Jointing patterns and tectonic evolution of the Maciço Calcário Estremenho, Lusitanian Basin, Portugal

• Autor(a) principal: Carvalho, Jorge
• Data de Publicação: 2018
• Tipo de documento: Artigo
• Idioma: eng
• Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
• Texto Completo: http://hdl.handle.net/10400.9/3171
• topic: Tectónica; Maciço Calcário Estremenho (Portugal); Bacia Lusitânica (Portugal)

ABSTRACT: The Macico Calcario Estremenho (MCE) is an uplifted Jurassic limestone massif unit of the Lusitanian Basin, Portugal, where five main joint sets trending NNE-SSW, WSW-ENE, WNW-ESE, NW-SE, and NNW-SSE are recognized. Except for the NNW-SSE set, all the other sets host calcite veins and barren joints, evidencing a multistage development by several deformation episodes, including shear reactivation. Orthogonal patterns defined by the NNE-SSW/WNW-ESE and NNW-SSE/WSW-ENE systems are characteristic of some tectonos-tratigraphic units of the MCE, but the sets of each one of the systems are genetically independent. They result from specific deformation episodes undergone by the studied area in the course of its Meso-Cenozoic evolution. NNE-SSW calcite veins were the first to form during Middle Jurassic fault-controlled subsidence. A renewal of this set as barren joints took place during the Eocene Pyrenean compressive phase. The WSW-ENE and WNW-ESE sets have a restricted spatial distribution and relate to transient compressive episodes of the Middle - Late Jurassic and Jurassic - Cretaceous transitions, respectively. The NW-SE set, also characteristic of a specific region, formed during the Late Jurassic rifting and is related to local NE-SW tension dependent on block tilting towards a major NW-SE fault. The Miocene Betic compressive phase is responsible for the formation of the NNW-SSE set, which is widespread throughout the MCE.