DSpace UNL

RUN >
Faculdade de Ciências e Tecnologia (FCT) >
FCT Departamentos >
FCT: Departamento de Ciências da Terra >
FCT: DCT - Ciências da Terra >

Please use this identifier to cite or link to this item: http://hdl.handle.net/10362/1542

Título: Estratigrafia do Caloviano do Algarve oriental
Autor: Manuppella, G.
Marques, B.
Rocha, R. B.
Palavras-chave: Stratigraphy
Callovian
Algarve
Issue Date: 13-Aug-2008
Resumo: The comparative study of the Callovian sections in eastern Algarve allowed us to demonstrate that the discontinuity surface at the base of Malm lies always over the Lower-Callovian, as opposite to what happens in western Algarve; the Bathonian-Callovian transition, continuous in western Algarve (Mareta beach) is marked, in eastern Algarve, by a generalised discontinuity of variable vertical extention. It is verified that, in eastern Algarve, the Callovian formations are always or at the nucleus of anticlinal structures, probably linked to halokinetic tectonic activity, or in large radins folds derived from compressive phases.
URI: http://hdl.handle.net/10362/1542
Appears in Collections:FCT: DCT - Ciências da Terra

Files in This Item:

File Description SizeFormat
CT_09_03.pdf1,96 MBAdobe PDFView/Open
Statistics
FacebookTwitterDeliciousLinkedInDiggGoogle BookmarksMySpaceOrkut
Formato BibTex mendeley Endnote Logotipo do DeGóis 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

Universidade Nova de Lisboa  - Feedback
Estamos no RCAAP Governo Português separator Ministério da Educação e Ciência   Fundação para a Ciência e a Tecnologia

Financiado por:

POS_C UE