Relevant bibliographies by topics / Granitoïdes Granit

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Granitoïdes Granit'

Author: Grafiati
Published: 4 June 2021
Last updated: 9 February 2022

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Journal articles on the topic "Granitoïdes Granit"

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Usman, Ediar. "THE GEOCHEMICAL CHARACTERISTIC OF MAJOR ELEMENT OF GRANITOID OF NATUNA, SINGKEP, BANGKA AND SIBOLGA." BULLETIN OF THE MARINE GEOLOGY 30, no. 1 (2016): 45. http://dx.doi.org/10.32693/bomg.30.1.2015.74.

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A study of geochemical characteristic of major elelemnt of granitoid in Western Indonesia Region was carried out at Natuna, Bangka, Singkep and Sibolga. The SiO2 contents of the granites are 71.16 to 73.02 wt%, 71.77 to 75.56wt% and 71.16 to 73.02wt% at Natuna, Bangka, and Singkep respectively, which are classified as acid magma. While in Sibolga the SiO2 content from 60.27 to 71.44wt%, which is classified as intermediate to acid magma. Based on Harker Diagram, the granites from Natuna, Bangka and Singkep as a co-genetic. In other hand the Sibolga Granite show as a scatter pattern. Granites of
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Naibaho, Tommy, and Lukman Arifin. "VERIFIKASI LITOLOGI TERHADAP NILAI KERENTANAN MAGNETIK DI PERAIRAN BANGKA BELITUNG." JURNAL GEOLOGI KELAUTAN 8, no. 1 (2016): 37. http://dx.doi.org/10.32693/jgk.8.1.2010.184.

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Peta anomali magnetik menunjukkan bahwa perairan Bangka Belitung dicirikan oleh pasangan tinggian dan rendahan panjang gelombang anomali dengan amplitudo -200 nT—500nT. Sedangkan dari peta distribusi kerentanan magnetik, tinggian magnetik Belitung dibatasi oleh nilai kerentanan magnetik antara 0,001 cgs unit dan 0,003 cgs unit. Anomali positip rendah dicirikan oleh nilai kerentanan magnetik batuan antara 0,001-0,003 cgs unit merupakan benda intrusif bawah laut yang diduga berupa pluton granitik jenis granit-biotit yang berasosiasi dengan mineral kasiterit. Pluton granitik tersebut sama seper
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Sevigny, J. H., and R. R. Parrish. "Age and origin of Late Jurassic and Paleocene granitoids, Nelson Batholith, southern British Columbia." Canadian Journal of Earth Sciences 30, no. 12 (1993): 2305–14. http://dx.doi.org/10.1139/e93-200.

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In the Middle Jurassic Nelson Batholith, southern British Columbia, young 40Ar/39Ar ages (i.e., 50–60 Ma) and distorted isobaric surfaces in the batholith suggest the possibility of Paleocene granitic plutonism. We present the results of a study undertaken to evaluate this possibility. Geochemical criteria successfully distinguish a suite of granitoids within the Nelson Batholith that differ from Nelson granites of similar SiO2 content. The granitoid suite is composed of 71.6–75.7 wt.% SiO2 leucocratic biotite granite and quartz monzonite with strong enrichments in alkaline, alkaline earth, an
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Stepanyuk, L., О. Hrinchenko, T. Dovbush, O. Ziultsle, N. Konoval, and T. Mironchuk. "AGE SPAN FORMATION IN GRANITOIDS OF UKRAINIAN SHIELD." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (88) (2020): 12–16. http://dx.doi.org/10.17721/1728-2713.88.02.

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The paper discusses Berdychiv type granitoids that have always stirred up interest among researchers of the Ukrainian Shield. These rocks include minerals that are uncharacteristic of granites - cordierite, sillimanite, andalusite - and are closely related to rocks of the supposed substratum. At the same time, there still remain questions about the genetic nature of Berdychiv granites. Despite the fact that most researchers treat these granites as intrusive (anatectic) formations, there are other concepts according to which these granites are considered to be the products of metasomatic transf
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Vapnik, Ye. "Melt inclusions in granitoids of the Timna Igneous Complex, Southern Israel." Mineralogical Magazine 62, no. 1 (1998): 29–40. http://dx.doi.org/10.1180/002646198547440.

