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- W2558829780 endingPage "4117" @default.
- W2558829780 startingPage "4103" @default.
- W2558829780 abstract "Abstract The fate of subducted oceanic slabs can provide important clues to plate reconstruction through Earth history. Since oceanic slabs in continental collision zones are typically not well preserved, ancient subduction zones have rarely been imaged by geophysical techniques. Here we present an exception from the Darbut belt in the Junggar accretionary collage in the southern Altaids of Asia. We deployed a 182 km long magnetotelluric (MT) profile including 60 broadband sounding sites across the belt. Quality off‐diagonal impedances were inverted by a three‐dimensional scheme to image resistivities beneath the profile. The resistivity model along with MT impedance phase ellipses and induction vectors were tested and interpreted in detail. Combining geological and geophysical observations, mineral physical experiment, and geodynamic modeling results, the MT transect suggests a fossil intraoceanic subduction zone during the Late Paleozoic in the western Junggar that has been well preserved due to lack of significant subsequent tecto‐thermal events." @default.
- W2558829780 created "2016-12-08" @default.
- W2558829780 creator A5011208510 @default.
- W2558829780 creator A5042019995 @default.
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- W2558829780 creator A5079301511 @default.
- W2558829780 creator A5085981009 @default.
- W2558829780 creator A5086237150 @default.
- W2558829780 date "2016-06-01" @default.
- W2558829780 modified "2023-10-09" @default.
- W2558829780 title "Magnetotelluric imaging of a fossil paleozoic intraoceanic subduction zone in western Junggar, NW China" @default.
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