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首页> 外文期刊>Geodinamica Acta >Dykes and Pipes of Remobilized Cornieules within the Cornieule Evaporitic-Complex of the Mont Jovet Area (Northwestern French Alps)
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Dykes and Pipes of Remobilized Cornieules within the Cornieule Evaporitic-Complex of the Mont Jovet Area (Northwestern French Alps)

机译：蒙特约维特地区（法国西北阿尔卑斯山）的角质层蒸发复合物中的带动角质层的堤坝和管道

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摘要

Dykes and pipes of remobilized cornieules outcrop widely within the evaporitic complex of the thrust sole of the Mont Jovet klippe, (North-Western French Alps). The morphology, nature, structures and pattern of these rocks are described. The bodies are not linked to erosive processes; they represent inherited morphologies within the gypsum exhumed by erosion. These upstanding pseudo-cornieules very likely originated from fault-related remobilization of primary cornieules from the tectonic contact. A genetic model is proposed to explain the genesis of these pseudo-cornieules, to highlight the possible relationships between these pseudo-cornieules and the other documented types of cornieules. (C) 2010 Lavoisier SAS. All rights reserved
机译：堤防和移动的小管的管道在Mont Jovet klippe（法国西北阿尔卑斯山）的逆冲底板的蒸发复合物中广泛露头。描述了这些岩石的形态，性质，结构和样式。尸体与侵蚀过程无关;它们代表了因侵蚀而发掘出的石膏中的继承形态。这些直立的伪角质层很可能源自与构造接触的初级角质层的断层相关移动。提出了遗传模型来解释这些假角质的起源，以突出这些假角质与其他已记录类型的角质之间的可能关系。 （C）2010 Lavoisier SAS。版权所有

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