Modern-style plate subduction preserved in the Palaeoproterozoic West African craton

被引：0
|
作者：
J. Ganne
V. De Andrade
R. F. Weinberg
O. Vidal
B. Dubacq
N. Kagambega
S. Naba
L. Baratoux
M. Jessell
J. Allibon
机构：
[1] IRD,Department of Earth Sciences
[2] UR 234,Département des Géosciences
[3] GET,Department of Mineralogy and Geochemistry
[4] Université Toulouse III,undefined
[5] NSLS II,undefined
[6] Brookhaven National Laboratory,undefined
[7] European Synchrotron Radiation Facility,undefined
[8] School of Geosciences,undefined
[9] Monash University,undefined
[10] IsTerre,undefined
[11] Université J. Fourier,undefined
[12] Maison des Géosciences,undefined
[13] University of Cambridge,undefined
[14] Université de Ouagadougou,undefined
[15] University of Lausanne,undefined
来源：
Nature Geoscience | 2012年 / 5卷 / 1期
关键词：
D O I：
10.1038/ngeo1321
中图分类号：
学科分类号：
摘要：
The timing of onset of modern-style plate tectonics on Earth is debated. Analysis of rocks in the West African metamorphic province, which is more than 2 Gyr old, reveals that some minerals formed under conditions similar to those in modern-day subduction zones, suggesting that subduction occurred on the Palaeoproterozoic Earth.
引用
收藏
页码：60 / 65
页数：5
相关论文
共 47 条
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    Ganne, J.
    De Andrade, V.
    Weinberg, R. F.
    Vidal, O.
    Dubacq, B.
    Kagambega, N.
    Naba, S.
    Baratoux, L.
    Jessell, M.
    Allibon, J.
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