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The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 38 (1968)No. 4. (December), Pages 1280-1289

Petrology and Depositional Environments of the Beck Spring Dolomite (Precambrian), Kingston Range, California

Allan M. Gutstadt

ABSTRACT

The Beck Spring Dolomite (upper Precambrian), Kingston Range, California, is divided into three informal members: lower laminated--150 to 200 m thick, composed of alternating laminae of pelletal and mosaic dolomite; middle oolitic--100 to 150 m thick, composed of mosaic dolomite with oolite, pisolite, and grapestone; and upper cherty--100 to 150 m thick, similar to the middle oolitic member except that it includes stromatolites and has been partially silicified and dedolomitized. Textural evidence suggests that the lower laminated member was deposited in a supratidal environment, and the middle and upper members in shallow, agitated waters of a subtidal environment. The characteristics of the Beck Spring Dolomite are similar to those of sediments now being deposited in parts of the Ba ama Banks.


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