Nature and origin of seismic reflection fabric, Ruby-East Humboldt Metamorphic Core Complex, Nevada (Q79489210)

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A. W. Snoke

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C. A. Hurich

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S. B. Smithson

Cordilleran metamorphic core complexes: Cenozoic extensional relics of Mesozoic compression

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publication date

April 1989

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published in

Tectonics

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volume

8

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issue

2

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page(s)

391-415

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cites work

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Overview of the COCORP 40°N Transect, western United States: The fabric of an orogenic belt

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Mid-crustal Cretaceous roots of Cordilleran metamorphic core complexes

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The velocity of compressional waves in rocks to 10 kilobars: 1

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Origin of reflections from the Brevard Fault Zone

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Lithoprobe seismic reflection structure of the Southeastern Canadian Cordillera: Initial results

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The Mesozoic-Cenozoic tectonothermal evolution of the Ruby Mountains, East Humboldt Range, Nevada: A Cordilleran Metamorphic Core Complex

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Structural characteristics of metamorphic core complexes, southern Arizona

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Thermochronologic evidence of major tectonic denudation associated with detachment faulting, Northern Ruby Mountains - East Humboldt Range, Nevada

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Tertiary structural development of selected valleys based on seismic data: Basin and Range province, northeastern Nevada

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Seismic reflectivity of mylonite zones in the crust

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An open-system, two-layer crustal stretching model for the Eastern Great Basin

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Crustal structure of eastern Nevada from COCORP deep seismic reflection data

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Metamorphic infrastructure in the northern Ruby Mountains, Nevada

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Seismic evidence of mylonite reflectivity and deep structure in the Kettle dome metamorphic core complex, Washington

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The nature of seismic reflections from deep crustal fault zones

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The Moho in the northern Basin and Range province, Nevada, along the COCORP 40°N seismic-reflection transect

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