Geochemical nature of sub-ridge mantle and opening dynamics of the South China Sea
The Indian-type mantle (i.e., above the north hemisphere reference line on the plot of 208Pb/204Pb vs. 206Pb/204Pb) has been considered as a “Southern Hemisphere” geochemical signature, whose origin remains enigmatic. The South China Sea is an extensional basin formed after rifting of the Euro-Asia...
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Published in | Earth and planetary science letters Vol. 489; pp. 145 - 155 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.05.2018
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Subjects | |
Online Access | Get full text |
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