Geophysical Investigation of the Yellowstone Hydrothermal System

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dc.contributor.authorDickey, Kira Annen
dc.contributor.committeechairHolbrook, W. Stevenen
dc.contributor.committeememberKing, Scott D.en
dc.contributor.committeememberFinn, Carol A.en
dc.contributor.departmentGeosciencesen
dc.date.accessioned2018-08-28T08:00:34Zen
dc.date.available2018-08-28T08:00:34Zen
dc.date.issued2018-08-27en
dc.description.abstractYellowstone National Park hosts over 10,000 thermal features (e.g. geysers, fumaroles, mud pots, and hot springs), yet little is known about the hydrothermally active zones hundreds of meters beneath the features. Transient electromagnetic (TEM) soundings and 2D direct current (DC) resistivity profiles show that hydrothermal alteration at active sites have a higher electrical conductivity than the surrounding hydrothermally inactive areas. For that reason, airborne TEM is an effective method to characterize large areas and identify hydrothermally active and inactive zones using electrical conductivity. Here we present results from an airborne TEM survey acquired jointly by the U.S. Geological Survey and the University of Wyoming in November, 2016. We integrate resistivity from the airborne electromagnetic (EM) survey with research drillhole data and rock physics models to investigate the controls on electrical conductivity in the upper few hundreds of meters of the Yellowstone hydrothermal system. Resistivities in Yellowstone are the product of complex variations of lithology, temperature, salinity, clay content, and hydrothermal fluids. Results show that the main drivers in lowering the high resistivitiy of volcanic rocks are water saturation and hydrothermal alteration. Salinities are not significantly elevated in Yellowstone and temperature is not a first order affect.en
dc.description.abstractgeneralYellowstone National Park is a popular scientific and tourist destination because of it’s vast amount of thermal features including hot springs like Grand Prismatic, geysers like Old Faithful, and many more. But what is happening beneath those features and how can we use geophysics to find out? In November 2016, the U.S. Geological Survey and University of Wyoming conducted an airborne geophysical survey that measures how conductive the rock is beneath Yellowstone. Using this data, we map fluids and hydrothermal activity, and relate them to the local geology. The goal of this thesis is to understand the geologic factors that make the rock beneath Yellowstone’s features conductive. We have shown that the main factors that contribute to the high conductivities in thermal areas of Yellowstone are hydrothermal alteration of the rocks and the high amount of fluids filling space inside the rocks.en
dc.description.degreeMaster of Scienceen
dc.format.mediumETDen
dc.identifier.othervt_gsexam:16801en
dc.identifier.urihttp://hdl.handle.net/10919/84922en
dc.publisherVirginia Techen
dc.rightsIn Copyrighten
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en
dc.subjectYellowstoneen
dc.subjectairborne electromagneticsen
dc.subjectresistivityen
dc.subjectrock physicsen
dc.subjectgeophysicsen
dc.titleGeophysical Investigation of the Yellowstone Hydrothermal Systemen
dc.typeThesisen
thesis.degree.disciplineGeosciencesen
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen
thesis.degree.levelmastersen
thesis.degree.nameMaster of Scienceen

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