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Black shales of Jurassic Newark basin

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5268563

Rock cores have exposed the complete Jurassic section of the Newark basin, including three sedimentary formations of fluvial origin. Within the Feltville, Towaco, and Boonton formations, 16 lacustrine/fan units range in thickness from 1 to 15 m. Each unit contains one black shale facies, although lower units of the Towaco contain multiple fining-upward sequences ending with truncated deep-water shale. Additional thinner gray sandstone facies in each formation occur at the margin of lacustrine units located farther southwest, in the paleodrainage direction of the Newark basin. Most microlaminated black shale shows evidence of turbidity flows. Freshly broken pieces of black shale and adjacent sandstones also have a strong organic odor.

Research Organization:
Army Engineers, New York, NY
OSTI ID:
5268563
Report Number(s):
CONF-860624-
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Vol. 70:5; ISSN AAPGB
Country of Publication:
United States
Language:
English