نتایج جستجو برای: volcanic arc

تعداد نتایج: 50065  

1998
Max W. Schmidt Stefano Poli

Phase diagrams of hydrous mid-ocean ridge (MOR) basalts to 330 km depth and of hydrous peridotites to 250 km depth are compiled for conditions characteristic for subduction zones. A synthesis of our experimentally determined phase relations of chlorite, lawsonite, epidote-zoisite, amphibole, paragonite, chloritoid, talc, and phengite in basalts and of phase relations from the literature of serp...

2014
Yan Hu Roland Bürgmann Jeffrey T Freymueller Paramesh Banerjee Kelin Wang

A better understanding of fluid-related processes such as poroelastic rebound of the upper crust and weakening of the lower crust beneath the volcanic arc helps better understand and correctly interpret the heterogeneity of postseismic deformation following great subduction zone earthquakes. The postseismic deformation following the 2011 Mw9.0 Tohoku earthquake, recorded with unprecedented high...

1999
J. A. PEARCE P. D. KEMPTON G. M. NOWELL S. R. NOBLE

attributed directly to subduction. One option consistent with Hf–Nd This paper develops methods for using the integrated study of systematics is that the positive Hf anomalies in the Protoarc boninites Hf–Nd element and isotope covariations to define the nature and were caused by fusion of mafic veins in their shallow mantle sources. provenance of the mantle and subduction inputs to subduction ...

2008
ROBERT J. STERN YOSHIHIKO TAMURA ROBERT W. EMBLEY OSAMU ISHIZUKA SUSAN G. MERLE NEIL K. BASU HIROSHI KAWABATA SHERMAN H. BLOOMER

West Rota Volcano (WRV) is a recently discovered extinct submarine volcano in the southern Mariana Arc. It is large (25 km diameter base), shallow (up to 300 m below sealevel), and contains a large caldera (6 ¥ 10 km, with up to 1 km relief). The WRV lies near the northern termination of a major NNE-trending normal fault. This and a second, parallel fault just west of the volcano separate uplif...

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