Deposition and Diagenesis in ...Permian Upper Wolfcamp Formation and Lower Wichita Group... Digital Download

RI0195D. Deposition and Diagenesis in a Marine-to-Evaporite Sequence: Permian Upper Wolfcamp Formation and Lower Wichita Group, Palo Duro Basin, Texas Panhandle, by R. S. Fisher and H. H. Posey. 34 p., 22 figs., 3 tables, 1990. doi.org/10.23867/RI0195D. Downloadable PDF.

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ABSTRACT
Lower Permian Wolfcamp and Wichita carbonates and anhydrites in the Palo Duro Basin, Texas Panhandle, record a change from normal-marine to marine evaporite depositional environment. These strata also contain a widespread porous and permeable interval that currently comprises a deep-basin brine aquifer system. In this study, we combine lithologic, mineralogic, and petrographic evidence of depositional conditions with the isotopic compositions of carbon, oxygen, sulfur, and strontium to determine the geochemical conditions during deposition and diagenesis. This information is then combined with chemical and isotopic analyses of formation water and the geologic history of the region to interpret the history of pore fluids in a deep-basin ground-water system and to establish time constraints on changes in pore-water composition.

Carbonate mudstone containing a normal-marine fauna was initially deposited from Early Permian seawater on an open, shallow shelf. The isotopic composition of carbon and oxygen indicates precipitation in equilibrium with Permian seawater for Wolfcamp carbonates distal from shelf margins. Samples from nearshore locations show depleted carbon and oxygen isotopic compositions that reflect the influxof terrestrial organic carbon and meteoric water. Depositional conditions gradually became more restricted, and seawater was concentrated by evaporation, resulting in deposition of penecontemporaneous, hypersaline dolomite and anhydrite in the overlying Wichita Group. Similarity in the sulfur and strontium isotopic compositions of Wolfcamp and Wichita anhydrite suggests that dolomitization of carbonate mudstone and displacive growth of anhydrite nodules in Wolfcamp strata occurred during reflux of Wichita evaporite brine.

Application of the sulfur and strontium isotope age curves yields discordant ages for strata at the Wolfcamp-Wichita boundary. Carbonate mudstone (the primary Wolfcamp lithology) and bedded nodular anhydrite (the primary Wichita lithology) have strontium isotopic compositions that indicate a Leonardian age, whereas sulfur isotopic compositions suggest an older (Wolfcampian) time of precipitation. This discrepancy records either a previously unrecognized excursion in the sulfur isotope age curve or inadequate cross-calibration of the two isotope curves. Strontium and sulfur isotopic compositions and petrographic relations indicate that bedded nodular mosaic (Wichita) and unaltered replacive nodular (Wolfcamp) anhydrite precipitated from Early Permian seawater. Silicified nodular, coarsely crystalline nodular, fossil-replacing, and vein-filling anhydrites have sulfur isotopic compositions that record minor sulfate reduction prior to anhydrite precipitation, whereas replacive anhydrite cement contains isotopically depleted sulfur indicative of sulfide oxidation prior to anhydrite precipitation. The strontium isotopic composition of most anhydrite forms indicates an Early Permian marine origin. However, strontium in anhydrite veins is slightly radiogenic compared with all other anhydrite forms, indicate that radiogenic strontium released locally from detrital siliciclastic minerals or imported by river water was present during vein filling.

The successive presence of four compositionally distinct pore fluids in Lower Permian strata of the Palo Duro Basin is interpreted from lithologic, rnineralogic, and petrographic evidence of depositional conditions, isotopic compositions of carbon, oxygen, and strontium in limestone and dolomite, limited data from fluid inclusions in sphalerite, and chemical and isotopic analyses of formation water. Permian seawater that initially filled pore spaces in Wolfcamp sediments was replaced by marine evaporite brine during deposition of overlying Wichita dolomite and anhydrite. Expulsion of warm, saline formation water from deeper in the basin through upper Wolfcamp strata is recorded in fluid inclusions in sphalerite. This change in pore-fluid composition occurred before or during the regional Tertiary uplift and tilting that led to the present hydrologic system. Meteoric recharge of at least the western third of the upper Wolfcamp aquifer occurred during the past 10 to 15 Ma, contemporaneous with deposition of the Neogene Ogallala Formation.

