THE TRIASSIC/JURASSIC BOUNDARY IN THE ANDES OF ARGENTINA

THE TRIASSIC/JURASSIC BOUNDARY IN THE ANDES OF ARGENTINA

The Arroyo Malo Formation at Alumbre Creek, on the northern bank of the Atuel River, west central Argentina, comprises a c. 300 m thick continuous marine succession across the Triassic-Jurassic System boundary, consisting of massive and laminated pelites indicative of a slope depositional environmen...

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Bibliographic Details
Main Authors:	ALBERTO C. RICCARDI, SUSANA E. DAMBORENEA, MIGUEL O. MANCEÑIDO, MARIA P. IGLESIA LLANOS
Format:	Article
Language:	English
Published:	Università degli Studi di Milano 2004-03-01
Series:	Rivista Italiana di Paleontologia e Stratigrafia
Online Access:	https://riviste.unimi.it/index.php/RIPS/article/view/6266

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