Book Nahcolite and Halite Deposition through Time During the Saline Mineral Phase of Eocene Lake Uinta, P U. S. Department of the Interior

portada Nahcolite and Halite Deposition through Time During the Saline Mineral Phase of Eocene Lake Uinta, Piceance Basin, Western Colorado

Type

Physical Book

Publisher

Createspace Independent Publishing Platform

Author

U. S. Department of the Interior

Language

Inglés

Pages

Format

Paperback

Dimensions

28.0 x 21.6 x 0.4 cm

Weight

0.20 kg.

ISBN13

9781495925542

Synopsis "Nahcolite and Halite Deposition through Time During the Saline Mineral Phase of Eocene Lake Uinta, Piceance Basin, Western Colorado"

Lake Uinta formed when two smaller fresh-water lakes, one in the Piceance Basin and one in the Uinta Basin to the west, expanded during the Long Point transgression (represented by the Long Point Bed) and coalesced to form a single large lake. Salinity in Lake Uinta progressively increased, first killing off the fresh-water mollusks that were ubiquitous during the earlier fresh-water phase and ultimately resulting in the deposition of dolomite-rich oil shale, nahcolite, and halite (Johnson, 1985).

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Nahcolite and Halite Deposition through Time During the Saline Mineral Phase of Eocene Lake Uinta, Piceance Basin, Western Colorado - U. S. Department of the Interior

Synopsis "Nahcolite and Halite Deposition through Time During the Saline Mineral Phase of Eocene Lake Uinta, Piceance Basin, Western Colorado"

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