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

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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Seamounts
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container_title Acta geologica Sinica (Beijing)
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creator WANG, Yanlin
WANG, Jun
YAN, Pin
QIU, Yan
description 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 southwest sub-basin （SWSB） of the SCS was found with much thin crust and numerous faulted blocks coupling with magma-poor continental margins along its flanks. Therefore, the southwestern part of the SWSB is most likely to be a tectonic-dominated basin. To justify the hypothesis with further evidence, we investigated the nature of seamounts on the southwestern mid-ridge of the SWSB which may inherit seafloor spreading.
doi_str_mv 10.1111/1755-6724.13479
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title An Anomalous Seamount on the Southwestern Mid-Ridge of the South China Sea
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