西伯利亚地台

结果表明：在塔里木地台及西伯利亚地台边缘，Q0值较高，为300~450；而在南部的西昆仑褶皱系、松潘甘孜褶皱系，Q0呈现出低值，在150~250的范围内变化；

The results indicate that Q 0 was higher ( 300 ~ 450 ) in the Tarim platform and the edges of Siberian platform , while Q 0 was lower ( 150 ~ 250 ) in the southern regions as west Kunlun fold system and Songpan Ganzi fold system .

西伯利亚地台西南部某些金矿床地质学与地球化学

Geology and geochemistry of gold deposits in the southwest of Siberian Platform

文章对西伯利亚地台的地质结构和油气生成及分布作简单介绍。

The text simply introduces geologic configuration , hydrocarbon generation and distribution of the Siberia platform .

西伯利亚地台西南缘加里东褶皱系中，金矿床发育有两种建造类型：a。

There are two kinds of gold-deposit formations within Caledonian foldsystem in the southwest of Siberian platform : a.

印度板块、塔里木盆地、东欧地块、西伯利亚地台、华北地块、扬子地台、东南沿海褶皱系均表现突出。

Some blocks are more obvious as India plate , Tarim basin east Europe block , Siberian plate , North-China block , Yangtze , etc.

西伯利亚地台的新元古代到早寒武世间的钙藻化石特别丰富，为研究钙藻化石的发育历史提供了模式。

The Siberian Platform is the model for studies of a history of development of calcareous algae that appeared in abundance at the transition from the Late Proterozoic to the Early Cambrian .

将北亚地区划分成西伯利亚地台、维尔霍扬斯克-科雷马造山带和中亚造山带三个一级构造单元，根据陆核、古褶带、地块的概念进行了二级构造单元划分。

The North Asia area may be divided into three first-rank tectonic units : the Siberia continental platform , the Verkhoyansk-Kolyma orogenic belt and the Centra-Asian orogenic belt . The second-rank tectonic units , including nuclei , fold belts and blocks , are subdivided in this study .