通过南里夫走廊从托尔顿到现在的大西洋和地中海之间的通信:cap des Trois Fourches地区(Rif Oriental,摩洛哥)新一代盆地的顺序地层学

A. Azdimousa , J. Bourgois
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引用次数: 17

摘要

将层序地层学的概念应用于三头盖地区新近系“后推覆”盆地。它可以通过这一关键区域对比序列和不整合面,并重建过去10万年通过南里夫海峡的大西洋-地中海门户的发展。在这一时期,主要受海平面变化控制的沉积物堆积记录了构造和火山活动。大西洋-地中海的门户分别在上托尔顿期和上墨西尼亚期的200至500年间被切断。今天的情况开始于上新世时期。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Les communications entre l'Atlantique et la Méditerranée par le couloir sud-rifain du Tortonien à l'actuel: stratigraphie séquentielle des bassins néogènes de la région du cap des Trois Fourches (Rif Oriental, Maroc)

The sequence stratigraphic concepts are applied to the Neogene “post-nappes” basins of the Cap des Trois Fourches area. It allows to correlate sequences and unconformities through this key area and reconstruct the development of the Atlantic-Mediterranean gateway through the South Riffian strait for the past 10 Ma. During this period of time, the sediment accumulation which was controlled essentially by sea level changes, have recorded tectonics and volcanics pulses. The Atlantic-Mediterranean gateways were cut off during two short period of times of 200 to 500 kyr that occurred during the Upper Tortonian and the Upper Messinian, respectively. The present day situation began during Upper Pliocene time.

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