Staff View: Late Paleogene rifting along the Malay Peninsula thickened crust

Late Paleogene rifting along the Malay Peninsula thickened crust

Sedimentary basins often develop above internal zones of former orogenic belts. We hereafter consider the Malay Peninsula (Western Sunda) as a crustal high separating two regions of stretched continental crust; the Andaman/Malacca basins in the western side and the Thai/Malay basins in the east....

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Main Author:	Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, .
Format:	Article
Institution:	Universiti Teknologi Petronas
Record Id / ISBN-0:	utp-eprints.12228 /
Published:	2016
Subjects:	QE Geology
Online Access:	http://www.sciencedirect.com/science/article/pii/S0040195116305893 http://eprints.utp.edu.my/12228/
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id	utp-eprints.12228
recordtype	eprints
spelling	utp-eprints.122282017-06-05T08:05:25Z Late Paleogene rifting along the Malay Peninsula thickened crust Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, . QE Geology Sedimentary basins often develop above internal zones of former orogenic belts. We hereafter consider the Malay Peninsula (Western Sunda) as a crustal high separating two regions of stretched continental crust; the Andaman/Malacca basins in the western side and the Thai/Malay basins in the east. Several stages of rifting have been documented thanks to extensive geophysical exploration. 2016-11 Article PeerReviewed http://www.sciencedirect.com/science/article/pii/S0040195116305893 Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, . (2016) Late Paleogene rifting along the Malay Peninsula thickened crust. Late Paleogene rifting along the Malay Peninsula thickened crust . http://eprints.utp.edu.my/12228/
institution	Universiti Teknologi Petronas
collection	UTP Institutional Repository
topic	QE Geology
spellingShingle	QE Geology Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, . Late Paleogene rifting along the Malay Peninsula thickened crust
description	Sedimentary basins often develop above internal zones of former orogenic belts. We hereafter consider the Malay Peninsula (Western Sunda) as a crustal high separating two regions of stretched continental crust; the Andaman/Malacca basins in the western side and the Thai/Malay basins in the east. Several stages of rifting have been documented thanks to extensive geophysical exploration.
format	Article
author	Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, .
author_sort	Benjamin Sautter, Manuel Pubellier, Pierre Jousselin, Paolo Datt, .
title	Late Paleogene rifting along the Malay Peninsula thickened crust
title_short	Late Paleogene rifting along the Malay Peninsula thickened crust
title_full	Late Paleogene rifting along the Malay Peninsula thickened crust
title_fullStr	Late Paleogene rifting along the Malay Peninsula thickened crust
title_full_unstemmed	Late Paleogene rifting along the Malay Peninsula thickened crust
title_sort	late paleogene rifting along the malay peninsula thickened crust
publishDate	2016
url	http://www.sciencedirect.com/science/article/pii/S0040195116305893 http://eprints.utp.edu.my/12228/
_version_	1741196158553817088
score	11.62408

Late Paleogene rifting along the Malay Peninsula thickened crust

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