收稿日期: 1998-01-14
修回日期: 1998-06-29
网络出版日期: 1998-12-01
基金资助
地矿部"九五"重大基础项目"重要盆地类型与高原隆升的关系"(项目编号:9501101-02)和国家杰出青年科学基金资助项目"特提斯喜马拉雅中新生代古海洋学与生烃环境"(项目编号: 49625203) 研究成果。
THE NEW RESEARCHING PROGRESS OF TIBET PLATEAU UPLIFT
Received date: 1998-01-14
Revised date: 1998-06-29
Online published: 1998-12-01
王成善,丁学林 . 青藏高原隆升研究新进展综述[J]. 地球科学进展, 1998 , 13(6) : 526 -532 . DOI: 10.11867/j.issn.1001-8166.1998.06.0526
Since 90's, there have been acquiring a lot of researching achievements about Tibet Plateau uplift owing to better methods and the wider thoughts. It not only emphasized the multi-part, multi-phase, multi-factor of Tibet Plateau uplift, but also found the important function of the deep dynamics, the collision of plates and history of uplift. On the one hand, the diachronism of the India-Eurasia collision is about 10 Ma, so it would not be accurate if thinking of the 45 Ma as the start of the collision; On the other hand, although it is different for different geologist thinking about the uplift history of Tibet Plateau, the Plateau has undergone multi-phase uplift which has been generally acknowledged.
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