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Статті в журналах з теми "Amphibolite geochemistry"
Fonseca, Ariadne Do Carmo. "Fragmento tectónico cabo frio: aspectos de campo, petrografía e geoquímica." Anuário do Instituto de Geociências 17 (December 1, 1994): 109–31. http://dx.doi.org/10.11137/1994_0_109-131.
Повний текст джерелаBOGDANOVA, Alyona Romanovna, Nadezhda Vladimirovna VAKHRUSHEVA, and Pavel Borisovich SHIRYAEV. "Main and rare earth elements of amphibolites of the Ray-Iz massif (Polar Urals)." NEWS of the Ural State Mining University, no. 4 (December 20, 2020): 19–27. http://dx.doi.org/10.21440/2307-2091-2020-4-19-27.
Повний текст джерелаAhmid-Said, Y., and B. E. Leake. "The composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria." Mineralogical Magazine 56, no. 385 (December 1992): 459–68. http://dx.doi.org/10.1180/minmag.1992.056.385.02.
Повний текст джерелаMoazzen, Mohssen, Zohreh Salimi, Yann Rolland, Michael Bröcker, and Robab Hajialioghli. "Protolith nature and P–T evolution of Variscan metamorphic rocks from the Allahyarlu complex, NW Iran." Geological Magazine 157, no. 11 (March 18, 2020): 1853–76. http://dx.doi.org/10.1017/s0016756820000102.
Повний текст джерелаBogoch, R., and M. Shirav. "Carbonate nodules of probable stromatolitic origin in amphibolite from the Neoproterozoic terrain of southern Israel." Mineralogical Magazine 68, no. 4 (August 2004): 579–89. http://dx.doi.org/10.1180/0026461046840213.
Повний текст джерелаMoyen, Jean-François, and Gordon R. Watt. "Pre-Nagssugtoqidian crustal evolution in West Greenland: geology, geochemistry and deformation of supracrustal and granitic rocks north-east of Kangaatsiaq." Geological Survey of Denmark and Greenland (GEUS) Bulletin 11 (December 5, 2006): 33–52. http://dx.doi.org/10.34194/geusb.v11.4915.
Повний текст джерелаSoret, Mathieu, Philippe Agard, Benoît Ildefonse, Benoît Dubacq, Cécile Prigent, and Claudio Rosenberg. "Deformation mechanisms in mafic amphibolites and granulites: record from the Semail metamorphic sole during subduction infancy." Solid Earth 10, no. 5 (October 23, 2019): 1733–55. http://dx.doi.org/10.5194/se-10-1733-2019.
Повний текст джерелаDolníček, Zdeněk, and Jana Ulmanová. "Chemické složení granátů v amfibolitech z lomu Libodřice u Kolína (kutnohorské krystalinikum, Česká republika)." Bulletin Mineralogie Petrologie 30, no. 2 (2022): 205–13. http://dx.doi.org/10.46861/bmp.30.205.
Повний текст джерелаShiraishi, Kazuyuki, Takanobu Oba, Morihisa Suzuki, and Ken’ichi Ishikawa. "Subsilicic magnesian potassium-hastingsite from the Prince Olav Coast, East Antarctica." Mineralogical Magazine 58, no. 393 (December 1994): 621–27. http://dx.doi.org/10.1180/minmag.1994.058.393.11.
Повний текст джерелаBelic, Maximilian, Christoph A. Hauzenberger, and Yunpeng Dong. "Multistage Metamorphic Evolution of Retrograded Eclogites from the Songshugou Complex, Qinling Orogenic Belt, China." Journal of Petrology 60, no. 11 (November 1, 2019): 2201–26. http://dx.doi.org/10.1093/petrology/egaa007.
Повний текст джерелаДисертації з теми "Amphibolite geochemistry"
Wang, Weiliang. "Amphibolites of the Bangong-Nujiang suture zone, Tibet." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/B41897237.
Повний текст джерелаGuilmette, Carl. "Petrology, geochemistry and geochronology of highly foliated amphibolites from the ophiolitic mélange beneath the Yarlung Zangbo ophiolites, Xigaze area, Tibet : geodynamical implications." Master's thesis, Université Laval, 2005. http://hdl.handle.net/20.500.11794/18102.
