Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A.

doi:10.2113/gsrocky.49.1.1

Title: Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A.

Full Record
Other Related Research

Abstract

The Thermopolis hydrothermal system is located in the southern portion of the Bighorn Basin, in and around the town of Thermopolis, Wyoming. It is the largest hydrothermal system in Wyoming outside of Yellowstone National Park. The system includes hot springs, travertine deposits, and thermal wells; published models for the hydrothermal system propose the Owl Creek Mountains as the recharge zone, simple conductive heating at depth, and resurfacing of thermal waters up the Thermopolis Anticline.

Authors:

Kaszuba, John P. ^[1]; Sims, Kenneth W.W. ^[2]; Pluda, Allison R. ^[3]

Univ. of Wyoming, Laramie, WY (United States). Dept. of Geology and Geophysics
Univ. of Wyoming, Laramie, WY (United States). School of Energy Resources
Univ. of Wyoming, Laramie, WY (United States). Wyoming High-Precision Isotope Lab.

Publication Date:: 2014-06-01

Research Org.:: Univ. of Wyoming, Laramie, WY (United States)

Sponsoring Org.:: USDOE Office of Fossil Energy (FE), Clean Coal and Carbon (FE-20)

OSTI Identifier:: 1171957

Grant/Contract Number:: FE0002112

Resource Type:: Journal Article: Accepted Manuscript

Journal Name:: Rocky Mountain Geology

Additional Journal Information:: Journal Volume: 49; Journal Issue: 1; Journal ID: ISSN 1555-7332

Publisher:: University of Washington, Dept. of Geology and Geophysics

Country of Publication:: United States

Language:: English

Subject:: 58 GEOSCIENCES; Bighorn Basin, hot springs, hydrogeochemistry, hydrothermal system, Thermopolis, Wyoming

Citation Formats


                    Kaszuba, John P., Sims, Kenneth W.W., and Pluda, Allison R. Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A..  United States: N. p., 2014. 
        Web.  doi:10.2113/gsrocky.49.1.1.

Copy to clipboard


                    Kaszuba, John P., Sims, Kenneth W.W., & Pluda, Allison R. Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A..  United States.  doi:10.2113/gsrocky.49.1.1.

Copy to clipboard


                    Kaszuba, John P., Sims, Kenneth W.W., and Pluda, Allison R. Sun .  
        "Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A.".  United States.  doi:10.2113/gsrocky.49.1.1.  https://www.osti.gov/servlets/purl/1171957.

Copy to clipboard


                    
@article{osti_1171957,

  title        = {Aqueous geochemistry of the Thermopolis hydrothermal system, southern Bighorn Basin, Wyoming, U.S.A.},

  author       = {Kaszuba, John P. and Sims, Kenneth W.W. and Pluda, Allison R.},

  abstractNote = {The Thermopolis hydrothermal system is located in the southern portion of the Bighorn Basin, in and around the town of Thermopolis, Wyoming. It is the largest hydrothermal system in Wyoming outside of Yellowstone National Park. The system includes hot springs, travertine deposits, and thermal wells; published models for the hydrothermal system propose the Owl Creek Mountains as the recharge zone, simple conductive heating at depth, and resurfacing of thermal waters up the Thermopolis Anticline.},

  doi          = {10.2113/gsrocky.49.1.1},

  journal      = {Rocky Mountain Geology},

  issn         = {1555-7332},

  number       = 1,

  volume       = 49,

  place        = {United States},

  year         = {2014},

  month        = {6}

}

Copy to clipboard

Journal Article:

Free Publicly Available Full Text

Accepted Manuscript (DOE)

Publisher's Version of Record

DOI: 10.2113/gsrocky.49.1.1

Other availability

Search WorldCat to find libraries that may hold this journal

Save / Share:

Export Metadata

Save to My Library

Similar records in OSTI.GOV collections:

