大地构造相(tectonic facies )概念最初由许靖华(1991)正式提出,其后在应用和使用过程中存在不同的理解和划分。
该蛇绿混杂岩带是义敦碰撞造山带大地构造相中的弧前混杂带相。
The ophiolite melange zone represents forearc melange facies of the Yidun collision orogens.
根据煤和蒸发岩的地史分布等资料,说明一个海陆相对固定的大地构造模型更符合实际。
The distribution of coal and evaporite in geohistory suggests a geotectonic hypothesis of relatively fixed continents and oceans rather than a drifting model.
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