skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

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

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:7092518
;  [1]; ;  [2]
  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-; CODEN: AABUD
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (USA), Vol. 74:5; Conference: Annual convention and exposition of the American Association of Petroleum Geologists, San Francisco, CA (USA), 3-6 Jun 1990; ISSN 0149-1423
Country of Publication:
United States
Language:
English

Similar Records

Contact metamorphism of clay minerals in central Utah
Conference · Mon Mar 01 00:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:7092518

Clay-mineral transformation as an indicator of depositional and diagenetic conditions in Pennsylvanian black shales, Paradox Member of the Hermosa Foundation, Utah and Colorado
Conference · Sun Aug 01 00:00:00 EDT 1993 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:7092518

Depositional environments, diagenesis, and hydrocarbon potential of nonmarine Upper Cretaceous and Lower Tertiary rocks, eastern Uinta Basin, Utah
Conference · Wed May 01 00:00:00 EDT 1985 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:7092518