Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal

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Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal

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作者：Jean-Claude Sibuet^a ; ^b ; ^c ; ^{jean.claude.sibuet@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; Frauke Klingelhoefer^c ; ^{frauke.klingelhoefer@ifremer.fr" class="auth_mail" title="E-mail the corresponding author} ; Yuan-Ping Huang^d ; ^{janushuang711@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; Yi-Ching Yeh^e ; ^{ycyeh@narlabs.org.tw" class="auth_mail" title="E-mail the corresponding author} ; Claude Rangin^f ; ^{rangin@geoazur.unice.fr" class="auth_mail" title="E-mail the corresponding author} ; Chao-Shing Lee^a ; ^{leecs@ntou.edu.tw" class="auth_mail" title="E-mail the corresponding author} ; Shu-Kun Hsu^d ; ^{hsu@ncu.edu.tw" class="auth_mail" title="E-mail the corresponding author}
关键词：Northern Bay of Bengal ; Wide-angle seismic reflection and refraction data ; Thinned continental crust intruded by volcanics
刊名：Marine and Petroleum Geology
出版年：2016
出版时间：November 2016
年：2016
卷：77
期：Complete
页码：471-486
全文大小：13049 K

文摘

•: Refraction velocity models show a sedimentary cover of 13 km minimum beneath the shelf and 7 km minimum beneath the deep ocean.
•: The crust is thinned continental crust, 10–20 km thick.
•: The thinned continental crust is intruded by volcanics, sills and SDRs.
•: Seismic velocities of 7.4 km/s found at the base of the crust is interpreted as magmatic underplating.
•: The thinned continental crust extends from 19°N (northern Bay of Bengal) to 25°N (Shillong Plateau).

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