Long-term interaction between mid-ocean ridges and mantle plumes

被引：1
作者：
J. M. Whittaker
J. C. Afonso
S. Masterton
R. D. Müller
P. Wessel
S. E. Williams
M. Seton
机构：
[1] Institute for Marine and Antarctic Studies,
[2] University of Tasmania,undefined
[3] Macquarie University,undefined
[4] Leeds University,undefined
[5] School of Geosciences,undefined
[6] University of Sydney,undefined
[7] School of Ocean and Earth Science and Technology,undefined
[8] University of Hawaii,undefined
[9] Present address: Getech Plc,undefined
[10] Kitson House,undefined
[11] Elmete Hall,undefined
[12] Elmete Lane,undefined
[13] Leeds LS28 2LL,undefined
[14] UK.,undefined
来源：
Nature Geoscience | 2015年 / 8卷 / 6期
关键词：
D O I：
10.1038/ngeo2437
中图分类号：
学科分类号：
摘要：
Tectonic plate and lower-mantle motions are often considered independent. Plate tectonic reconstructions reveal long-lived interactions between mantle plumes and mid-ocean ridges that imply feedback between plate boundaries and the deep mantle.
引用
收藏
页码：479 / 483
页数：4
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