Повний текст джерелаBlocks of highly foliated amphibolites are locally found within the serpentinite matrix mélange underlying the Yarlung Zangbo ophiolites near Bainang and Buma, Xigaze area, Yarlung Zangbo Suture Zone (YZSZ), Tibet. The mélange is thought to be the result of the tectonic dismemberment of the base of the ophiolitic napes during its obduction over the Indian passive margin, circa 50 Ma. Prior to dismemberment, amphibolites were probably parts of a coherent dynamothermal sole, as observed at the base of many ophiolites. Sampled amphibolites can be subdivided in three groups: garnet, banded and common amphibolites. Medium-grained garnet amphibolites contain the assemblage A) Hb+CPX+Gt+Pl±Rt and B) Gt+Hb+Pl (corona assemblage). Fine to medium-grained banded amphibolites contain the assemblage C) Hb+CPX+Pl+Ep±Sp+Qtz+Ap. Fine-grained common amphibolites contain facies D) Hb+Pl±Ep+Ap+Sp. In all assemblages, plagioclase is pseudomorphosed by an albite-prehnite simplectite. Retrograde cataclastic veins contain the assemblage E) Ab+Pr±Ch+Ep. The geochemistry of the garnet, banded and common amphibolites is very similar to the geochemistry of other mafic blocks in the mélange and of mafic igneous rocks within the ophiolitic massifs. When compared to MORBs, light depletion of LREE (La/Yb = 0.65-0.97) and mild HFSE depletion (Ta/Th = 0.33-0.65) would suggest a mixing between the IAT and MORB sources, as seen in back-arc basins and nascent intra-oceanic arcs. The amphibolites were buried at the inception of a subduction within the back-arc to peak metamorphism conditions of 11-14 kbars and ~800 °C. Ar/Ar analysis of amphiboles revealed a metamorphic age of 121-130 Ma, which is synchronous with ages obtained from the overlying ophiolites. Overlapping in ophiolite-sole age relationship reveals inception of the subduction near or at the spreading center from which originated the ophiolite. Subduction of a buoyant body could explain heterogeneous coronitization of pyrope-rich (up to 35 %) garnet by Al-Tschermakites (Al2O3 up to 21 wt %) at high-pressures. After exhumation, amphibolites were injected by very fine-grained diabasic dykes and were subject to percolation of a prehnite-precipitating fluid. Oxygen stable isotopes suggest that a magmatic fluid is responsible for prehnite precipitation. The magmatic and metamorphic history of the dynamothermal sole and field relationships with adjacent units seem to indicate that most of Neo-Tethys oceanic domain was subducted along this new Late Cretaceous subduction zone.
Wang, Weiliang, and 王維亮. "Amphibolites of the Bangong-Nujiang suture zone, Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B41897237.
Повний текст джерелаFernandez, Laure. "Etude géochimique et géochronologique d'un massif basique et ultrabasique des zones internes de la chaîne des Maghrébides (Edough, NE Algégrie) : contraintes sur l'évolution de la Méditerranée Occidentale au Cénozoïque." Thesis, Montpellier, 2015. http://www.theses.fr/2015MONTS102/document.
