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- W2069792625 abstract "A magnetotelluric survey in northern Pakistan contains effects from both 2-D and 3-D structure. Identification of the effects of the sediments along the Indus River valley using 3-D modeling permitted the selection of modes that could be accurately inverted with 2-D inversions. The resulting 2-D model reveals generally resistive (> 500 ohm-m) upper crust (0–8 km), a more conductive (30–50 ohm-m) middle to lower crust (8–40 km), and a resistive (> 300 ohm-m) upper mantle. Shallow crustal (< 10 km) conductors correlate with a hydrothermally altered fault zone and/or carbonaceous metamorphic rocks near the Raikot fault. A prominent midcrustal conductor located beneath Nanga Parbat is required to fit the data, but its depth, dimensions, and conductivity are poorly constrained by existing data." @default.
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- W2069792625 date "1997-10-01" @default.
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- W2069792625 title "Crustal structure at Nanga Parbat, northern Pakistan, from magnetotelluric soundings" @default.
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- W2069792625 doi "https://doi.org/10.1029/97gl02147" @default.
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