Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal”
The northern Bay of Bengal velocity-depth profiles do not follow the velocity-depth curve of the North Atlantic volcanic margins, and only partially the Kerguelen velocity-depth curves. Deep seismic refraction and reflection profiles acquired across the Hatton bank and Feroes ridge show that the mel...
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Online Access: | https://archimer.ifremer.fr/doc/00393/50459/51192.pdf https://doi.org/10.1016/j.marpetgeo.2017.07.023 https://archimer.ifremer.fr/doc/00393/50459/ |
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ftarchimer:oai:archimer.ifremer.fr:50459 2023-05-15T17:32:48+02:00 Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” Sibuet, Jean-claude Klingelhoefer, Frauke Yeh, Yi-ching Rangin, Claude Lee, Chao-shing 2017-12 application/pdf https://archimer.ifremer.fr/doc/00393/50459/51192.pdf https://doi.org/10.1016/j.marpetgeo.2017.07.023 https://archimer.ifremer.fr/doc/00393/50459/ eng eng Elsevier Sci Ltd https://archimer.ifremer.fr/doc/00393/50459/51192.pdf doi:10.1016/j.marpetgeo.2017.07.023 https://archimer.ifremer.fr/doc/00393/50459/ 2017 Elsevier Ltd. All rights reserved. info:eu-repo/semantics/openAccess restricted use Marine And Petroleum Geology (0264-8172) (Elsevier Sci Ltd), 2017-12 , Vol. 88 , P. 1126-1129 Northern Bay of Bengal Wide-angle and reflection seismic profiles Multichannel seismic profiles Thinned continental crust intruded by volcanics text Publication info:eu-repo/semantics/article 2017 ftarchimer https://doi.org/10.1016/j.marpetgeo.2017.07.023 2021-09-23T20:29:44Z The northern Bay of Bengal velocity-depth profiles do not follow the velocity-depth curve of the North Atlantic volcanic margins, and only partially the Kerguelen velocity-depth curves. Deep seismic refraction and reflection profiles acquired across the Hatton bank and Feroes ridge show that the melt is intruded into the lower thinned continental crust as sills, which cross-cut the continental fabric rather than underplating as it was often assumed in the past. Compared with the SCS northern margin proxy, we still suggest that the BoB crust is thinned continental crust intruded by post-rifting volcanics, as also shown by the interpretation of the numerous high-quality deep MCS profiles we collected there. What was supposed to be underplating might be sills intruded through the lower thinned continental crust. Article in Journal/Newspaper North Atlantic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Hatton Bank ENVELOPE(-18.000,-18.000,58.583,58.583) Kerguelen Marine and Petroleum Geology 88 1126 1129 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Northern Bay of Bengal Wide-angle and reflection seismic profiles Multichannel seismic profiles Thinned continental crust intruded by volcanics |
spellingShingle |
Northern Bay of Bengal Wide-angle and reflection seismic profiles Multichannel seismic profiles Thinned continental crust intruded by volcanics Sibuet, Jean-claude Klingelhoefer, Frauke Yeh, Yi-ching Rangin, Claude Lee, Chao-shing Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
topic_facet |
Northern Bay of Bengal Wide-angle and reflection seismic profiles Multichannel seismic profiles Thinned continental crust intruded by volcanics |
description |
The northern Bay of Bengal velocity-depth profiles do not follow the velocity-depth curve of the North Atlantic volcanic margins, and only partially the Kerguelen velocity-depth curves. Deep seismic refraction and reflection profiles acquired across the Hatton bank and Feroes ridge show that the melt is intruded into the lower thinned continental crust as sills, which cross-cut the continental fabric rather than underplating as it was often assumed in the past. Compared with the SCS northern margin proxy, we still suggest that the BoB crust is thinned continental crust intruded by post-rifting volcanics, as also shown by the interpretation of the numerous high-quality deep MCS profiles we collected there. What was supposed to be underplating might be sills intruded through the lower thinned continental crust. |
format |
Article in Journal/Newspaper |
author |
Sibuet, Jean-claude Klingelhoefer, Frauke Yeh, Yi-ching Rangin, Claude Lee, Chao-shing |
author_facet |
Sibuet, Jean-claude Klingelhoefer, Frauke Yeh, Yi-ching Rangin, Claude Lee, Chao-shing |
author_sort |
Sibuet, Jean-claude |
title |
Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
title_short |
Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
title_full |
Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
title_fullStr |
Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
title_full_unstemmed |
Reply to the comment of Talwani et al. (2017) on the Sibuet et al. (2016) paper entitled “Thinned continental crust intruded by volcanics beneath the northern Bay of Bengal” |
title_sort |
reply to the comment of talwani et al. (2017) on the sibuet et al. (2016) paper entitled “thinned continental crust intruded by volcanics beneath the northern bay of bengal” |
publisher |
Elsevier Sci Ltd |
publishDate |
2017 |
url |
https://archimer.ifremer.fr/doc/00393/50459/51192.pdf https://doi.org/10.1016/j.marpetgeo.2017.07.023 https://archimer.ifremer.fr/doc/00393/50459/ |
long_lat |
ENVELOPE(-18.000,-18.000,58.583,58.583) |
geographic |
Hatton Bank Kerguelen |
geographic_facet |
Hatton Bank Kerguelen |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Marine And Petroleum Geology (0264-8172) (Elsevier Sci Ltd), 2017-12 , Vol. 88 , P. 1126-1129 |
op_relation |
https://archimer.ifremer.fr/doc/00393/50459/51192.pdf doi:10.1016/j.marpetgeo.2017.07.023 https://archimer.ifremer.fr/doc/00393/50459/ |
op_rights |
2017 Elsevier Ltd. All rights reserved. info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1016/j.marpetgeo.2017.07.023 |
container_title |
Marine and Petroleum Geology |
container_volume |
88 |
container_start_page |
1126 |
op_container_end_page |
1129 |
_version_ |
1766131073099497472 |