VERTICAL GRAIN SIZE PROGRESSIONS AS AN AID IN INTERPRETING THE DEPOSITIONAL ENVIRONMENTS OF THE QUEEN CITY FORMATION (EOCENE), EAST TEXAS
Vertical grain size progressions of sand deposits in the Queen City Formation (Eocene), East Texas, were studied to determine if unique textural trends characterize depositional environments. Results from this study indicate that certain groups of environments are more easily distinguished from othe...
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| Format: | Others |
| Language: | English |
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2007
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| Online Access: | http://hdl.handle.net/1911/13264 |