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Carbonate bank sedimentation in a volcaniclastic arc setting: Lower Carboniferous limestones of the eastern Klamath terrane, California

Journal Article · · Journal of Sedimentary Petrology; (United States)
OSTI ID:5836339
 [1]
  1. Milwaukee Public Museum, WI (United States). Dept. of Geology

Carboniferous volcaniclastic-arc deposits of the eastern Klamath terrane, California, include Late Visean/Namurian limestone lenses that formed as small carbonate banks. The limestone lenses, within the Bragdon and Baird formations, reach 17 m in thickness and 1.2 km in length. Slope deposits consist of argillaceous spiculitic wackestone, and bank-edge deposits include ooid grainstone, Striatifera packstone, argillaceous phylloid algal packstone, and argillaceous skeletal packstone, Bank-interior deposits include skeletal wackestone/packstone and argillaceous sandy mudstone. The limestone lenses overlie proximal deltaic deposits of thick-bedded volcaniclastic sandstone and conglomerate. Carbonate banks developed on delta lobes during intervals of minimal clastic sedimentation, possibly related to sea-level rise and volcanic quiescence. The carbonate banks were short-lived depositional systems, and they were covered by prograding deposits of younger volcaniclastic sands.

OSTI ID:
5836339
Journal Information:
Journal of Sedimentary Petrology; (United States), Journal Name: Journal of Sedimentary Petrology; (United States) Vol. 63:5; ISSN 0022-4472; ISSN JSEPAK
Country of Publication:
United States
Language:
English