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AbstractHigh temperature microthermometry and Scanning Electron Microprobe (SEM) analyses were used to study natural magmatic remnants in quartz crystals in granitoids from the Timna Igneous Complex, southern Israel, and to constrain physicochemical parameters during their crystallization. For the porphyritic granite, alkali granite and quartz monzodiorite, liquidus temperatures are 710–770, 770–830 and 770–840°C, respectively; solidus temperatures are 690–770, 710–790 and 770°C, respectively. Pressures during crystallization and water content in the magmas were determined using the phase diag
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Mamtani, Manish A., Sandeep Bhatt, Virendra Rana, Koushik Sen, and Tridib K. Mondal. "Application of anisotropy of magnetic susceptibility (AMS) in understanding regional deformation, fabric development and granite emplacement: examples from Indian cratons." Geological Society, London, Special Publications 489, no. 1 (2019): 275–92. http://dx.doi.org/10.1144/sp489-2019-292.

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AbstractIn this paper the authors review various applications of analysing fabric in granites from Indian cratons using anisotropy of magnetic susceptibility (AMS). First the general importance of AMS in identifying the internal fabric in massive granitoids devoid of visible foliations/lineations is highlighted. Subsequently, three important applications of AMS in granitoids are discussed. (a) The case of Godhra Granite (southern parts of the Aravalli Mountain Belt) is presented as an example of the robustness of AMS in working out the time relationship between emplacement/fabric development a
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Sandeman, Hamish A., and John Malpas. "Epizonal I- and A-type granites and associated ash-flow tuffs, Fogo Island, northeast Newfoundland." Canadian Journal of Earth Sciences 32, no. 11 (1995): 1835–44. http://dx.doi.org/10.1139/e95-141.

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Magmatic activity of Silurian–Devonian age is widespread in the Appalachian–Caledonian Orogen. A marked characteristic of this magmatism is the composite nature of the igneous suites, which range from peridotite to granodiorite in single plutonic bodies. The origin of these suites is still enigmatic, and the assumption that all are the same not proven. Such a suite of intrusive rocks, ranging in composition from minor peridotite to granodiorite, intrudes an openly folded sequence of Silurian volcanogenic sandstones and ash-flow tuffs on Fogo Island, northeast Newfoundland. Two units, the Roger
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Mughal, Muhammad Saleem, Chengjun Zhang, Amjad Hussain, et al. "Petrogenesis and Geochronology of Tianshui Granites from Western Qinling Orogen, Central China: Implications for Caledonian and Indosinian Orogenies on the Asian Plate." Minerals 10, no. 6 (2020): 515. http://dx.doi.org/10.3390/min10060515.

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The precise timing, petrogenesis, and geodynamic significance of three granitoid bodies (Beidao granite, Caochuanpu granite, Yuanlongzhen granite, and the Roche type rock) of the Tianshui area in the Western Qinling Orogen, central China, are poorly constrained. We performed an integrated study of petrology, geochemistry, and zircon U-Pb dating to constrain their genesis and tectonic implication. Petrographic investigation of the granites shows that the rocks are mainly monzogranites. The Al saturation index (A/CNK versus SiO2) of the granitoid samples indicates meta-aluminous to peraluminous
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Broska, Igor, and Igor Petrík. "Variscan thrusting in I- and S-type granitic rocks of the Tribeč Mountains, Western Carpathians (Slovakia): evidence from mineral compositions and monazite dating." Geologica Carpathica 66, no. 6 (2015): 455–71. http://dx.doi.org/10.1515/geoca-2015-0038.

