Mantle wedge anisotropy in the Hikurangi subduction zone, central North Island, New Zealand

[1] The anisotropic characteristics of the Hikurangi subduction zone in central North Island, New Zealand are studied using shear-wave splitting measurements from 55 local earthquakes recorded on a 200 km profile of 19 stations. The eastern fore-arc shows trench-parallel fast directions and a low av...

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מידע ביבליוגרפי
Main Authors: Morley, AM, Stuart, GW, Kendall, J, Reyners, M
פורמט: Journal article
שפה:English
יצא לאור: Wiley 2006