Pérmico continental en España.

C. Virgili, Amparo Ramos, A. Sopeña, S. Costa
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引用次数: 8

Abstract

The present data show that the Spanish Permian is represented by the «Autunian» (Lower Rotliegendes) in a typical grey facies and redbeds similar to the «Saxonian» (Upper Rotliegendes). The Upper Permian has been found only in a very few points. In general it is made of detrital series, from clays to conglomerates; some volcanic levels are found. Tickness is very variable, up to 2.000 meters. Sedimentation takes place in continental basins, tectonically con troled 1w the tardihercynian pbases. Their caracteristics and problenis are similar to the ones of Western European Permian. 1.
目前的资料表明,西班牙二叠系以“奥图尼亚”(下罗特列根系)为代表,具有典型的灰色相和类似于“萨克森”(上罗特列根系)的红色层。上二叠统只在少数几个地方被发现。一般来说,它是由碎屑系列组成的,从粘土到砾岩;发现了一些火山水平。海拔高度变化很大,最高可达2000米。沉积作用发生在陆相盆地,在构造上受迟发西期基底控制。它们的特征和存在的问题与西欧二叠系相似。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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