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...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Università degli Studi di Milano
2004-03-01
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| Series: | Rivista Italiana di Paleontologia e Stratigrafia |
| Online Access: | https://riviste.unimi.it/index.php/RIPS/article/view/6266 |