Controls on synchronous ephemeral- and perennial-river sedimentation in the middle sandstone member of the Triassic Chinle Formation, northeastern New Mexico, U.S.A.
- 1 February 1989
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 61 (3-4) , 155-175
- https://doi.org/10.1016/0037-0738(89)90056-0
Abstract
No abstract availableKeywords
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