|Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)|
|Paper No. 41-3|
|Presentation Time: 8:00 AM-12:00 PM|
TRACE ELEMENT GEOCHEMISTRY OF SHALE : IMPLICATIONS ON THE DEPOSITIONAL ENVIRONMENTS
KHANDAKER, Nazrul I., Natural Sciences, YORK COLLEGE OF CUNY, 94-20 Guy R. Brewer Boulevard, Jamaica, New York, NY 11451, firstname.lastname@example.org.|
The shale unit selected in this study is interbedded with bentonite horizons, laterally persistent, and belongs to the Upper Cretaceous Frontier Formation, north-central Wyoming. The geochemical data involving Peay (lower Frontier) and Torchlight (upper Frontier)shale samples provided significant clues as to the precise identification of the depositional environments of these fine-grained sediments. A multi-element plot shows similar trace element concentrations for both Peay and Torchlight shale samples. Ni, Ce, and Zn are significantly abundant in both Peay and Torchlight shale. Relatively higher concentrations of La in the Peay shale compared with the Torchlight shale reflect less terrigenous quartz input into the depositional basin and perhaps signify deposition in a quiet, less turbulent, offshore marine setting. Consistent Zr, Ni, Y, and Nb concentrations in all the shale samples analyzed suggest a similar source for the Peay and Torchlight shale, and the overall trace-element behavior (with the exception of La) is controlled by the rate of sedimentation, terrigenous input, and subsequent deepening of the depositional basin.
Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
General Information for this Meeting
|Session No. 41--Booth# 17|
Sedimentation and Stratigraphy II (Posters)
Hilton McLean Tysons Corner: Ballrooms A and B
8:00 AM-12:00 PM, Friday, March 26, 2004
Geological Society of America Abstracts with Programs, Vol. 36, No. 2, p. 90
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