Titlebook: Backarc Basins; Tectonics and Magmat Brian Taylor Book 1995 Springer Science+Business Media New York 1995 evolution.geology.sediment.sedime

Migratory

Taupo Volcanic Zone and Central Volcanic Region Backarc Structures of North Island, New Zealand, the highest on record for a backarc basin. Rates of extension in the currently active TVZ are about 7 mm/yr in the north and 18 mm/yr in the south, derived from shear strain rates varying between 0.18 and 0.5 × 10./yr shear. Subsidence rates are 1–2 mm/yr. Focal mechanisms from recent small earthqu

MUMP

The Southern Havre Trough Geological Structure and Magma Petrogenesis of an Active Backarc Rift Comhward toward New Zealand, penetrating the continental-oceanic arc crustal boundary. Contrary to previous models, the entire Havre Trough is now interpreted to be undergoing backarc rifting prior to true spreading, with the attendant tectonic fabric dextrally oblique to the bounding Colville and Kerm

nerve-sparing

amyloid

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