Ponded melt at the boundary between the lithosphere and asthenosphere

被引：0

作者：

Tatsuya Sakamaki

Akio Suzuki

Eiji Ohtani

Hidenori Terasaki

Satoru Urakawa

Yoshinori Katayama

Ken-ichi Funakoshi

Yanbin Wang

John W. Hernlund

Maxim D. Ballmer

机构：

[1] Tohoku University,Department of Earth and Planetary Materials Science

[2] Osaka University,Department of Earth and Space Science

[3] Okayama University,Department of Earth Sciences

[4] Japan Atomic Energy Agency,Department of Earth and Planetary Science

[5] SPring-8,Department of Geology and Geophysics

[6] Japan Synchrotron Radiation Research Institute,undefined

[7] Center for Advanced Radiation Sources,undefined

[8] The University of Chicago,undefined

[9] Chicago,undefined

[10] University of California,undefined

[11] School of Ocean and Earth Sciences and Technology,undefined

[12] University of Hawaii at Manoa,undefined

[13] Present address: Earth-Life Science Institute,undefined

[14] Tokyo Institute of Technology,undefined

[15] Meguro-ku,undefined

[16] Tokyo 152-8550,undefined

[17] Japan,undefined

来源：

Nature Geoscience | 2013年 / 6卷

关键词：

D O I：

暂无

中图分类号：

学科分类号：

摘要：

The boundary between Earth’s rigid lithosphere and ductile asthenosphere is marked by a seismic discontinuity. Laboratory experiments on basaltic magmas show that melts should pond at pressures that correspond to the lithosphere–asthenosphere boundary. Thus, magma ponding could explain the observed seismic discontinuity.

引用

页码：1041 / 1044

页数：3

共 50 条

[1] Ponded melt at the boundary between the lithosphere and asthenosphere
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[J]. NATURE GEOSCIENCE, 2013, 6 (12) : 1041 - 1044
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