Late Variscan events in the outer Ligurian Briançonnais.

R. Cabella, L. Cortesogno, G. Dallagiovanna, R. Vannucci, M. Vanossi
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引用次数: 1

Abstract

In ihe Ligurian Brian9onnais domain a late Variscan sequence of volcanie, mainly ignimbritic, and sedimentary continental deposits filled up graben and halfgraben struciures,bordered by two seis of syngeneticfaults (presently trendingnearlyE-Wand N-S), during tree man phases. The oldestone,ofWestphalian-Siephanian age, was accompanied by calc-alkaline rhyolite; ihe second one, of middle (7) Siephanian age, is marked by «shoshonitic» andesites; te last, early Permian one, gaye buge volumesof calc-alkaline rhyolitic to dacitic volcanics and was closed by a K-rhyolitic event. No volcanism is associaied with te uncamformably overlying late Permian continental coarse deposiis (Verrucano).
外利古里亚布里阿尼奥纳斯的晚期瓦利斯会事件。
在利古里亚-布里奥内斯域,一个以火成岩为主的晚瓦里西斯火山层序和沉积陆相沉积,在树人期填满了地堑和半地堑构造,并与两组同生断裂(目前走向近北北北南)接壤。最古老的岩石为威斯特伐利亚-西法尼亚时代,伴有钙碱性流纹岩;第二个是西番尼亚中期(7),以“肖肖尼”安山岩为标志;最后一个是早二叠世,由大量钙碱性流纹岩到英白质火山岩组成,并被钾流纹岩事件关闭。没有火山作用与不平整的上覆晚二叠世大陆粗沉积(Verrucano)有关。
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