首页> 外文期刊>Periodico di mineralogia >The Calabria-Peloritani Orogen, a composite terrane in Central Mediterranean; its overall architecture and geodynamic significance for a pre-Alpine scenario around the Tethyan basin
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The Calabria-Peloritani Orogen, a composite terrane in Central Mediterranean; its overall architecture and geodynamic significance for a pre-Alpine scenario around the Tethyan basin

机译:卡拉布里亚-佩洛里塔尼造山带,地中海中部的复合地层;特提斯盆地周围高山前情景的整体构造和地球动力学意义

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摘要

The Calabria-Peloritani Orogen is an arcuate segment of the peri-Mediterranean orogenic Alpine nappe system that comprises the whole Calabria and the north-eastern sector of Sicily. It comprises the Sila and Catena Costiera Massifs in northern Calabria, the Serre and Aspromonte Massifs in central and southern Calabria, and the Peloritani Mountains in Sicily.
机译:卡拉布里亚-佩洛里塔尼造山带是地中海沿岸造山带高山推覆系统的弧形部分,包括整个卡拉布里亚和西西里岛的东北部。它包括卡拉布里亚北部的Sila和Catena Costiera地块,卡拉布里亚中部和南部的Serre和Aspromonte地块以及西西里岛的Peloritani山。

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