The Carnian Pluvial Event in the Tofane area (Cortina d‘Ampezzo, Dolomites, Italy)
The Carnian Pluvial Event in the Tofane area (Cortina d‘Ampezzo, Dolomites, Italy)
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发表时间：
2009
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影响因子：
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通讯作者：
A. Breda;N. Preto;G. Roghi;S. Furin;R. Meneguolo;E. Ragazzi;P. Fedele;P. Gianolla
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作者：
A. Breda;N. Preto;G. Roghi;S. Furin;R. Meneguolo;E. Ragazzi;P. Fedele;P. Gianolla
“卡尼期洪水事件”一词是指降雨量增加的一次事件，它对卡尼期海洋和大陆沉积系统产生了明显且广泛的影响。根据菊石和牙形刺生物地层学，它的起源可以追溯到最晚的早卡尼世（儒略世）（图2）。最初被认为是北阿尔卑斯山地层演化的主要翻转之一（Schlager 和 Schöllnberger 的“Reingrabener Wende”，1974 年），后来被解释为向
The term “Carnian Pluvial Event” denotes an episode of increased rainfall which had a well recognizable and widespread influence on Carnian marine and continental sedimentary systems. Its onset is dated to the latest Early Carnian (Julian), by ammonoid and conodont biostratigraphy (Fig. 2). Initially identified as one of the major turnovers in the stratigraphic evolution of the Northern Calcareous Alps (the “Reingrabener Wende” of Schlager and Schöllnberger, 1974), it was then interpreted as a shift towards