Linking time-equivalent paleosols and lacustrine rocks to reconstruct paleoclimate in the Ischigualasto Basin, NW Argentina
Field relationships between the coeval Ischichuca and Chanares Formations in the southern part of the Ischigualasto rift basin, northwestern Argentina, combined with mineralogical, geochemical, and petrographic analyses demonstrates that the climate was semi-arid to semi-humid during the Middle Tria...
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| Language: | en_US |
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The University of Arizona.
2001
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| Online Access: | http://hdl.handle.net/10150/279903 |