Повний текст джерелаThe Edough massif is the Easternmost crystalline massif of the Maghrebide belt. This area presents strong similarities with the internal zones of the Peri-Mediterranean Alpine belt but its evolution stillremains poorly constrained. Edough can be approximated as a metamorphic dome of gneisses and migmatites containing garnet amphibolite and metaperidotites of Sidi Mohamed in its core. In the North, the dome is overlain by a nappe stack constituted by a “melange” unit composed of various lithologies and, upward, by the Kef Lakhal massive amphibolites of oceanic origin. This work is focused on three units containing mafic and ultramafic lithologies i.e. the Sidi Mohamed peridotites, the “melange” unit and the Kef Lakhal amphibolites. The aim of this Ph.D. work is to characterize all three units, to determine their relationships and establish the timing of the main events identified. We chose a combined geochronological-geochemical approach using in situ analyses (major and trace elements, U-Pb geochronology and Hf isotopes on accessory minerals) and bulk analyses on whole rock/mineral fraction (major and trace elements, Ar-Ar geochronology and Sr-Nd-Pb-Hf isotopes). We show that the Sidi Mohamed mafic rocks display an affinity with the Alboran mantle. The mantle rocks from Sidi Mohamed display affinities with a subcontinental mantle influenced by subduction processes and late metamorphism at crustal levels. The melange unit is interpreted as a Permo-Carboniferous passive margin. The amphibolite lenses in the mélange unit originate from a mantle modified by subduction processes. This unit contains relics of Ultra-High Pressure rocks as evidenced by the occurrence of diamonds in a megacrystal of garnet showing oceanic affinities. These ultra-high pressure rocks document a prograde stage at ~32 Ma and exhumation to lower crustal levels at ~21 Ma. The Kef Lakhal unit displays oceanic crust-like signatures and characteristics of fluid induced signatures. We interpret the Kef Lakhal amphibolites as a shallow subducted Tethys fragment, which was exhumed at 21 Ma. We propose that the Edough massif represents the Permo-carboniferous passive margin of Africa basement onto which a fragment of the Tethys Ocean was thrusted. The whole massif was finally exhumed as a metamorphic core complex at 18 Ma and experienced fast cooling until ~16 Ma. We relate this fast processes to the interplay between trench and slab movements
Dalpé, Claude. "Trace element partitioning between amphibole and basaltic melt." Thesis, McGill University, 1997. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=34939.
Повний текст джерелаKuyumjian, Raul Minas. "The geochemistry and tectonic significance of amphibolites from the Chapada sequence, Central Brazil." Thesis, Imperial College London, 1989. http://hdl.handle.net/10044/1/47522.
Повний текст джерелаInjoque-Espinoza, J. "Geochemistry of the Cu-Fe-amphibole skarn deposits of the Peruvian coast." Thesis, University of Nottingham, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.355424.
Повний текст джерелаCHWAE, Ueechan, Izumi KAJIZUKA, Daniel J. DUNKLEY, and Kazuhiro SUZUKI. "A preliminary report on the geochemistry of amphibolites from the Chuncheon area in the Gyeonggi massif, Korea." Dept. of Earth and Planetary Sciences, Nagoya University, 2009. http://hdl.handle.net/2237/14731.
Повний текст джерелаRosatelli, Gianluigi. "The petrogenesis of carbonitic rocks and their relation to mantle amphibole and carbonate as exemplified in contrasting volcanoes from Vulture, Italy and Rangwa, East Africa." Thesis, University College London (University of London), 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.252281.
Повний текст джерелаCollins, Nathan. "Geochemical Systematics Among Amphibolitic Rocks in the Central Blue Ridge Province of southwestern North Carolina." Scholar Commons, 2011. http://scholarcommons.usf.edu/etd/3045.
Повний текст джерелаКниги з теми "Amphibolite geochemistry"
Awdankiewicz, Honorata. Petrologia i geochemia metabazytów masywu Niedźwiedzia na bloku przedsudeckim: The petrology and geochemistry of the metabasites of the Niedźwiedź Massif in the Fore-Sudetic Block. Warszawa: Państwowy Instytut Geologiczny, 2008.
Знайти повний текст джерелаLaurs, Brendan M. Emerald mineralization and amphibolite wall-rock alteration at the Khaltaro pegmatite-hydrothermal vein system, Haramosh Mountains, Northern Pakistan. 1995.
Знайти повний текст джерелаЧастини книг з теми "Amphibolite geochemistry"
Cummings, Michael L., and William R. McCulloch. "Geochemistry and origin of amphibolite and ultramafic rocks, Branham Lakes area, Tobacco Root Mountains, southwestern Montana." In Proceedings of the International Conferences on Basement Tectonics, 323–40. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-1614-5_22.
Повний текст джерелаOlajide-Kayode, Jerry, Olugbenga Okunlola, and Akinade Olatunji. "Geochemistry and Mineral Chemistry of Amphibolites in Parts of the Proterozoic Ilesa Schist Belt, Southwestern Nigeria." In Advances in Science, Technology & Innovation, 333–35. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-72547-1_71.
