Subduction zone anisotropy beneath Corvallis, Oregon: A serpentinite skid mark of trench‐parallel terrane migration?

Publisher: John Wiley & Sons Inc

E-ISSN: 2156-2202|109|B10|2003JB002718-2003JB002718

ISSN: 0148-0227

Source: Journal Of Geophysical Research, Vol.109, Iss.B10, 2004-10, pp. : n/a-n/a

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Abstract