Palynology, Stratigraphy and Geometry of the Pennsylvanian continental Santa Susana Basin (SW Portugal)

Journal of Iberian geology

P. Almeida¹  G. Machado²  I. Dias da Silva³ 

[1] Centro de Geofísica de Évora, Dep. de Física da Universidade de Évora.Laboratorio de Investigação em Rochas Industriais e Ornamentais, Pólo de Estremoz da Universidade de Évora;Galp Energia E&P.Centro de Geologia da Universidade de Lisboa;Instituto Geológico y Minero de España, Unidad de Salamanca

关键词: Santa Susana Basin;   

DOI  :  10.5209/rev_JIGE.2012.v38.n2.40467

学科分类：地质学

来源: Universidad Complutense de Madrid * Servicio de Publicaciones

【 摘 要 】

The continental Pennsylvanian Santa Susana Basin (SSB) is located along an important N-S strike shear zone (Santa Susana Shear Zone - SSSZ) that separates the Ossa-Morena and South Portuguese Zones (SW Portugal). This shear zone controlled the sedimentation of the basin and probably its post-sedimentary evolution. The lower (basal) unit is mostly conglomeratic and is known essentially from drill-hole data while the upper unit, that covers most of the current surface area, is composed by sandstones, shales and some coal beds. Fluvial sedimentary rocks seem to prevail, but evidences of lacustrine sedimentation can be found in restricted areas within the upper unit. Palynological data indicate that at least part of the sedimentation took place during the Early Kasimovian (Cantabrian) but the sporomorph content of different localities suggest that significantly older sediments (Late Moscovian -Early Bashkirian) may be present. Geometrical, structural, and cartographical evidences indicate that the SSB formed as a pull-apart basin along the SSSZ and was later partially uplifted during latest Varsican and Alpine orogenies.>

【 授权许可】

Unknown