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Depositional and diagenetic controls on source-rock characteristics of the Lower Jurassic ``Nordegg Member``, western Canada

Journal Article · · Journal of Sedimentary Research, Section A: Sedimentary Petrology and Processes
 [1];  [2]
  1. Univ. of Waterloo, Ontario (Canada). Dept. of Earth Sciences
  2. Inst. of Sedimentary and Petroleum Geology, Calgary, Alberta (Canada)

Petrographic, mineralogical, and bulk-geochemical (XRD, XRF, and Rock-Eval) data indicate that depositional and early diagenetic processes were the principal controls on the organic and inorganic characteristics of the Lower Jurassic Nordegg Member source rock. This unit comprises organic-rich, calcareous mudstones to marlstones and marly limestones that were deposited in a predominantly anoxic, hypersaline, silled marine basin during two transgressive-regressive (T-R) events. Sediments deposited during marine transgression have a higher content of carbonate (calcite and dolomite) and organic matter. Fe (mainly as pyrite) content varies inversely with carbonate content. The basal ``Nordegg Member`` is phosphatic with stratiform apatite laminae and phosphatic nodules. Early diagenetic phosphatogenesis was probably mediated by bacteria under variably dysoxic conditions during the initial transgressive event. Regressive parts of T-R cycles are expressed as an increase in abundance of silicate (quartz, illite, kaolinite, and minor K-feldspar) and lower organic carbon contents. Deposition of abundant marine organic matter fueled vigorous bacterial reduction of sulfate and almost total bacterial reworking of the sedimented organic matter, resulting in significant production of reduced sulfur species and predominantly amorphous kerogen. Pyrite formation was ubiquitous but limited by the abundance of Fe. Furthermore, content of organic S increases with increasing Hydrogen Index, indicating the importance of type and reactivity of organic matter on the extent of incorporation of sulfur into the kerogen during early diagenesis.

Sponsoring Organization:
USDOE
OSTI ID:
37116
Journal Information:
Journal of Sedimentary Research, Section A: Sedimentary Petrology and Processes, Journal Name: Journal of Sedimentary Research, Section A: Sedimentary Petrology and Processes Journal Issue: 1 Vol. 65; ISSN JSRAEA; ISSN 1073-130X
Country of Publication:
United States
Language:
English

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