Subduction and accretion of sedimentary rocks in the Yakutat collision zone, St. Elias orogen, Gulf of Alaska
about
Mid-Pleistocene climate transition drives net mass loss from rapidly uplifting St. Elias Mountains, Alaska.Rapid sedimentation and overpressure in shallow sediments of the Bering Trough, offshore southern AlaskaCooperation among tectonic and surface processes in the St. Elias Range, Earth's highest coastal mountainsGulf of Alaska continental slope morphology: Evidence for recent trough mouth fan formationMoho interface beneath Yakutat terrane, southern Alaska
P2860
Subduction and accretion of sedimentary rocks in the Yakutat collision zone, St. Elias orogen, Gulf of Alaska
description
im November 2013 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в листопаді 2013
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name
Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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type
label
Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
@en
Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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prefLabel
Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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P2093
P50
P1476
Subduction and accretion of se ...... . Elias orogen, Gulf of Alaska
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P2093
Harm J.A. Van Avendonk
Kenneth D. Ridgway
Terry L. Pavlis
P304
P356
10.1016/J.EPSL.2013.08.049
P407
P577
2013-11-01T00:00:00Z