Eogenetic diagenesis of Chinle sandstones, Petrified Forest National Park (Arizona, USA): A record of Late Triassic climate change
Author:
Affiliation:
1. Department of Geosciences; Baylor University; Waco TX USA
Funder
American Association of Petroleum Geologists
Baylor University
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12421/fullpdf
Reference81 articles.
1. Triassic bentonite of the Painted Desert;Allen;Am. J. Sci.,1930
2. A linkage among Pangean tectonism, cyclic alluviation, climate change, and biologic turnover in the Late Triassic: the record from the Chinle Formation, southwestern United States;Atchley;J. Sediment. Res.,2014
3. Timing of magmatism following initial vonvergence at a passive margin, southwestern U.S. Cordillera, and ages of lower crustal magma sources;Barth;J. Geol.,2006
4. Paleomagnetism of the Chinle and Kayenta Formations, New Mexico and Arizona;Bazard;J. Geophys. Res.,1991
5. Palaeo-climate controlled diagenesis of the Westphalian C & D fluvial sandstones in the Campine Basin (north-east Belgium);Bertier;Sedimentology,2008
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