Zobrazeno 1 - 5
of 5
pro vyhledávání: '"M. C. De Paoli"'
Publikováno v:
Australian Journal of Earth Sciences. 69:1149-1176
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::088782c36df2ed2b94fd26a0882d9625
https://doi.org/10.1080/08120099.2022.2102076
https://doi.org/10.1080/08120099.2022.2102076
Autor:
Mark Peternell, Roberto F. Weinberg, I. Zibra, Malcolm P. Roberts, S. Romano, M. C. De Paoli, Roberto Braga, Fawna J. Korhonen
During the Neoarchean, the dominant tectonic style progressively changed from an episodic-overturn/stagnant-lid regime to modern-style plate tectonics. The Neoarchean strengthening of continental lithosphere changed the style of deformation of orogen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::09a74754d6d7c2f786028cb519f32b74
http://hdl.handle.net/11585/603682
http://hdl.handle.net/11585/603682
Publikováno v:
Journal of Petrology. 53:949-970
P^T^X(composition) pseudosections constructed for natural monzodioritic to peridotgabbroic rock compositions using THERMOCALC in the model system Na2O^CaO^K2O^FeO^MgO^Al2O3^ SiO2^H2O^TiO2^O (NCKFMASHTO) illustrate the dependence of granulite and eclo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a7a3c09208eedd7d27d47ec8ed2e048
https://doi.org/10.1093/petrology/egs004
https://doi.org/10.1093/petrology/egs004
The Eclogite-Granulite Transition: Mafic and Intermediate Assemblages at Breaksea Sound, New Zealand
Publikováno v:
Journal of Petrology. 50:2307-2343
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aaf271de739a2efa57f1580a8a6b508e
https://doi.org/10.1093/petrology/egp078
https://doi.org/10.1093/petrology/egp078
Autor:
Nathan R. Daczko, L. A. Milan, M. C. De Paoli, I. M. Turnbull, R. Jongens, Andrew J. Tulloch, Andrew Allibone
Publikováno v:
New Zealand Journal of Geology and Geophysics. 52:379-415
This paper provides a comprehensive description of the plutonic rocks of western Fiordland between Breaksea and Sutherland Sounds. The area is dominated by the Early Cretaceous Western Fiordland Orthogneiss (WFO), but also includes smaller bodies of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::932c68b66e2621d36cd2f4558276978d
https://doi.org/10.1080/00288306.2009.9518465
https://doi.org/10.1080/00288306.2009.9518465