Academic literature on the topic 'Fluid assisted metamorphism'
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Journal articles on the topic "Fluid assisted metamorphism"
Touret, Jacques L. R., and Jan Marten Huizenga. "Fluid-assisted granulite metamorphism: A continental journey." Gondwana Research 21, no. 1 (January 2012): 224–35. http://dx.doi.org/10.1016/j.gr.2011.07.022.
Full textAdmou, Safouane, Yannick Branquet, Lakhlifi Badra, Luc Barbanson, Mohamed Outhounjite, Abdelali Khalifa, Mohamed Zouhair, and Lhou Maacha. "The Hajjar Regional Transpressive Shear Zone (Guemassa Massif, Morocco): Consequences on the Deformation of the Base-Metal Massive Sulfide Ore." Minerals 8, no. 10 (October 7, 2018): 435. http://dx.doi.org/10.3390/min8100435.
Full textLi, Yang, Ai-Cheng Zhang, Jia-Ni Chen, Li-Xin Gu, and Ru-Cheng Wang. "Formation of phosphorus-rich olivine in Dar al Gani 978 carbonaceous chondrite through fluid-assisted metamorphism." American Mineralogist 102, no. 1 (January 2017): 98–107. http://dx.doi.org/10.2138/am-2017-5881.
Full textWhittington, A. G., and P. J. Treloar. "Crustal anatexis and its relation to the exhumation of collisional orogenic belts, with particular reference to the Himalaya." Mineralogical Magazine 66, no. 1 (February 2002): 53–91. http://dx.doi.org/10.1180/0026461026610015.
Full textFornelli, Annamaria, Vincenzo Festa, Francesca Micheletti, Richard Spiess, and Fabrizio Tursi. "Building an Orogen: Review of U-Pb Zircon Ages from the Calabria–Peloritani Terrane to Constrain the Timing of the Southern Variscan Belt." Minerals 10, no. 11 (October 23, 2020): 944. http://dx.doi.org/10.3390/min10110944.
Full textVacher, Lionel G., and Wataru Fujiya. "Recent Advances in our Understanding of Water and Aqueous Activity in Chondrites." Elements 18, no. 3 (June 1, 2022): 175–80. http://dx.doi.org/10.2138/gselements.18.3.175.
Full textDidier, A., V. Bosse, Z. Cherneva, P. Gautier, M. Georgieva, J. L. Paquette, and I. Gerdjikov. "Syn-deformation fluid-assisted growth of monazite during renewed high-grade metamorphism in metapelites of the Central Rhodope (Bulgaria, Greece)." Chemical Geology 381 (August 2014): 206–22. http://dx.doi.org/10.1016/j.chemgeo.2014.05.020.
Full textHoerlle, Guilherme Sonntag, Marcus Vinicius Dorneles Remus, and Norberto Dani. "Metamafic dyke and sill swarms in the Dom Feliciano Belt: Insights for post-collisional strike-slip tectonics and fluid-assisted metamorphism." Precambrian Research 383 (December 2022): 106906. http://dx.doi.org/10.1016/j.precamres.2022.106906.
Full textTursi, Fabrizio. "The key role of µH2O gradients in deciphering microstructures and mineral assemblages of mylonites: examples from the Calabria polymetamorphic terrane." Mineralogy and Petrology 116, no. 1 (October 20, 2021): 1–14. http://dx.doi.org/10.1007/s00710-021-00766-8.
Full textKapsiotis, Argyrios. "Composition and alteration of Cr-spinels from Milia and Pefki serpentinized mantle peridotites (Pindos Ophiolite Complex, Greece)." Geologica Carpathica 65, no. 1 (February 1, 2014): 83–95. http://dx.doi.org/10.2478/geoca-2013-0006.
Full textDissertations / Theses on the topic "Fluid assisted metamorphism"
Bhowany, K. "Eclogite; fluid assisted metamorphism; P–T pseudosections; Caledonian Orogeny; Bergen Arcs; P–T path." Thesis, 2015. http://hdl.handle.net/2440/117958.
Full textExhumed deep crust is rare and exposures that preserve both protoliths and altered domains are limited around the world. Mesoproterozoic anorthositic granulites exposed on the island of Holsnøy, western Norway, preserve different stages of progressive deformation together with the corresponding metamorphism that record the conversion to Siluro-Ordovician eclogites during fluid infiltration. Five different stages of deformation can be identified: 1) brittle deformation resulting in the formation of fractures and generation of pseudotachylites in the granulite; 2) development of mesoscale shear zones associated with increased fluid–rock interaction; 3) large-scale replacement of granulite by hydrous eclogite with blocks of granulite sitting in an eclogitic ‘matrix’; 4) complete conversion of granulite to eclogite within large-scale shear zones; and 5) break up of completely eclogitised granulite by continued fluid influx, resulting in the formation of potassium-rich mineral assemblages. P–T constraints derived from phase equilibria forward modelling document a burial and partial exhumation path with peak conditions around 21–22 kbar and 640–660 °C. Fluid infiltration began on the prograde path and continued throughout the recorded P–T evolution. However, in places limited fluid availability on the prograde path resulted in an excellent preservation of prograde mineral assemblage, allowing the burial path to be well constrained.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Book chapters on the topic "Fluid assisted metamorphism"
Oliver, Nicholas H. S., Andrew Allibone, Michael J. Nugus, Carlos Vargas, Richard Jongens, Richard Peattie, and Vaughan A. Chamberlain. "Chapter 6: The Supergiant, High-Grade, Paleoproterozoic Metasedimentary Rock- and Shear Vein-Hosted Obuasi (Ashanti) Gold Deposit, Ghana, West Africa." In Geology of the World’s Major Gold Deposits and Provinces, 121–40. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.06.
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