Keywords: anhydrite diagenesis, carbonate diagenesis, isotope chronostratigraphy, Palo Duro Basin, stable isotope geochemistry, strontium isotope geochemistry, Texas Panhandle

CONTENTS

Abstract

Introduction

Geologic Setting

Palo Duro Basin Stratigraphy and Depositional Setting

Wolfcamp-Wichita Stratigraphic Interval

Upper Wolfcamp Aquifer

Samples

Methods

Carbonates

Anhydrites

Fluid Inclusions

Results

Carbon and Oxygen Isotopic Compositions of Carbonates

Strontium Isotopic Composition of Calcites, Dolomites, and Anhydrites

Sulfur Isotopic Composition of Anhydrites

Fluid Inclusions

Discussion

Carbon and Oxygen Isotopic Evidence of Depositional Conditions

Strontium and Sulfur Isotopic Chronostratigraphy

Strontium Isotope Age Curve

Sulfur Isotope Age Curve

Age of the Wolfcamp-Wichita Boundary

Anhydrite Paragenesis

Hydrogeochemical History of the Upper Wolfcamp Aquifer

Summary and Conclusions

Acknowledgments

References

Figures

1. Map showing core locations, major structural features, and Wolfcamp shelf-margin positions, Texas Panhandle
2. Generalized stratigraphic column of Palo Duro Basin showing formation names and idealized porosity and total organic carbon profiles
3. Stratigraphic correlation showing distribution of major carbonate units and anhydrite types in sampled wells
4. Photomicrograph of felted anhydrite crystals within a bedded nodule and the sharp boundary between nodule and encasing dolomite
5. Photograph of replacive nodular anhydrite showing the sharp boundary between nodule and host carbonate, clay seams, and similar fabrics within the nodule and the encasing carbonate host
6. Photograph of partly silicified anhydrite nodules in carbonate matrix
7. Photomicrographs of interior of a silicified anhydrite nodule showing chalcedony botryoids rimmed with quartz and radiating masses of quartz crystals
8. Photomicrographs of interior of a silicified anhydrite nodule showing the boundary between anhydrite-free chalcedonic rim and anhydrite-containing quartz interior
9. Photomicrograph of anhedral, granular replacive anhydrite cement and small anhydrite vein in carbonate matrix
10. Photomicrograph of euhedral anhydrite replacing ooids
11. Photomicrograph of anhydrite pseudomorph after fossil
12. Photograph showing chert nodule and anhydrite vein cutting replacive anhydrite nodule
13. Plot of carbon isotopic composition of calcite and dolomite mudstones versus depth
14. Plot of oxygen isotopic composition of calcite and dolomite mudstones versus depth
15. Plot of strontium isotopic composition of carbonate and anhydrite samples versus depth
16. Histogram showing ⁸⁷Sr/⁸⁶Sr values of carbonate and anhydrite samples
17. Plot of sulfur isotopic composition of anhydrite samples versus depth
18. Histogram showing sulfur isotopic values of Wolfcamp and Wichita anhydrite samples
19. Plot of variations in ⁸⁷Sr/⁸⁶Sr values of marine strontium over time combined with the Van Eyshga time scale and mean ⁸⁷Sr/⁸⁶Sr values of Wolfcamp-Wichita samples
20. Plot of variations in sulfur isotopic composition of marine sulfate over time combined with the Van Eysinga time scale and histogram of sulfur isotopic compositions of unaltered Wolfcamp-Wichita anhydrite
21. Schematic diagram showing mean sulfur isotopic composition of bedded nodular mosaic, replacive nodular, and silicified nodular anhydrite and their relative stratigraphic positions
22. Interpreted paragenetic sequence of anhydrite in Wolfcamp and Wichita units of the Palo Duro Basin

Tables

1. Generalized stratigraphic column, Palo Duro Basin

2. Carbon, oxygen, and strontium isotopic compositions of limestone and dolomite mudstones

3. Sulfur and strontium isotopic compositions of anhydrite samples



Citation
Fisher, R. S., and Posey, H. H., 1990, Deposition and Diagenesis in a Marine-to-Evaporite Sequence: Permian Upper Wolfcamp Formation and Lower Wichita Group, Palo Duro Basin, Texas Panhandle: The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations No. 195, 34 p