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AbstractThe Tribeč granitic core (Tatric Superunit, Western Carpathians, Slovakia) is formed by Devonian/Lower Carboniferous, calc-alkaline I- and S-type granitic rocks and their altered equivalents, which provide a rare opportunity to study the Variscan magmatic, post-magmatic and tectonic evolution. The calculatedP-T-Xpath of I-type granitic rocks, based on Fe-Ti oxides, hornblende, titanite and mica-bearing equilibria, illustrates changes in redox evolution. There is a transition from magmatic stage atTca. 800–850 °C and moderate oxygen fugacity (FMQ buffer) to an oxidation event at 600 °C
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Wilton, Derek H. C. "Tectonic evolution of southwestern Newfoundland as indicated by granitoid petrogenesis." Canadian Journal of Earth Sciences 22, no. 7 (1985): 1080–92. http://dx.doi.org/10.1139/e85-110.

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Four granitoid suites are recognized in the region of the Cape Ray Fault Zone of southwestern Newfoundland. The two oldest (Ordovician–Silurian (?)) suites represent partial melts of their enclosing host rocks. The Port aux Basques granite is modelled as a partial melt of the gneissic component of its host, Port aux Basques Complex. The Cape Ray granite forms a dominantly tonalitic terrane derived by partial melting of ophiolitic material. The Red Rocks granite and a megacrystic phase of the Cape Ray granite form coherent lines of geochemical descent from the parental tonalite but show evidenc
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Dissertations / Theses on the topic "Granitoïdes Granit"

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Foster, Pedro Luiz Luppi [UNESP]. "Geologia e petrologia do Maciço Palanqueta, Mina Bom Futuro, Rondônia." Universidade Estadual Paulista (UNESP), 2016. http://hdl.handle.net/11449/144675.

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Submitted by PEDRO LUIZ LUPPI FOSTER null (luppifoster@gmail.com) on 2016-11-16T19:23:57Z No. of bitstreams: 1 Tese_Mestrado_Pedro_Foster.pdf: 23543008 bytes, checksum: 970cd8b58cfa88e2188ef3b76510d096 (MD5)<br>Approved for entry into archive by Felipe Augusto Arakaki (arakaki@reitoria.unesp.br) on 2016-11-23T12:41:25Z (GMT) No. of bitstreams: 1 foster_pll_me_rcla.pdf: 23543008 bytes, checksum: 970cd8b58cfa88e2188ef3b76510d096 (MD5)<br>Made available in DSpace on 2016-11-23T12:41:25Z (GMT). No. of bitstreams: 1 foster_pll_me_rcla.pdf: 23543008 bytes, checksum: 970cd8b58cfa88e2188ef3b76510d
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Henrique-Pinto, Renato. "Metaconglomerados e rochas associadas do Grupo São Roque a noroeste da cidade de São Paulo: proveniência e implicações para a idade da sedimentação." Universidade de São Paulo, 2008. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-11112008-115527/.

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O Grupo São Roque caracteriza-se por rochas de baixo grau metamórfico, depositadas em ambiente marinho com atividade vulcânica submarina. As ocorrências da Formação Morro Doce são dominadas por metarcóseos e metarenitos feldspáticos com expressivas lentes metaconglomeráticas, que formam uma seqüência considerada como unidade basal do Grupo São Roque. Os metaconglomerados, com o amplo predomínio de clastos graníticos, têm excelente potencial para identificação de suas fontes e idades. Rochas metavulcânicas ácidas e básicas intercaladas nesta seqüência constituem importante marcador tectônico e
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SILVA, Mickey Anderson Paixão da. "Influência das características morfológicas de britas graníticas e gnaíssicas na resistência à compressão do concreto." Universidade Federal de Pernambuco, 2016. https://repositorio.ufpe.br/handle/123456789/18425.

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Submitted by Irene Nascimento (irene.kessia@ufpe.br) on 2017-03-23T18:49:28Z No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Dissertação Mickey Paixão.pdf: 4062224 bytes, checksum: 47b4af597c13bbbf32f479aa0e076a4a (MD5)<br>Made available in DSpace on 2017-03-23T18:49:28Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Dissertação Mickey Paixão.pdf: 4062224 bytes, checksum: 47b4af597c13bbbf32f479aa0e076a4a (MD5) Previous issue date: 2016-08-09<br>Em virtude dos agregados constituírem os
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Yang, Wenjin. "Géochimie et minéralogie des granites de la région de Hetai, province de Guangdong, Chine méridionale = Geochemistry and mineralogy of granites in the Hetai area, Guangdong, South China /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1993. http://theses.uqac.ca.

