Genesis of clay mineral assemblages and micropaleoclimatic implications in the Tertiary Powder River Basin, Wyoming

Conference · Tue May 01 04:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA)

OSTI ID:7092518

Flores, R M; Weaver, J N ^[1]; Bossiroy, D; Thorez, J ^[2]

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1. Geological Survey, Denver, CO (USA)
2. Liege State Univ. (Belgium)

An x-ray diffraction (XRD) study was undertaken on the clay mineralogy of the early Tertiary coal-bearing sequences of the Powder River basin. The vertical and lateral distribution of alternating fluvial conglomerates, sandstones, mudstones, shales, coals, and paleosols reveals a transition from alluvial fans along the basin margin to an alluvial plain and peat bogs basinward. Samples included unweathered shales and mudstones from a borehole and a variety of corresponding surface outcrop samples of Cambrian to Eocene age. Samples older than Tertiary were collected along the basin margin specifically to determine the potential source of parent material during Tertiary sedimentation. XRD analyses were performed on the <2-{mu}m fraction prepared as oriented aggregates. To investigate the materials in their natural state, no chemical pre-treatments the authors applied before the analysis. A series of specific post-treatments, consisting of catonic saturation (Li+, K+), a solution with polyalcohols, heating, acid attack and hydrazine saturation was selectively applied. These post-treatments permit a good discrimination between the mimetic clay minerals such as smectite and illite-smectite mixed layers that constitute the bulk of the clay fraction in the Tertiary rocks. When analyzed only using routine XRD, these swelling minerals are apparently uniformly distributed in the fluvial sedimentary rocks and are better interpreted as a single smectitic population. However, the post-treatments clearly differentiate both qualitatively and quantitatively this smectitic stock. Other clays include illite and kaolinite, which have different degrees of crystallinity, and minor interstratified clays (i.e., illite-chlorite, chlorite-smectite). The clay minerals in pre-Tertiary (and pedogenic) materials are different from those in the Tertiary rocks.

• OSTI ID: 7092518
• Report Number(s): CONF-900605--
• Conference Information: Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Journal Volume: 74:5
• Country of Publication: United States
• Language: English

Related Subjects

01 COAL, LIGNITE, AND PEAT
011000* -- Coal
Lignite
&amp; Peat-- Reserves
Geology
&amp; Exploration
58 GEOSCIENCES
580000 -- Geosciences
ALLUVIAL DEPOSITS
ALUMINIUM COMPOUNDS
ALUMINIUM SILICATES
CENOZOIC ERA
CHLORITE MINERALS
CLAYS
COAL DEPOSITS
COHERENT SCATTERING
CONGLOMERATES
DIFFRACTION
FEDERAL REGION VIII
GEOLOGIC AGES
GEOLOGIC DEPOSITS
ILLITE
KAOLINITE
MINERAL RESOURCES
MINERALOGY
MINERALS
MONTANA
NORTH AMERICA
OXYGEN COMPOUNDS
PALEOCLIMATOLOGY
PALEONTOLOGY
POWDER RIVER BASIN
RESOURCES
ROCKS
SCATTERING
SEDIMENTARY ROCKS
SHALES
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
SMECTITE
TERTIARY PERIOD
USA
WYOMING
X-RAY DIFFRACTION