1988
DOI: 10.1029/gl015i012p01437
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Evidence for multiple boundary faults beneath the northwest moat of Long Valley Caldera: Magnetotelluric results

Abstract: The boundaries of Long Valley Caldera, in Eastern California, are sharply delineated by steeply dipping normal faults which, for the most part, are buried and obscured by recent volcanic and sedimentary cover. The only evidence for their presence is from their geophysical signatures on regional gravity, seismic and electromagnetic surveys. Recently, a surge of interest has focused studies in the western moat, where the volcanism is most recent, and where many workers feel that the geothermal potential is highe… Show more

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Cited by 6 publications
(5 citation statements)
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References 23 publications
(19 reference statements)
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“…The Bishop Tuff, most of which is moderately to densely welded, appears resistive overall (cf. Hermance and Neumann, 1988).…”
Section: Structural Implications and Geothermal Significancementioning
confidence: 95%
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“…The Bishop Tuff, most of which is moderately to densely welded, appears resistive overall (cf. Hermance and Neumann, 1988).…”
Section: Structural Implications and Geothermal Significancementioning
confidence: 95%
“…If some off-profile coupling between the axial graben conductors and other caldera structures in the upper 2-3 km can be discovered to reproduce 5-10 degrees of anomaly in <Pxy at 100 s, then there seems no need to invoke a mid-crustal conductor to explain the long period TE data. However, simple channeling of currents from conductive fill in the northern or southern parts of the caldera (Hermance et al, 1988;Park and Torres-Verdin, 1988) should not be responsible and in fact should actually amplify Pxy (e.g., Jones, 1983).…”
Section: Structural Implications and Geothermal Significancementioning
confidence: 98%
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“…Long Valley caldera has seen extensive MT and active source EM work to explore for hydrothermal and magmatic energy resources. Hermance et al , [1988] and Hermance and Neumann [1988] have continued to interpret long period telluric results in terms of caldera fill conductance and possible boundary faults. Park and Torres‐Verdin [1988] carried out a fully 3D interpretation of industry‐donated MT data over the caldera, concluding that the data forbid highly anomalous deep crustal structure below the upper 2 km of variably conductive post‐caldera volcanics, but that more subtle structures were not resolvable given the limited data quality.…”
Section: Earth Structure Processes and Resourcesmentioning
confidence: 99%