Search Results - "Toy, V.G."
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A Late Cretaceous and Cenozoic reconstruction of the Southwest Pacific region: Tectonics controlled by subduction and slab rollback processes
Published in Earth-science reviews (01-06-2006)“…A Cenozoic tectonic reconstruction is presented for the Southwest Pacific region located east of Australia. The reconstruction is constrained by large…”
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Hydraulic and acoustic properties of the active Alpine Fault, New Zealand: Laboratory measurements on DFDP-1 drill core
Published in Earth and planetary science letters (15-03-2014)“…We report on laboratory measurements of permeability and elastic wavespeed for a suite of samples obtained by drilling across the active Alpine Fault on the…”
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Microstructures imply cataclasis and authigenic mineral formation control geomechanical properties of New Zealand's Alpine Fault
Published in Journal of structural geology (01-05-2018)“…The Alpine Fault is capable of generating large (MW > 8) earthquakes and is the main geohazard on South Island, NZ, and late in its 250–291-year seismic cycle…”
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How do lineations reflect the strain history of transpressive shear zones? The example of the active Alpine Fault zone, New Zealand
Published in Journal of structural geology (01-05-2013)“…Lineations within mylonites exhumed in the hanging wall of New Zealand's active Alpine Fault zone have a complicated relationship to contemporary plate…”
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Recrystallisation, phase mixing and strain localisation in peridotite during rapid extrusion of sub-arc mantle lithosphere
Published in Journal of structural geology (01-07-2016)“…The Anita Peridotite, in southwestern New Zealand, is a ∼1 × 20 km ultramafic massif that was rapidly extruded from beneath a Cretaceous arc within the 4 km…”
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Significance of brittle deformation in the footwall of the Alpine Fault, New Zealand: Smithy Creek Fault zone
Published in Journal of structural geology (01-07-2014)“…The Smithy Creek Fault represents a rare exposure of a brittle fault zone within Australian Plate rocks that constitute the footwall of the Alpine Fault zone…”
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Localisation of deformation in the thermal contrast at a granite batholith margin, New Zealand
Published in Journal of structural geology (01-07-2014)“…The Wainui Shear Zone is a ∼ 1.2 km wide steeply dipping ductile shear zone that is intimately associated with the western margin of a very extensive granite…”
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