维琴蒂尼前山晚三叠纪构造活动的证据

IF 1.6 3区地球科学 Q2 GEOLOGY Rivista Italiana Di Paleontologia E Stratigrafia Pub Date : 2020-04-29 DOI:10.54103/2039-4942/13383

V. DE ZANCHE, P. Mietto

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引用次数: 1

摘要

在雷科阿罗地区（意大利北部），多洛米亚-普林卡勒地层（上三叠统）的下部夹杂着一种槽状角砾岩，其中含有大量的结晶基底变质碎屑，这种角砾岩被解释为一种河道沉积物，它暂时中断了多洛米亚-普林卡勒地层的循环沉积。这一事件与当地的构造阶段有关，不稳定性可能与涉及雷科罗地区南部的更重要构造活动有关。

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TESTIMONIANZE Dl ATTIVITA' TETTONICA TARDOTRIASSICA NELLE PREALPI VICENTINE

In the Recoaro area (Northern Italy) a channelized breccia containing abundant metamorphic clasts of the crystalline basement is interbedded in the Iower part of the Dolomia Principale formation (Upper Triassic) The breccia is interpreted as a fluvial deposit, which momentarily interrupted the cyclic sedimentation of the Dolomia Principale. This event is connected with a local tectonic phase The instability rnay be related to a more important tectonic activity which involved a region located South of the Recoaro area.

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来源期刊

Rivista Italiana Di Paleontologia E Stratigrafia 地学-地质学

CiteScore

3.60

自引率

4.30%

发文量

审稿时长

>12 weeks

期刊介绍： The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.