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Home > Society and Social Sciences > Politics and government > Analysis of Magnetotelluric Profile Data from the Ruby Mountains Metamorphic Core Complex and Southern Carlin Trend Region, Nevada: Open-File Report 2002-214
Analysis of Magnetotelluric Profile Data from the Ruby Mountains Metamorphic Core Complex and Southern Carlin Trend Region, Nevada: Open-File Report 2002-214

Analysis of Magnetotelluric Profile Data from the Ruby Mountains Metamorphic Core Complex and Southern Carlin Trend Region, Nevada: Open-File Report 2002-214


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About the Book

We have collected about 150 magnetotelluric (MT) soundings in northeastern Nevada in the region of the Ruby Mountains metamorphic core complex uplift and southern Carlin mineral trend, in an effort to illuminate controls on core complex evolution and deposition of world-class gold deposits. The region has experienced a broad range of tectonic events including several periods of compressional and extensional deformation, which have contributed to the total expression of electrical resistivity. Most of the soundings are in three east-west profiles across increasing degrees of core uplift to the north (Bald Mountain, Harrison Pass and Secret Pass latitudes). Two shorter lines cross a prominent east-west structure to the north of the northern profile. MT impedance tensor and vertical magnetic field rotations imply a N-NNE average regional geoelectric strike, similar to surface geologic trends. Model resistivity cross sections were derived using a 2-D inversion algorithm, which damps departures of model parameters from an a priori structure, emphasizing the transverse magnetic (TM) mode and vertical magnetic field data. Geological interpretation of the resistivity combines previous seismic, potential field and isotope models, structural and petrological models for regional compression and extension, and detailed structural/stratigraphic interpretations incorporating drilling for petroleum and mineral exploration. To first order, the resistivity structure is one of a moderately conductive, Phanerozoic sedimentary section fundamentally disrupted by intrusion and uplift of resistive crystalline rocks. Late Devonian and early Mississippian shales of the Pilot and Chainman Formations together form an important conductive marker sequence in the stratigraphy and show pronounced increases in conductance (conductivity-thickness product) from east to west. These increases in conductance are attributed to graphitization caused by Elko-Sevier era compressional shear deformation and


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Product Details
  • ISBN-13: 9781288750146
  • Publisher: Bibliogov
  • Publisher Imprint: Bibliogov
  • Height: 246 mm
  • Sub Title: Open-File Report 2002-214
  • Width: 189 mm
  • ISBN-10: 1288750145
  • Publisher Date: 11 Feb 2013
  • Binding: Paperback
  • Spine Width: 3 mm
  • Weight: 113 gr


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Analysis of Magnetotelluric Profile Data from the Ruby Mountains Metamorphic Core Complex and Southern Carlin Trend Region, Nevada: Open-File Report 2002-214
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Analysis of Magnetotelluric Profile Data from the Ruby Mountains Metamorphic Core Complex and Southern Carlin Trend Region, Nevada: Open-File Report 2002-214
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