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Comparative Sedimentology and Diagenesis of Upper Jurassic Ooid Grainstone Sequences, East Texas Basin

By
Gill M. Harwood
Gill M. Harwood
Department of Geology, The University, Newcastle upon Tyne, England, NE1 7RU
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Clyde H. Moore
Clyde H. Moore
Applied Carbonate Research Program, Department of Geology, Louisiana State University, Baton Rouge, Louisiana 70803
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Published:
January 01, 1984

Abstract

Ooid grainstones in Upper Jurassic carbonates in East Texas have been hydrocarbon exploration targets for some thirty years. Shoaling-upward sequences through mudstones/wackestones and packstones culminate in well-sorted ooid grainstones in many cores. A succession of several shoaling-upward sequences, each averaging 12-18 m (40-60 ft) thick, is commonly developed in upper Smackover carbonates around the basin margin where it produces large cumulative thicknesses of grainstones. In contrast, basinal carbonates contain fewer and thinner grainstone sequences.

Porosity and permeability within the grainstones are controlled by their diagenetic history. Along the northern flank of the East Texas Salt Basin it is possible to trace a lateral continuation of the northern, transitional and southern diagenetic zones recognized in Louisiana and Arkansas. Oomoldic porosity is well developed in the northern zone and patchily present in the transitional zone. Early complete dolomitization is prevalent at the top of the Upper Smackover in the northern and transitional zones; late dolomitization is minimal. Little or no dolomitization occurs in the southern zone.

On the western flank of the basin early dolomitization of upper Smackover carbonates is less common but some percentage of later, post-compaction dolomite is present in both updip and downdip carbonates. In updip areas fracturing is common, with fracture fill calcite cement precipitation. Little or no fracturing is observed in the downdip carbonates.

Diagenesis of the more basinward carbonates is comparable to that of the southern diagenetic zone of Louisiana-Arkansas, with the exception of the presence of some replacive baroque dolomite. In addition, there is no evidence of late, solution-enhanced porosity development in East Texas.

Porosities and permeabilities are highest in the dolomitized updip Smackover grainstones; oomoldic limestones have good porosity but often low permeability. In general, downdip and basinward grainstones possess lower porosities and permeabilities.

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Contents

SEPM Core Workshop Notes

Carbonate Sands-A Core Workshop

Paul M. Harris
Paul M. Harris
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SEPM Society for Sedimentary Geology
Volume
5
ISBN electronic:
9781565762602
Publication date:
January 01, 1984

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