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Organic matter in Delaware Mountain Group sediments - Geochemistry, source, and role in diagenetic alteration of reservoir sandstones

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:6969530
;  [1]
  1. Texas A and M Univ., College Station (United States)
Rock-Eval pyrolysis data show that Delaware Mountain Group siltstone organic matter is oxygen-rich type II and type III kerogen, prone to generation of significant quantities of carboxylic acids and CO{sub 2} during thermal maturation. Rock-Eval T{sub max} data and various biomarker maturity indicators show that the organic matter is at a moderate stage of maturity, well within the oil generative phase. Petrologic study shows that the reservoir sandstones have experienced four major episodes of diagenetic alteration: (1) early cementation by carbonate, sulfate, and halite cements that partly arrested compaction and preserved significant intergranual volume during progressive burial; (2) extensive dissolution of cements and some detrital material to form voluminous secondary porosity; (3) extensive chlorite authigenesis, which dissected nearly half of the porosity into microporosity; (4) authigenesis of dolomite, feldspar, and Ti oxides during late diagenesis. Characterization of the organic geochemistry of Delaware Mountain Group siltstones and analysis of late authigenic products in the sandstones indicates that organic diagenesis controlled pore fluid chemical evolution within the sandstones and resulted in creation of secondary porosity there. Authigenic minerals in the sandstones exhibit isotopic and trace element content indicative of this organic influence.
OSTI ID:
6969530
Report Number(s):
CONF-9204139--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 76:4
Country of Publication:
United States
Language:
English