Ordovician K-bentonites in the upper-plate active margin of Western Gondwana, (Famatina Ranges): Stratigraphic and palaeogeographic significance
- 25 September 2006
- journal article
- Published by Elsevier in Gondwana Research
- Vol. 11 (3) , 311-325
- https://doi.org/10.1016/j.gr.2006.05.005
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Terra Australis Orogen: Rodinia breakup and development of the Pacific and Iapetus margins of Gondwana during the Neoproterozoic and PaleozoicPublished by Elsevier ,2004
- Ordovician back arc foreland and Ocloyic thrust belt development on the western Gondwana margin as a response to Precordillera terrane accretionTectonics, 2004
- “Proterozoic–Early Paleozoic evolution in western South America—a discussion” in: Tectonophysics, 354: 121–137 (2002)Tectonophysics, 2003
- EARLY ORDOVICIAN (ARENIG) BRACHIOPODS FROM VOLCANICLASTIC ROCKS OF THE FAMATINA RANGE, NORTHWEST ARGENTINAJournal of Paleontology, 2003
- El Grupo Cerro Morado (Ordovícico Medio) en el Famatina (28-29°S), Andes centrales del oeste argentinoRevista geológica de Chile, 2002
- Proterozoic–Early Paleozoic evolution in western South America—a discussionPublished by Elsevier ,2002
- Characterization of mixed-layer illite-smectite from bentonites using microscopic, chemical, and X-ray methods; constraints on the smectite-to-illite transformation mechanismAmerican Mineralogist: Journal of Earth and Planetary Materials, 1998
- The early Paleozoic evolution of the Argentine Precordillera as a Laurentian rifted, drifted, and collided terrane: A geodynamic modelGSA Bulletin, 1995
- Model for K-bentonite formation: Evidence from zoned K-bentonites in the disturbed belt, MontanaGeology, 1984
- Spatial distribution of earthquakes and subduction of the Nazca plate beneath South AmericaGeology, 1976