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Thèse (D.R.Min.)-- Université du Québec à Chicoutimi, 1993.<br>Thèse presentee en collaboration de l'Université du Quebec à Chicoutimi et Institute of geochemistry, Academia Sinica, China. CaQCU Document électronique également accessible en format PDF. CaQCU
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Prado, Maurício. "O Granito europa e o grupo Iricoumé na parte leste do distrito mineiro de Pitinga (Amazonas)." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2006. http://hdl.handle.net/10183/8522.

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O granito Europa intrude rochas do Grupo Iricoumé, que é constituído predominantemente por rochas vulcanoclásticas de ambiente subaéreo (ignimbritos ricos em cristais, tufos maciços finos e arenitos sílticos tufáceos) e, subordinadamente, por riolitos hipabissais com composições equivalentes a sienogranitos, provavelmente geradas em ambiente do tipo caldeira. O granito Europa é um pertita granito (hipersolvus) de natureza peralcalina, não têm relação genética com as rochas vulcânicas do Grupo Iricoumé, mas pode ter sido originado em estágios de ressurgência. Dados petrográficos e geoquímicos a
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Mello, Roberta Monteiro de. "Utilização do resíduo proveniente do acabamento e manufatura de mármores e granitos como matéria-prima em cerâmica vermelha." Universidade de São Paulo, 2006. http://www.teses.usp.br/teses/disponiveis/85/85134/tde-04062007-164950/.

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A utilização da lama residual de marmoraria em cerâmica vermelha foi colocada em prática visando à diminuição do impacto ambiental, causado tanto pelo descarte da lama como também pela quantidade de argila extraída no setor cerâmico. Foram coletadas amostras em 12 marmorarias localizadas na Grande São Paulo. No entanto, apenas as amostras de quatro foram selecionadas para serem incorporadas, levando em consideração suas características distintas. O argilito foi a matéria-prima escolhida para confecção da massa padrão de cerâmica vermelha, devido à sua grande utilização no setor. Tanto as amost
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England, Richard W. "The ascent and emplacement of granitic magma : the Northern Arran granite." Thesis, Durham University, 1988. http://etheses.dur.ac.uk/6609/.

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This thesis is a study of the mechanisms by which granitic magmas rise through the crust to be empiaced at a level above their source, with particular reference to diapirisni. and how these mechanisms may be analysed by combined structural and petrological studies. The Northern Arran granite is used as an example of how this problem may be approached. The Northern Arran granite is a two component granite of Tertiary age intruded into structurally heterogeneous upper crustal rocks under regional tension. A synform concentric to the granite, synchronous with the development of a narrow thermal a
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Villaros, Arnaud. "Petrogenesis of S-type granites : the example of the Cape Granite Suite." Thesis, Stellenbosch : University of Stellenbosch, 2010. http://hdl.handle.net/10019.1/4015.

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Thesis (PhD (Earth Sciences))--University of Stellenbosch, 2010.<br>ENGLISH SUMMARY: S-type granite intrusions are extremely common in the continental crust and form from the partial melting of metasediments. Compositions of S-type granite range from leucogranite to granodiorite and have trace element contents that globally increase with increasing maficity (Fe + Mg). Models proposed for the formation of S-type granite do not answer satisfactorily all petrological and compositional requirements. In this study, S-type granite of the Cape Granite Suite (CGS), South Africa is used to discri
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Oukemeni, Driss. "Géochimie, géochronologie (U-Pb) du pluton d'Aouli et comparaisons géochimiques avec d'autres granitoïdes hercyniens du Maroc par analyse discriminante /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1993. http://theses.uqac.ca.

