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Book Chapter

Lithologies and Diagenesis of the Lacustrine Sediments of the Lockatong Formation (Upper Triassic) in the Newark Rift Basin

By
Mohamed El Tabakh
Mohamed El Tabakh
1
Earth and Environmental Sciences Program, Graduate School C.U.N.Y., New York, NY 10036;
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;
B. Charlotte Schreiber
B. Charlotte Schreiber
1
Earth and Environmental Sciences Program, Graduate School C.U.N.Y., New York, NY 10036;
2
Department of Geology, Queens College (CUNY), Flushing, NY 11367
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Published:
January 01, 1994

Abstract

The Lockatong Formation lacustrine sequences are the most extensive Upper Triassic deep-lake deposits exposed in eastern North America. Sedimentation took place within tropical lakes in a developing rift basin. These lacustrine deposits and their sedimentary structures exhibit a generally upward-shallowing sedimentary pattern and follow an internal repetitive pattern of cyclicity. The sequences suggest that lake depth responded to continuing changes in climatic conditions, although the basinal bounding faults were also active during sedimentation and may have had some general control. The identified lithologies formed in these lakes are black and gray shales, carbonate-rich mudstones, siltstones, and evaporite-bearing mudstones. The authigenic minerals present are analcime, dolomite, and calcite.

Petrographic and electron microprobe investigations suggest that (1) analcime formed both as a direct chemical precipitate from lake and groundwaters and as an early diagenetic mineral, due to the early alteration of original clay minerals by the increasingly concentrated alkaline waters; (2) the lacustrine calcites are primary and/or early diagenetic; and (3) dolomite also was formed penecontemporaneously during evaporative concentration of shallow groundwaters. These observations are supported by carbon and oxygen isotopic ratios of the carbonates taken from major sections of the Lockatong Formation, and show that variations in the stable isotope ratios closely match the lithological alternations of the Lockatong Formation. The sedimentary succession shows an overall upward trend of increased evaporation, upsection increase in evaporite development, and, with this, a concomitant enrichment in δ18O. The δ13C isotope ratio, on the other hand, remains quite constant throughout the section, having a value appropriate to lacustrine deposition.

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Contents

SEPM Core Workshop Notes

Lacustrine Reservoirs and Depositional Systems

Anthony J. Lomando
Anthony J. Lomando
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;
B. Charlotte Schreiber
B. Charlotte Schreiber
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;
Paul M. Harris
Paul M. Harris
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SEPM Society for Sedimentary Geology
Volume
19
ISBN electronic:
9781565762718
Publication date:
January 01, 1994

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