High- to ultrahigh-temperature metamorphism in the lower crust: An example resulting from Hikurangi Plateau collision and slab rollback in New Zealand-Reference-Cited by-同舟云学术

High- to ultrahigh-temperature metamorphism in the lower crust: An example resulting from Hikurangi Plateau collision and slab rollback in New Zealand

Published:2017-08-07 Issue:8 Volume:35 Page:831-853
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Jacob Jean-Baptiste¹,Scott James M.¹^ORCID,Turnbull Rose E.²,Tarling Matthew S.¹,Sagar Matthew W.³

Affiliation:

1. Department of Geology; University of Otago; Dunedin New Zealand

2. GNS Science; Dunedin Research Centre; Dunedin New Zealand

3. School of Geography, Environment and Earth Sciences; Victoria University of Wellington; Wellington New Zealand

Funder

GNS Science's Minerals, Urban and Regional Geology programme

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12257/fullpdf

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3. Excess heat capacity and entropy of mixing in ternary series of high-structural-state feldspars;Benisek;European Journal of Mineralogy,2010

4. Peak metamorphic temperature and thermal history of the Southern Alps (New Zealand);Beyssac;Tectonophysics,2016

5. Progressive metamorphism from prehnite-pumpellyite to greenschist facies in the Dansey Pass area, Otago, New Zealand;Bishop;Geological Society of America Bulletin,1972

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