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Caltabeloti, Fabrizio Prior. "Alojamento e deformação de plútons graníticos da extremidade nordeste da Suíte Intrusiva Cunhaporanga (Domínio Apiaí - Faixa Ribeira, PR)." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-16082011-170032/.

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Plútons graníticos (Patrimônio Santo Antônio, São Domingos, Ouro Verde e Santa Rita) alojados na porção nordeste da Suíte Intrusiva Cunhaporanga (c. 620-590 Ma) intrudiram metassedimentos pelíticos e carbonáticos de baixo grau metamórfico do Grupo Itaiacoca. Os plútons são isótropos, de coloração cinza a rósea e composição monzo- a sienogranítica, predominando granitóides porfiríticos grossos e, secundariamente, tipos inequigranulares a equigranulares. A cartografia regional mostrou que a foliação das rochas metassedimentares encaixantes mergulha dominantemente para NE e contém uma lineação (i
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Books on the topic "Granitoïdes Granit"

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St. George Red Granite Co. The act of incorporation and the by-laws of the St. George Red Granite Co. (Limited). s.n.], 1986.

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Jørgensen, Børge. Børge Jørgensen: Fra granit til stål = Børge Jørgensen : from granite to steel. Asbæk, 1986.

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Minkowski, Aleksander. Czarny granit. Siedmioróg, 1995.

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Clarke, D. Barrie. Granitoid rocks. Chapman & Hall, 1992.

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Bergeron, Michel. Granite industry in Canada : 1993 directory =: L'industrie du granite au Canada : répertoire de 1993. Natural Resources Canada = Ressources naturelles Canada, 1993.

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Mitchell, James Leslie. Grey granite. Canongate Pub., 1990.

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Archer, Michael. Granite sculpture. Nottingham Castle Museum, 1990.

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ill, Hawkes Kevin, ed. Granite baby. Farrar, Straus and Giroux, 2005.

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Mitchell, James Leslie. Grey granite. Canongate Classics, 1990.

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Moroles, Jesús Bautista. Granite sculpture. Simms Fine Arts, 1988.

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Book chapters on the topic "Granitoïdes Granit"

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von Engelhardt, Wolf. "Granit." In Goethe im Gespräch mit der Erde. J.B. Metzler, 2003. http://dx.doi.org/10.1007/978-3-476-02940-9_8.

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Arndt, Nicholas. "Granite." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_665.

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Arndt, Nicholas. "Granite." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_665-3.

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Arndt, Nicholas. "Granite." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_665.

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Stevenson, David S. "Our Island Earth: Granite Here, Granite Everywhere?" In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_7.

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Stevenson, David S. "Our Planet’s Torrid Heart." In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_1.

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Stevenson, David S. "The Formation of Granites & Plate Tectonics." In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_2.

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Stevenson, David S. "The Evolution of Modern Continents." In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_3.

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Stevenson, David S. "Plate Tectonics, Planetary Magnetism and Life." In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_4.

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Stevenson, David S. "Jotunheim –In the Realm of Giants." In Granite Skyscrapers. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_5.

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Conference papers on the topic "Granitoïdes Granit"

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Mouroux, B., T. Merceron, D. Vilogeux, and J. de Me`redieu. "The Disposal of HLLL Waste in a Granitic Formation: The Status of Research in France." In ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4818.

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In accordance with the French Law of 1991 December 30, Andra is preparing a report on the possibilities of geological disposal to be submitted in 2005. For that purpose, a research programme has been launched to assess the suitability of granite geological formations for the implementation of a high-level long-lived radioactive waste repository. The programme relies mainly on Andra’s participation in experiments in Swedish, Swiss and Canadian underground research laboratories. The main issues under investigation include granite fracturing and the behaviour of engineered barriers. Furthermore,
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Stevenson, Alexandria M., and Jonathan D. Price. "ANOMALOUS GRANITES WITHIN THE QUANAH GRANITE PLUTON, WICHITA MOUNTAINS, OKLAHOMA." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343875.

