Comment on: Magalhães et al., Middle Jurassic multi‐scale transgressive–regressive cycles: An example from the Lusitanian Basin, The Depositional Record, 9, 174–202

Author:

Schneider S.1ORCID,Fürsich F. T.2,Werner W.34,Pierce C. S.1

Affiliation:

1. CASP Cambridge UK

2. GeoZentrum Nordbayern, FG Paläoumwelt Friedrich‐Alexander‐Universität Erlangen‐Nürnberg Erlangen Germany

3. Bayerische Staatssammlung für Paläontologie und Geologie Munich Germany

4. GeoBio‐Center LMU Munich Germany

Abstract

This is a comment to an article previously published in The Depositional Record.

Publisher

Wiley

Subject

Paleontology,Stratigraphy,Geology,Environmental Science (miscellaneous),Oceanography

Reference38 articles.

1. Calcareous debris‐flows as evidence for a distally steepened carbonate ramp in west‐central Portugal;Azerêdo A.C.;Comunicações dos Serviços Geológicos de Portugal,1988

2. Formalização da litostratigrafia do Jurássico Inferior e Médio do Maciço Calcário Estremenho (Bacia Lusitânica);Azerêdo A.C.;Comunicações Geológicas,2007

3. Da dinâmica continental no Triásico aos mares do Jurássico Inferior e Médio;Azerêdo A.C.;Cadernos de Geologia de Portugal,2003

4. Carbonate reservoir outcrop analogues with a glance at pore-scale (Middle Jurassic, Lusitanian Basin, Portugal)

5. The Middle‐Upper Jurassic disconformity in the Lusitanian Basin, Portugal: preliminary facies analysis and evidence for palaeoclimatic fluctuation;Azerêdo A.C.;Cuadernos de Geología Iberica,1998

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