Late Ordovician ice-marginal processes and sea-level change from the north Gondwana platform: Evidence from the Valongo Anticline (northern Portugal)-Reference-Cited by-同舟云学术

Late Ordovician ice-marginal processes and sea-level change from the north Gondwana platform: Evidence from the Valongo Anticline (northern Portugal)

Published:2013-04 Issue: Volume:375 Page:1-15
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Couto Helena,Knight Jasper,Lourenço Alexandre

Funder

Centro de Geologia da Universidade do Porto (CGUP),

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference72 articles.

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3. Sedimentos glaciomarinos del Ordovícico terminal en la Zona Cantábrica (NO de España);Bernárdez;Geogaceta,2006

4. Hirnantian glaciomarine diamictites—evidence for the spread of glaciations and its effect on Upper Ordovician faunas;Brenchley;Geological Survey of Canada,1991

5. Cooper, H., 1980. The stratigraphy and palaeontology of the Ordovician to Devonian rocks of the area North of Dornes (near Figueiró dos Vinhos), central Portugal. Unpublished PhD thesis, Sheffield University, 378 pp.

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