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Makovsky, Kyle A., Scott Samson, and Dave Moecher. "GRENVILLE GRANITOIDS IN THE SOUTHERN APPALACHIANS – FURTHER EVIDENCE OF THE “HOT” GRANITE HYPOTHESIS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321790.

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Arbain, Azizi, Mohd Hafiz Zawawi, Mohd Rashid Mohd Radzi, Nurul Husna Hassan, and Ahmad Zhafran Ahmad Mazlan. "Natural frequencies comparison between the pure granite and bonded granite-concrete." In PROCEEDINGS OF GREEN DESIGN AND MANUFACTURE 2020. AIP Publishing, 2021. http://dx.doi.org/10.1063/5.0044239.

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Price, Jonathan D. "OF GRANOPHYRE AND GRAINS: MICROSTRUCTURE VARIATION IN THE WICHITA GRANITE GROUP, OKLAHOMA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338820.

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Newcomb, Sally. "THE CONTROVERSIAL GRANITE CONTROVERSY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334628.

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Rebreyend, Dominique. "The GRANIT project: status and perspectives." In XXIst International Europhysics Conference on High Energy Physics. Sissa Medialab, 2012. http://dx.doi.org/10.22323/1.134.0072.

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Hassan, Diyar. "Bir Kilin Atık Granit Kırığıyla İyileştirilmesi." In 6. Geotechnical Symposium. LookUs Scientific, 2016. http://dx.doi.org/10.5505/2015geoteknik.s065.

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René, Miloš. "Nb-Ta-Ti oxides in topaz granites of the Geyer granite stock (Erzgebirge Mts., Germany)." In The 1st International Electronic Conference on Mineral Science. MDPI, 2018. http://dx.doi.org/10.3390/iecms2018-05448.

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"Analiz vzaimodeystviya dislokatsiy i granits zeren v medi v zavisimosti ot razorientirovok i tipa granitsy." In Perspektivnye materialy s ierarkhicheskoy strukturoy dlya novykh tekhnologiy i nadezhnykh konstruktsiy, Khimiya nefti i gaza. Tomsk State University, 2018. http://dx.doi.org/10.17223/9785946217408/131.

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Reports on the topic "Granitoïdes Granit"

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Petkovic, Peter. Gravity and granites : technical notes on mapping relationships of known granites and gravity. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.012.

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Burns, L. E., K. J. Johnson, and R. J. Newberry. Discriminant function for separating tin from non-tin granites: application to the Hope Granite Suite, eastern interior Alaska. Alaska Division of Geological & Geophysical Surveys, 1988. http://dx.doi.org/10.14509/1361.

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Susskind, Lawrence E., Susan L. Podziba, and Eileen Babbitt. Granite Construction Co. Defense Technical Information Center, 1989. http://dx.doi.org/10.21236/ada225177.

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Sinclair, W. D. Granitic pegmatites. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/208026.

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Swaja, R. E., and W. D. Cottrell. Results of the radiological survey at the Granite City Steel facility, Granite City, Illinois. Office of Scientific and Technical Information (OSTI), 1990. http://dx.doi.org/10.2172/6605990.

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Buettner, Edwin W., and V. Lance Nelson. Smolt Monitoring at the Head of Granite Reservoir and Lower Granite Dam, 1989 Annual Report. Office of Scientific and Technical Information (OSTI), 1990. http://dx.doi.org/10.2172/6854896.

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Bedrossian, P. Neutrons and Granite: Transport and Activation. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/15009828.

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Jackson, L. E. Surficial geology, Granite Canyon, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208953.

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Buettner, Edwin W., and Arnold F. Brimmer. Smolt Monitoring at the Head of Lower Granite Reservoir and Lower Granite Dam, 1995 Annual Report. Office of Scientific and Technical Information (OSTI), 1996. http://dx.doi.org/10.2172/441714.

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Brimmer, Arnold F. Smolt Monitoring at the Head of Lower Granite Reservoir and Lower Granite Dam, 1996 Annual Report. Office of Scientific and Technical Information (OSTI), 1998. http://dx.doi.org/10.2172/14907.

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