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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Online Access: | http://paleopolis.rediris.es/cg/CG2007_M02/CG2007_M02_Abstract07.html |
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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 |
_version_ |
1725412434387140608 |