In situ Stable Isotopic Evidence for Protracted and Complex Carbonate Cementation in a Petroleum Reservoir, North Coles Levee, San Joaquin Basin, California, U.S.A

Fayek, Mostafa; Harrison, T. Mark; Grove, Marty; Mckeegan, Kevin D.; Coath, Chris D.; Boles, James R.

doi:10.1306/2dc40954-0e47-11d7-8643000102c1865d

Cited by 97Hydrocarbon exploration and reservoir analysisGeological and Geochemical AnalysisGeochemistry and Elemental Analysis

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In situ Stable Isotopic Evidence for Protracted and Complex Carbonate Cementation in a Petroleum Reservoir, North Coles Levee, San Joaquin Basin, California, U.S.A

Fayek, Mostafa, Harrison, T. Mark, Grove, Marty, Mckeegan, Kevin D., Coath, Chris D., Boles, James R.·2001·Journal of Sedimentary Research

DOI 10.1306/2dc40954-0e47-11d7-8643000102c1865d

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Abstract

Knowledge of the evolution of carbonate cementation in hydrocarbon reservoirs is key to understanding the history of fluid flow during petroleum accumulation. The Stevens sands is a sequence of marine shales and deep-sea fan sands that was deposited within the Miocene Monterey Formation in the south-central part of the San Joaquin basin, California, during the upper Miocene (10-6 Ma). Rapid, high-precision in situ oxygen and carbon isotopic analyses of carbonate phases using the ion microprobe operated in multi-collection mode, in conjunction with electron microprobe analyses, indicate that carbonate cement zones within the Stevens sands at North Coles Levee (NCL) have had a complex and protracted fluid history. Three main generations of carbonate cement were identified. The relative timing of carbonate cement precipitation within the Stevens sands at NCL was estimated using the thermal and burial history of the San Joaquin basin, in situ oxygen isotope data, and cementation temperatures derived from equilibrium oxygen isotope fractionation factors for calcite-water and dolomite-water. Precipitation of these cement zones began soon after sediment deposition (∼ 7 Ma) and is ongoing. Early dolomite was precipitated at a temperature of ∼ 10°C, near the sediment-water interface, and soon after sediment deposition. Calcite cements, which are the most abundant variety, precipitated semicontinuously between 4 Ma and 5 Ma, at temperatures between 50°C and 65°C, and depths of 800 m to…

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Authors: Fayek, M., Harrison, T. M., Grove, M., Mckeegan, K. D., Coath, C. D., & Boles, J. R.
Affiliations: Oak Ridge National Laboratory (US)
University of California, Los Angeles (US)
5Department of Earth and Space Sciences and Institute of Geophysical and Planetary Physics, University of California, Los Angeles, California 90095-1567, U.S.A.
University of California, Santa Barbara (US)
ORCID: Fayek, Mostafa
Harrison, T. Mark
Grove, Marty
Mckeegan, Kevin D.
Venue: Journal of Sedimentary Research
Publisher: Society for Sedimentary Geology
Published: 2001-05-01
Volume: 71
Issue: 3
Pages: 444-458
ISSN: 0022-4472 (ISSN-L)
1938-3681
1527-1404
DOI: 10.1306/2dc40954-0e47-11d7-8643000102c1865d
OpenAlex: W2098751466
Cited by: 96
References: 49
Citations by year: 2026: 2 · 2025: 10 · 2024: 7 · 2023: 5 · 2022: 11 · 2021: 9 · 2020: 8 · 2019: 9 · 2018: 6 · 2017: 5 · 2016: 6 · 2015: 3 · 2014: 4 · 2012: 1
FWCI: 3.15
Type: journal article
Language: en
Open access: closed
Locations: Journal of Sedimentary Research (publishedVersion)
Funders: National Science Foundation
Topics: Physical Sciences › Earth and Planetary Sciences › Geology › Hydrocarbon exploration and reservoir analysis
Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Keywords: carbonate cementation, calcite cement, dolomite cement, Monterey Formation, San Joaquin Basin, oxygen isotopes, carbon isotopes, hydrocarbon reservoirs, pore pressure reduction, methanogenesis, ion microprobe

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In situ Stable Isotopic Evidence for Protracted and Complex Carbonate Cementation in a Petroleum Reservoir, North Coles Levee, San Joaquin Basin, California, U.S.A

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