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- W2943459502 abstract "Abstract The Dun Mountain ophiolite, South Island, New Zealand, records complex overprinting of mantle fabrics. Using structural observations, microstructural analysis, geothermometry, geobarometry, geochronology and rheological constraints from the Red Hills and Dun Mountain massifs, we propose that three deformation events occurred during the early stages of subduction initiation along the Permian margin of Gondwana. During the first deformation event, the lineated Two Tarns Harzburgite from the Red Hills formed in a transtensional setting associated with subduction initiation. Deformation was pervasive, homogeneous and simultaneous with boninitic melt migration through the unit; it also occurred at very fast strain rates (10−9–10−8 s−1). During the second deformation event, progressive exhumation to c. 5 kbar and cooling to 1000°C led to the localization of melt and deformation into distinct zones (Dun Mountain, and the Plateau Complex, Plagioclase Zone and Ellis Stream Complex of the Red Hills). The third deformation event resulted in continued cooling and exhumation along serpentinized faults. This history provides a rare glimpse of the coupled fabric development and melt migration that sequentially develop in the early mantle wedge during the initiation of a subduction zone." @default.
- W2943459502 created "2019-05-09" @default.
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- W2943459502 date "2019-01-01" @default.
- W2943459502 modified "2023-09-26" @default.
- W2943459502 title "Chapter 6 Coupled deformation and melt-migration events recording subduction initiation, Dun Mountain ophiolite, New Zealand" @default.
- W2943459502 cites W1496399568 @default.
- W2943459502 cites W1510217688 @default.
- W2943459502 cites W1543257786 @default.
- W2943459502 cites W1593136970 @default.
- W2943459502 cites W1654749589 @default.
- W2943459502 cites W1669138304 @default.
- W2943459502 cites W1968999833 @default.
- W2943459502 cites W1970758245 @default.
- W2943459502 cites W1971281588 @default.
- W2943459502 cites W1973365735 @default.
- W2943459502 cites W1973990596 @default.
- W2943459502 cites W1979906797 @default.
- W2943459502 cites W1985160890 @default.
- W2943459502 cites W1991475651 @default.
- W2943459502 cites W1993052821 @default.
- W2943459502 cites W2008412316 @default.
- W2943459502 cites W2009121591 @default.
- W2943459502 cites W2011449231 @default.
- W2943459502 cites W2012428364 @default.
- W2943459502 cites W2019143985 @default.
- W2943459502 cites W2021730199 @default.
- W2943459502 cites W2021862210 @default.
- W2943459502 cites W2022857073 @default.
- W2943459502 cites W2036016724 @default.
- W2943459502 cites W2036279624 @default.
- W2943459502 cites W2036293114 @default.
- W2943459502 cites W2039269540 @default.
- W2943459502 cites W2041176411 @default.
- W2943459502 cites W2041975117 @default.
- W2943459502 cites W2042692134 @default.
- W2943459502 cites W2046141409 @default.
- W2943459502 cites W2046294829 @default.
- W2943459502 cites W2047519592 @default.
- W2943459502 cites W2048044581 @default.
- W2943459502 cites W2051241532 @default.
- W2943459502 cites W2053907214 @default.
- W2943459502 cites W2062561986 @default.
- W2943459502 cites W2065051607 @default.
- W2943459502 cites W2069873041 @default.
- W2943459502 cites W2071610076 @default.
- W2943459502 cites W2075557265 @default.
- W2943459502 cites W2077188212 @default.
- W2943459502 cites W2078477853 @default.
- W2943459502 cites W2084072312 @default.
- W2943459502 cites W2085629521 @default.
- W2943459502 cites W2092678733 @default.
- W2943459502 cites W2096473959 @default.
- W2943459502 cites W2099995121 @default.
- W2943459502 cites W2101046437 @default.
- W2943459502 cites W2101320847 @default.
- W2943459502 cites W2104959535 @default.
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- W2943459502 cites W2127705220 @default.
- W2943459502 cites W2129886013 @default.
- W2943459502 cites W2139316879 @default.
- W2943459502 cites W2152495027 @default.
- W2943459502 cites W2153024854 @default.
- W2943459502 cites W2161493148 @default.
- W2943459502 cites W2162260886 @default.
- W2943459502 cites W2163683475 @default.
- W2943459502 cites W2164336999 @default.
- W2943459502 cites W2266383339 @default.
- W2943459502 cites W2312255672 @default.
- W2943459502 cites W2321767914 @default.
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- W2943459502 cites W2611705086 @default.
- W2943459502 cites W2924406045 @default.
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- W2943459502 doi "https://doi.org/10.1144/m49.5" @default.
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