Повний текст джерелаShimabukuro, David H., and Claire Battistella. "Ligurian hyperextended continental margin preserved in an ophiolitic block at Timpa di Pietrasasso, Calabrian Arc, southern Italy." In From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid: Honoring the Career of Walter Alvarez. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2557(10).
Повний текст джерелаAmgaa, Tsolmon, Dieter Mader, Wolf Uwe Reimold, and Christian Koeberl. "Tabun Khara Obo impact crater, Mongolia: Geophysics, geology, petrography, and geochemistry." In Large Meteorite Impacts and Planetary Evolution VI. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2550(04).
Повний текст джерелаBaird, Graham B., Timothy W. Grover, Kevin H. Mahan, Michael G. Frothingham, Markus B. Raschke, Andreas Möller, Adam S. Chumley, Jacob C. Hooker, Nigel M. Kelly, and Julien M. Allaz. "Paleoproterozoic tectonics of the northern Colorado Rocky Mountains Front Range, USA." In Field Excursions in the Front Range and Wet Mountains of Colorado for GSA Connects 2022, 39–66. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.0064(03).
Повний текст джерелаSmith Nagihara, S., and J. F. Casey. "Whole-rock geochemistry of amphibolites and metagabbros from the west Iberia Margin, Leg 173." In Proceedings of the Ocean Drilling Program. Ocean Drilling Program, 2001. http://dx.doi.org/10.2973/odp.proc.sr.173.011.2001.
Повний текст джерелаТези доповідей конференцій з теми "Amphibolite geochemistry"
Baird, Graham, and Adam S. Chumley. "TECTONIC STYLE INSIGHTS FROM PALEOPROTEROZOIC AMPHIBOLITE GEOCHEMISTRY, BIG THOMPSON AND POUDRE CANYONS, NORTHERN COLORADO FRONT RANGE." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380099.
Повний текст джерелаVetter, Scott K., Austin Greber, Kaleb Kirk, Zachary Harrison, Allison Scates, Spencer R. Nelson, Rylan Whan, and David Bieler. "MITCHELL DAM AMPHIBOLITES: GEOCHEMISTRY AND PETROLOGY OF CORE HOLE SAMPLES, SENIOR CLASS PROJECT." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289269.
Повний текст джерелаR, Sierra, David H. Shimabukuro, Jo Black, and Steven Skinner. "GEOCHEMISTRY, GEOCHRONOLOGY, AND THERMOBAROMETRY OF HIGH-PRESSURE AMPHIBOLITES FROM THE CENTRAL ARC AND MELANGE BELT NEAR COLFAX, CALIFORNIA." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363222.
Повний текст джерелаHampel, Tim, Michael Rowe, and Adam J. R. Kent. "Reassessing Volatile and Trace Element Mobility at Mount St. Helens (2004-2008) from Amphibole and Melt Inclusion Geochemistry." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.939.
Повний текст джерелаGeneviève, Tsama Mbani, Ekollo Kingue Ngolle Serge, Tchouffa Bertrand Boris, and Ndong Bidzang François. "GEOCHEMISTRY AND SM-ND DATING OF AMPHIBOLITES OF ESEKA GREEN STONES BELT (NYONG COMPLEX SOUTH CAMEROON): HIGHLIGHTING OF DISTENSIVE EPISODES IN A COMPRESSIVE OROGENIC CONTEXT." In 7th International Scientific Conference GEOBALCANICA 2021. Geobalcanica Society, 2021. http://dx.doi.org/10.18509/gbp210445m.
Повний текст джерелаЗвіти організацій з теми "Amphibolite geochemistry"
Matte, S., M. Constantin, and R. Stevenson. Mineralogical and geochemical characterisation of the Kipawa syenite complex, Quebec: implications for rare-earth element deposits. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329212.
Повний текст джерелаCaritat, P. de, and U. Troitzsch. Towards a regolith mineralogy map of the Australian continent: a feasibility study in the Darling-Curnamona-Delamerian region. Geoscience Australia, 2021. http://dx.doi.org/10.11636/record.2021.035.
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