Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Raphael Quentin de Gromard"'
Autor:
Christopher L. Kirkland, Maximilian Dröllner, Raphael Quentin de Gromard, Bruno V. Ribeiro, Hugo K. H. Olierook, Michael Hartnady, Milo Barham, Janne Liebmann, Hugh Smithies, Andreas Zametzer
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-12 (2024)
Abstract Deep geology of ancient continental crust can be difficult to access, with direct observation restricted to limited exposures. The age and composition of hidden geology can be gleaned from indirect isotopic modelling or via detrital minerals
Externí odkaz:
https://doaj.org/article/946e65d58a50467a966b92df434e1ddd
Publikováno v:
Journal of Metamorphic Geology. 38:831-852
Preservation of partially completed metamorphic reactions in the form of partial pseudomorphs is very important as it provides direct insight onto the reaction mechanism and the phases involved in the reaction. The staurolite and andalusite grade roc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ccf709f58c745e3775bf643ff037631
https://doi.org/10.1111/jmg.12551
https://doi.org/10.1111/jmg.12551
Autor:
Christopher L. Kirkland, Raphael Quentin de Gromard, Noreen J. Evans, R. Hugh Smithies, Michael T.D. Wingate, H.M. Howard, Brent I.A. McInnes, Martin Danišík, Bradley J. McDonald, Fred Jourdan
Publikováno v:
Geoscience Frontiers, Vol 10, Iss 1, Pp 149-164 (2019)
The post-Mesoproterozoic tectonometamorphic history of the Musgrave Province, central Australia, has previously been solely attributed to intracontinental compressional deformation during the 580–520 Ma Petermann Orogeny. However, our new structura
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e846b46d1d5a8ef09685a00ca1a94438
http://www.sciencedirect.com/science/article/pii/S1674987118301993
http://www.sciencedirect.com/science/article/pii/S1674987118301993
Publikováno v:
Geoscience Frontiers, Vol 6, Iss 1, Pp 23-37 (2015)
The Musgrave Province developed at the nexus of the North, West and South Australian cratons and its Mesoproterozoic evolution incorporates a 100 Ma period of ultra-high temperature (UHT) metamorphism from ca. 1220 to ca. 1120 Ma. This was accompanie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2183f7e9c5b33b5a1d4688b2bc875fbe
https://doi.org/10.1016/j.gsf.2014.03.001
https://doi.org/10.1016/j.gsf.2014.03.001
Autor:
Raphael Quentin de Gromard
Publikováno v:
Tectonophysics. 587:168-187
E–W structural and igneous trends in the Charters Towers Province are highly anomalous within the overall N–S trending Tasman orogen of eastern Australia and resulted from a sequence of N–S shortening events. A succession of ~ E–W trending FI
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03e22e8d733fe145ad950fde3629cc39
https://doi.org/10.1016/j.tecto.2012.09.002
https://doi.org/10.1016/j.tecto.2012.09.002