Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response

Rogério Eduardo Bordalo da Rocha; José Carlos Ribeiro Kullberg

Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response

Rogério Eduardo Bordalo da Rocha, José Carlos Ribeiro Kullberg

DCT - Departamento de Ciências da Terra

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Abstract

In this paper we present the general tectonic framework that conditioned the evolution of the Lusitanian Basinduring the Jurassic, when most of the filling of the basin was accumulated. The rifting episodes and the evolutionof the basin's geometry are presented and their close relation with the main basin-wide unconformities isdiscussed. The unconformity bounded sequences are briefly presented, in order to understand the evolution of thesedimentary environments. This constitutes the basic geological information to make the palaeogeographicalmaps presented in Part II of this paper (in this volume).

Original language	English
Title of host publication	Ciências da Terra, volume especial
Editors	Jacques Rey
Place of Publication	Monte da Caparica
Publisher	Departamento de Ciências da Terra, FCT/UNL
Pages	205
Volume	7
ISBN (Print)	978-972-8893-09-5
Publication status	Published - 1 Jan 2013
Event	1st International Congress on Stratigraphy (STRATI 2013) - Lisbon, Portugal Duration: 1 Jul 2013 → 7 Jul 2013

Conference

Conference	1st International Congress on Stratigraphy (STRATI 2013)
Country/Territory	Portugal
City	Lisbon
Period	1/07/13 → 7/07/13

Cite this

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title = "Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response",

abstract = "In this paper we present the general tectonic framework that conditioned the evolution of the Lusitanian Basinduring the Jurassic, when most of the filling of the basin was accumulated. The rifting episodes and the evolutionof the basin's geometry are presented and their close relation with the main basin-wide unconformities isdiscussed. The unconformity bounded sequences are briefly presented, in order to understand the evolution of thesedimentary environments. This constitutes the basic geological information to make the palaeogeographicalmaps presented in Part II of this paper (in this volume).",

keywords = "unconformities, Jurassic, Lusitanian Basin, tectono-stratigraphical evolution, palaeoenvironments",

author = "Rocha, {Rog{\'e}rio Eduardo Bordalo da} and Kullberg, {Jos{\'e} Carlos Ribeiro}",

year = "2013",

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booktitle = "Ci{\^e}ncias da Terra, volume especial",

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note = "1st International Congress on Stratigraphy (STRATI 2013) ; Conference date: 01-07-2013 Through 07-07-2013",

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Rocha, REBD & Kullberg, JCR 2013, Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response. in J Rey (ed.), Ciências da Terra, volume especial. vol. 7, Departamento de Ciências da Terra, FCT/UNL, Monte da Caparica, pp. 205, 1st International Congress on Stratigraphy (STRATI 2013), Lisbon, Portugal, 1/07/13.

Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response. / Rocha, Rogério Eduardo Bordalo da ; Kullberg, José Carlos Ribeiro.
Ciências da Terra, volume especial. ed. / Jacques Rey. Vol. 7 Monte da Caparica: Departamento de Ciências da Terra, FCT/UNL, 2013. p. 205.

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

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AB - In this paper we present the general tectonic framework that conditioned the evolution of the Lusitanian Basinduring the Jurassic, when most of the filling of the basin was accumulated. The rifting episodes and the evolutionof the basin's geometry are presented and their close relation with the main basin-wide unconformities isdiscussed. The unconformity bounded sequences are briefly presented, in order to understand the evolution of thesedimentary environments. This constitutes the basic geological information to make the palaeogeographicalmaps presented in Part II of this paper (in this volume).

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Palaeogeographical evolution of the Lusitanian Basin (Portugal) during the Jurassic: Part I: the tectonical constraints and the sedimentary response

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