took actions during last ten thousands yeas , and surface traces of fault scarps , detached gullies and folds in alluvial deposit are apparent , so it is easy to distinguish them from other geological phenomema
    天山位于亚洲中部,天山造山带形成于晚古生代,到中生代时,在天山内部形成了一些山间盆地,印度板块在始新世向北与欧亚板块碰撞,天山受南北向挤压力的作用再度于早中新世隆起,由于板块碰撞的持续进行,在天山山间及山前发育了许多的活动构造。
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Last modified time:Thu, 14 Aug 2025 00:29:56 GMT

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