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Статті в журналах з теми "Intracontinental magmatism"
Huo, Hailong, Da Zhang, Zhengle Chen, Yongjun Di, Xiaolong He, Ning Li, and Bojie Hu. "Geochemistry and Zircon U–Pb Geochronology of the Zhuxi Granites in the Jingdezhen Area, Jiangxi Province, China: Implications for the Mesozoic Tectonic Development of South China." Minerals 12, no. 3 (February 24, 2022): 283. http://dx.doi.org/10.3390/min12030283.
Повний текст джерелаMao, Jianren, Kuiyuan Tao, Zhuliang Yang, Yunhe Zhu, and Huaimin Xue. "Geodynamic background of the mesozoic intracontinental magmatism in Southeast China." Chinese Journal of Geochemistry 16, no. 3 (July 1997): 230–39. http://dx.doi.org/10.1007/bf02870906.
Повний текст джерелаGvirtzman, Zohar, and Zvi Garfunkel. "Vertical movements following intracontinental magmatism: An example from southern Israel." Journal of Geophysical Research: Solid Earth 102, B2 (February 10, 1997): 2645–58. http://dx.doi.org/10.1029/96jb02567.
Повний текст джерелаYu, JinHai, Qian Liu, XiuMian Hu, Qin Wang, and Suzanne Y. O’Reilly. "Late Paleozoic magmatism in South China: Oceanic subduction or intracontinental orogeny?" Chinese Science Bulletin 58, no. 7 (November 16, 2012): 788–95. http://dx.doi.org/10.1007/s11434-012-5376-8.
Повний текст джерелаAshwal, Lewis D., Madelein Patzelt, Mark D. Schmitz, and Kevin Burke. "Isotopic evidence for a lithospheric origin of alkaline rocks and carbonatites: an example from southern Africa." Canadian Journal of Earth Sciences 53, no. 11 (November 2016): 1216–26. http://dx.doi.org/10.1139/cjes-2015-0145.
Повний текст джерелаLee, C. T. A. "Chemical modification of lithosphere and the origin of intracontinental magmatism and deformation." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A346. http://dx.doi.org/10.1016/j.gca.2006.06.701.
Повний текст джерелаAitken, Alan R. A., R. Hugh Smithies, Mike C. Dentith, Aurore Joly, Shane Evans, and Heather M. Howard. "Magmatism-dominated intracontinental rifting in the Mesoproterozoic: The Ngaanyatjarra Rift, central Australia." Gondwana Research 24, no. 3-4 (November 2013): 886–901. http://dx.doi.org/10.1016/j.gr.2012.10.003.
Повний текст джерелаOuyang, Hegen, Jingwen Mao, Zhenhua Zhou, and Huiming Su. "Late Mesozoic metallogeny and intracontinental magmatism, southern Great Xing'an Range, northeastern China." Gondwana Research 27, no. 3 (April 2015): 1153–72. http://dx.doi.org/10.1016/j.gr.2014.08.010.
Повний текст джерелаXu, Wenjing, and Xisheng Xu. "Early Paleozoic intracontinental felsic magmatism in the South China Block: Petrogenesis and geodynamics." Lithos 234-235 (October 2015): 79–92. http://dx.doi.org/10.1016/j.lithos.2015.08.006.
Повний текст джерелаBRIAND, BERNARD, JEAN-LUC BOUCHARDON, PAUL CAPIEZ, and MICHEL PIBOULE. "Felsic (A-type)–basic (plume-induced) Early Palaeozoic bimodal magmatism in the Maures Massif (southeastern France)." Geological Magazine 139, no. 3 (May 2002): 291–311. http://dx.doi.org/10.1017/s0016756802006477.
Повний текст джерелаДисертації з теми "Intracontinental magmatism"
Siqueira, Luzia Helena. "Granito São Domingos : registro de magmatismo pós-tectônico do orógeno intracontinental aguapeí - SW do Cráton Amazônico." Universidade Federal de Mato Grosso, 2015. http://ri.ufmt.br/handle/1/114.
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O Granito São Domingos corresponde a um dos corpos da Suíte Intrusiva Guapé, localizado na Faixa Móvel Aguapeí, relacionado à Orogenia Sunsás, SW do Cráton Amazônico. Trata-se de um corpo com dimensões batolíticas de 150 Km² de área aflorante, levemente alongado segundo direção NE e localizado ao norte do distrito São Domingos, município de Jaurú, estado de Mato Grosso. Constitui-se de rochas holo a leucocráticas, de cor rosa-claro a cinza-rosado, isotrópicas, equi a inequigranulares, por vezes, porfiríticas e pegmatíticas, classificadas como Muscovita biotita monzo a sienogranitos tendo por vezes, granada e monazita como minerais acessórios primários e caracterizadas como granitos do tipo S ou Muscovite bearing Peraluminous Granitoids (MPG). Essas rochas apresentam restritos e elevados teores de sílica, caracterizando-as como muito evoluídas; formadas por magmatismo cálcio alcalino de alto K a shoshonítico, peraluminoso e ferroso. A idade U-Pb (SHRIMP) de 928 ± 5 Ma foi obtida em zircões ígneos, e coincide com idades U-Pb (TIMS) relatadas para este granito. A análise Sm-Nd indica uma idade modelo TDM de 1,58 Ga, e valor ɛND(0,93Ga) negativo (-2,90). Esses resultados indicam que o Granito São Domingos formou-se em um ambiente pós-tectônico, no final da Orogenia Sunsás, cuja origem magmática está associada ao retrabalhamento de crosta continental mesoproterozoica. Três padrões diferentes de ETR foram encontrados para esses litotipos, sugerindo a geração de magmas contemporâneos não cogenéticos, provenientes de fontes crustais distintas.
