91人妻人人澡人人爽人人DVD|日韩激情天堂国产av综合网|91国产1区av天堂网|一级国产A片AV无码网站|爱综合偷排网国产成人片|日韩高免费五码视频|欧美黄色A级片|a毛三级久久99|深夜无码激情人妻黄片看黄片|A片成人免费视频网站

Mantle plumes: Why the current skept

時間:2023-05-01 01:50:16 生物醫(yī)學(xué)論文 我要投稿
  • 相關(guān)推薦

Mantle plumes: Why the current skepticism?

The present reappraisal of the mantle plume hypothesis is perhaps the most exciting current debate in Earth science. Nevertheless, the fundamental reasons for why it has arisen are often not well understood. They are that 1) many observations do not agree with the predictions of the original model, 2) it is possible that convection of the sort required to generate thermal plumes in the Earth's mantle does not occur, 3) so many variants of the original model have been invoked to accommodate conflicting data that the plume hypthesis is in practice no longer testable, and 4) alternative models are viable, though these have been largely neglected by researchers. Regardless of the final outcome, the present vigorous debate is to be welcomed since it is likely to stimulate new discoveries in a way that unquestioning acceptance of the conventional plume model will not.

作 者: Gillian R. Foulger   作者單位: Department of Earth Sciences, Science Laboratories, University of Durham, South Rd., Durham DH1 3LE, U.K.  刊 名: 科學(xué)通報(英文版)  SCI 英文刊名: CHINESE SCIENCE BULLETIN  年,卷(期): 2005 50(15)  分類號: Q95  關(guān)鍵詞: plume   volcanism   hotspots   convection   mantle   plate tectonics  

【Mantle plumes: Why the current skept】相關(guān)文章:

Parafermion Fields Constructed by Current Algebra04-29

Some Thoughts on Current Education in China05-04

Environmental radioactivity level at a mantle factory in eastern Zhejiang04-27

Why Is Writing So Difficult?05-04

Effect of a Small Current Quark Mass on Bag Constant04-29

Why Illness Always Accompanied by Vulnerability04-25

Why Electrolytic Aluminum Overcapacity Lingering for Years04-30

不定式的特殊句型Why not05-04

Effect of the integrated time of the induced current signal on the position resolution of the RPC detector04-28

Velocity structure of the crust and uppermost mantle in the boundary area of the Tianshan Mountains and the Tarim Basin04-29