中国大陆区域地质和区域成矿规律的若干基本特征(纲要)

    SOME ESSENTIAL CHARACTERIISTICS OF REGIONAL GEOLOGYAND REGIONAL METALLOGENY OF THE CHINESE CONTINENT

    • 摘要: 从区域地质特征和区域成矿规律的角度,首次提出了中国大陆的主体部分是曾经独立存在于北方劳亚古陆和南方冈瓦纳古陆之间的古中国古陆。该古陆的基本地质特征是:稳定区的稳定程度较低,而活动区的活动强度却又相对较弱。重点论述了由此基本地质特征而造成的中国古陆的沉积环境和沉积建造、岩浆活动和火成岩建造、构造环境和构造特点、内生和外生矿产成矿规律等一系列独特的特征。

       

      Abstract: From the viewpoint of the characteristics of regional geology and regional metallogeny inChina,it is first proposed in this paper that the bulk part of the Chinese continent was once theChinese proto-continent ,located independently between Laurasia and Gondwana. The basiccharacteristics of the proto-continent is that the stability of its stable region is relatively low,while the activity of its mobile regions is relatively weak.And a series of peculiar features areemphatically discussed in the present paper,such as sedimentary environments and sedimentaryformations ,magmatic activity and igneous formations , tectonic environments and features andmetalIogenic features of endogenic and exogenic mineral deposits,which are caused by basic ge-ological characteristics.

       

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