A gravity study of the thermopolis anticline, southern Bighorn Basin, Wyoming

Conference Grannell, R B ; Showalter, P K

Approximately three hundred gravity stations were measured in the area of the Thermopolis anticline along the southern margin of the Bighorn Basin, Wyoming. Three broad anomaly patterns dominate the isostatic residual gravity map: a 10 mgal negative anomaly associated with sedimentary fill in the Bighorn Basin, a 20 mgal positive anomaly associated with the uplift of Precambrian basement in the Owl Creek Mountains, and a 2-3 mgal positive anomaly associated with the Thermopolis anticline. The anticline anomaly dominates a complex anomaly pattern located between the Owl Creek uplift and Bighorn Basin. Three poorly controlled patterns characterize the Owl Creek Mountainsmore »« less
Testing some models of foreland deformation at the Thermopolis anticline, southern Bighorn Basin, Wyoming

Journal Article Paylor, E D ; Lang, H R ; Conel, J E ; ... - Mountain Geologist; (USA)

The Thermopolis anticline is a typical structure in the Rocky Mountain foreland, southern Bighorn Basin, Wyoming. Photogeologic interpretation of Landsat Thematic Mapper data, in combination with the evaluation of topographic, bore hole, seismic reflection, and field data were used to analyze structure and constrain tectonic models. The anticline is near-concentric, asymmetric with a southwest sense of vergence, and plunges to the northwest. The steeply dipping to overturned southwest limb of the fold is cut at the surface by several thrust faults dipping northeast. Approximately 25% of the stratigraphic section on the southwest limb is missing due to faulting. Two eastmore »« less
Cross folding in southern Bighorn basin

Conference Gubbels, T L - Am. Assoc. Pet. Geol., Bull.; (United States)

Analysis of Landsat Thematic Mapper imagery coupled with surface structural investigations of well-exposed folds in the southern Bighorn basin have revealed two northwest-trending folds that have been refolded. The eastern boundary of the Owl Creek Mountains is characterized by a well-defined alignment of folds that extend north-northwest from the Owl Creek thrust front. Bridger monocline, Wildhorse Butte anticline, and Red Hole anticline lie along this trend. Initial Laramide folding, probably during latest Cretaceous time, resulted in a single, continuous, north-northwest-trending anticline with a southwestward vergence. This anticline was progressively unfolded from south to north as the Owl Creek Range wasmore »« less
Uranium hydrogeochemical and stream sediment reconnaissance of the thermopolis NTMS Quadrangle, Wyoming, including concentrations of forty-two additional elements

Technical Report Maassen, L W

The Los Alamos Scientific Laboratory conducted a hydrogeochemical and stream sediment reconnaissance for uranium in the Thermopolis National Topographic Map Series quadrangle, Wyoming. Totals of 920 water and 1821 sediment samples were collected from 1977 locations at an average density of one sample location per 9 km/sup 2/ over an 18,000-km/sup 2/ area. Water samples were collected from streams, springs, and wells; sediment samples were collected from streams and springs. The uranium contents of water samples range from below the detection limit of 0.02 ppB to 307.98 ppB with a median of 0.56 ppB. Six clusters of anomalous water samplesmore »« less
Maturation history and thermal evolution of Cretaceous source rocks of Bighorn basin, Wyoming and Montana

Conference Hagen, E S ; Surdam, R C - Am. Assoc. Pet. Geol., Bull.; (United States)

The Laramide basins of the Rocky Mountain region are deep asymmetric structural depressions containing thick sequences of Upper Cretaceous and Tertiary sandstone strata. The combined effects of tectonics and sedimentation have contributed to the thermal evolution of the basins and to the maturation history of the source rocks. In the Bighorn basin of Wyoming and Montana, total organic carbon (TOC) values for samples from a 2000-ft (610-m) thick interval, including the Thermopolis, Mowry, Frontier, and Cody Formations, average 1 wt. %. The hydrogen indices and elemental analyses suggest that most of the samples presently contain kerogen between types II andmore »« less

Similar Records