On the trail of a major trans-Tethyan discontinuity

At the base of the Valanginian a major discontinuity associated with one of the major transgressions of the Cretaceous is nominated as a candidate for the boundary between the Cretaceous and Jurassic systems. This surface has been identified in both platform and basinal domains, at the eastern edge...

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Bibliographic Details
Main Author: Granier Bruno
Format: Article
Language:English
Published: Rediris 2007-05-01
Series:Carnets de Géologie
Subjects:
Online Access:http://paleopolis.rediris.es/cg/CG2007_M02/CG2007_M02_Abstract07.html
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spelling doaj-42d794df0ebc4440833864c2c4ba514b2020-11-25T00:09:21ZengRedirisCarnets de Géologie1765-25531634-07442007-05-01CG2007M02_Abstract07On the trail of a major trans-Tethyan discontinuityGranier BrunoAt the base of the Valanginian a major discontinuity associated with one of the major transgressions of the Cretaceous is nominated as a candidate for the boundary between the Cretaceous and Jurassic systems. This surface has been identified in both platform and basinal domains, at the eastern edge of the North American continent and in the Middle East, as well as through the western edge of Africa and Europe.http://paleopolis.rediris.es/cg/CG2007_M02/CG2007_M02_Abstract07.htmlJurassicCretaceousTithonianBerriasianValanginianboundarystagessystemsperiods
collection DOAJ
language English
format Article
sources DOAJ
author Granier Bruno
spellingShingle Granier Bruno
On the trail of a major trans-Tethyan discontinuity
Carnets de Géologie
Jurassic
Cretaceous
Tithonian
Berriasian
Valanginian
boundary
stages
systems
periods
author_facet Granier Bruno
author_sort Granier Bruno
title On the trail of a major trans-Tethyan discontinuity
title_short On the trail of a major trans-Tethyan discontinuity
title_full On the trail of a major trans-Tethyan discontinuity
title_fullStr On the trail of a major trans-Tethyan discontinuity
title_full_unstemmed On the trail of a major trans-Tethyan discontinuity
title_sort on the trail of a major trans-tethyan discontinuity
publisher Rediris
series Carnets de Géologie
issn 1765-2553
1634-0744
publishDate 2007-05-01
description At the base of the Valanginian a major discontinuity associated with one of the major transgressions of the Cretaceous is nominated as a candidate for the boundary between the Cretaceous and Jurassic systems. This surface has been identified in both platform and basinal domains, at the eastern edge of the North American continent and in the Middle East, as well as through the western edge of Africa and Europe.
topic Jurassic
Cretaceous
Tithonian
Berriasian
Valanginian
boundary
stages
systems
periods
url http://paleopolis.rediris.es/cg/CG2007_M02/CG2007_M02_Abstract07.html
work_keys_str_mv AT granierbruno onthetrailofamajortranstethyandiscontinuity
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