An Anomalous Seamount on the Southwestern Mid-Ridge of the South China Sea

Objective The development of continental rifting and seafloor spreading can be predominated by magmatic upwelling (magma-rich) or tectonic stretching (magma-poor). Located in the terminal portion of propagating seafloor spreading of the South China Sea (SCS), the southwestern mid-ridge of the southw...

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2017-12, Vol.91 (6), p.2340-2341
Hauptverfasser: WANG, Yanlin, WANG, Jun, YAN, Pin, QIU, Yan
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Sprache:eng
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