Paleocurrent Analysis of the Upper Miocene Formation, Los Angeles Basin, California
Almost all sandstone beds occurring in the Upper Miocene formations at the Los Angeles basin were deposited by turbidity currents. Primary textures and structures indicative of turbidites occur in fair abundance throughout all three Upper Miocene formations. All accessible outcrops of the Puente, Mo...
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| Language: | en_US |
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The University of Arizona.
2012
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| Online Access: | http://hdl.handle.net/10150/244083 |