The São Domingos Granite is an intrusive body of the Guapé Intrusive Suite, located in the Aguapeí mobile belt, corresponding to a branch of the Sunsás Orogeny in SW Amazonian Craton. This body is considered as a batholith slightly elongated in the NE direction, which crops out over an area of ca. 150 km2. It is situated to the north of the São Domingos District, a municipality of the Jauru city, Mato Grosso State. It consists of hololeucocratic to leucocratic rocks ranging from pinky to pinky-gray. They are isotropic, ranging from equigranular to inequigranular grains, sometimes porphyritic and pegmatitic, classified as muscovite-biotite monzo to syenogranites. Sometimes they present garnet and monazite as primary accessory minerals. These features characterize them as S-type granites or Muscovite bearing Peraluminous Granitoides (MPG). The rocks contain high silica content, which characterizes them as very evolved, formed by high-K to shoshonitic, peraluminous, and ferrous calc-alkaline magmatism. A U-Pb age of 928 ± 5 Ma was obtained for one of the analyzed rocks, which agrees with previous U-Pb ages obtained for this granite. Sm-Nd analysis indicates a TDM model age of 1.58 Ga, and negative ND value (-2.90). These results demonstrate that the São Domingos intrusion corresponds to a post tectonic environment, related to the Sunsás orogeny, whose magmatic origin is associated to re-working of the ancient continental crust. Moreover, three different ETR patterns were found for these lithotipes, suggesting the generation of contemporaneous non-cogenetic magmas, involving distinct crustal sources.
Poitrasson, Franck. "Apports du système radiométrique Samarium-Néodyme à la connaissance du magnétisme anorogénique intracontinental. Exemple du sud-est de la France (Corse et Estérel)." Clermont-Ferrand 2, 1994. http://www.theses.fr/1994CLF21601.
Повний текст джерелаPopoff, Michel. "Déformation intracontinentale Gondwanienne : rifting mézoique en Afrique : évolution meso-cénozoique du fossé de la Bénoué, Nigéria : relations avec l'ouverture de l'Océan Atlantique Sud." Aix-Marseille 3, 1990. http://www.theses.fr/1990AIX3A002.
Повний текст джерелаКниги з теми "Intracontinental magmatism"
Armando, Giovanni. Intracontinental alkaline magmatism: Geology, petrography, mineralogy and geochemistry of the Jebel Hayim Massif (Central High Atlas - Morocco). Lausanne, Suisse: Université de Lausanne, 1999.
Знайти повний текст джерелаЧастини книг з теми "Intracontinental magmatism"
Sawkins, Frederick J. "Intracontinental Hotspots, Anorogenic Magmatism, and Associated Metal Deposits." In Metal Deposits in Relation to Plate Tectonics, 239–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-662-08681-0_7.
Повний текст джерелаPirajno, Franco. "Intracontinental Magmatism, Anorogenic Metamorphism, Ore Systems and Mantle Plumes." In Ore Deposits and Mantle Plumes, 291–321. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-2502-6_6.
Повний текст джерелаIzokh, A. E., G. S. Fedoseev, and V. A. Kutolin. "Late Cretaceous Intracontinental Alkaline-Basaltoid Magmatism of the Chebakovo-Balakhta Depression." In Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin, 215–32. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29559-2_9.
Повний текст джерелаPirajno, Franco. "Oceanic Islands, Large Igneous Provinces, Mafic Dyke Swarms, and Intracontinental Alkaline Magmatism." In Ore Deposits and Mantle Plumes, 111–214. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-2502-6_3.
Повний текст джерелаMacdonald, Francis A., W. Adolph Yonkee, Rebecca M. Flowers, and Nicholas L. Swanson-Hysell. "Neoproterozoic of Laurentia." In Laurentia: Turning Points in the Evolution of a Continent. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.1220(19).
Повний текст джерелаRogers, John J. W., and M. Santosh. "History of Continents after Rifting from Pangea." In Continents and Supercontinents. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195165890.003.0012.
Повний текст джерелаSharman, Glenn R., Daniel F. Stockli, Peter Flaig, Robert G. Raynolds, Marieke Dechesne, and Jacob A. Covault. "Tectonic influence on axial-transverse sediment routing in the Denver Basin." In Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma). Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2555(11).
Повний текст джерелаТези доповідей конференцій з теми "Intracontinental magmatism"
Wang, Yu, Songnan LIU, and Liyun Zhou. "TECTONIC STRESS TRANSMISSION FROM MARGIN TO INTERIORS: RESPONSIBILITY FOR INTRACONTINENTAL DEFORMATION, MAGMATISM AND SEDIMENTATION." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-366225.
Повний текст джерелаClinkscales, Christopher Andrew, and Paul Kapp. "JURASSIC TO CRETACEOUS INTRACONTINENTAL SHORTENING AND MAGMATISM IN NORTH CHINA: EVIDENCE FOR FLAT-SLAB SUBDUCTION OF THE IZANAGI PLATE." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336397.
Повний текст джерела