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Relevant bibliographies by topics / Greenstone belt

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Academic literature on the topic 'Greenstone belt'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 January 2023

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Journal articles on the topic "Greenstone belt"

1

St. Seymour, Karen, Andrew Turek, Ronald Doig, Stephen Kumarapeli, and Robert Fogal. "First U–Pb zircon ages of granitoid plutons from the La Grande greenstone belt, James Bay area, New Quebec." Canadian Journal of Earth Sciences 26, no. 5 (1989): 1068–73. http://dx.doi.org/10.1139/e89-088.

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Zircon ages from three granitoid plutons are the first to be reported from the La Grande greenstone belt. Two of the dated samples are from highly tectonized, early tectonic plutons that at the present level of erosion are just outside the greenstone belt proper. Their zircon ages of ca. 2740 Ma are emplacement ages or alternatively represent the age of maximum deformation of the greenstone belt. The third sample is from a mildly deformed late tectonic pluton within the greenstone belt. Its zircon age of ca. 2670 Ma probably represents the emplacement age. The above dates and the relationships

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Kozlov, N. E., N. O. Sorokhtin, N. E. Kozlova, and Eu V. Martynov. "Geological structure of the Ustoyarvi region (North-Western part of the Russian Arctic)." Vestnik MGTU 25, no. 1 (2022): 12–26. http://dx.doi.org/10.21443/1560-9278-2022-25-1-12-26.

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The paper presents data on geology and composition of rocks from the Ustoyarvi region (the North-Western Arctic zone of Russian Federation). Their compositional analysis (including mathematical evaluation of the similarity/difference measure) provided much reliable conclusion that the rocks from this area, which are presumably attributed to the Ustoyarvi structure (Ustoyarvinsky Greenstone Belt) were similar to those from the Ura-Guba area in the Kolmozero-Voronya Belt and continued it. In addition, it has been shown that from west to east lithotectonic units in the adjacent (Suormussky) Block

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Benn, Keith, Edward W. Sawyer, and Jean-Luc Bouchez. "Orogen parallel and transverse shearing in the Opatica belt, Quebec: implications for the structure of the Abitibi Subprovince." Canadian Journal of Earth Sciences 29, no. 11 (1992): 2429–44. http://dx.doi.org/10.1139/e92-191.

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The late Archean Opatica granitoid-gneiss belt is situated within the northern Abitibi Subprovince, along the northern margin of the Abitibi greenstone belt. Approximately 200 km of structural section was mapped along three traverses within the previously unstudied Opatica belt. The earliest preserved structures are penetrative foliations and stretching and mineral lineations recording regional ductile shearing (D1). Late-D1 deformation was concentrated into kilometre-scale ductile fault zones, typically with L > S tectonite fabrics. Two families of lineations are associated with D1, indica

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Lodge, Robert W. D., Harold L. Gibson, Greg M. Stott, James M. Franklin, and George J. Hudak. "Geodynamic setting, crustal architecture, and VMS metallogeny of ca. 2720 Ma greenstone belt assemblages of the northern Wawa subprovince, Superior Province." Canadian Journal of Earth Sciences 52, no. 3 (2015): 196–214. http://dx.doi.org/10.1139/cjes-2014-0163.

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The greenstone belts along the northern margin of the Wawa subprovince of the Superior Province (Vermilion, Shebandowan, Winston Lake, Manitouwadge) formed at ca. 2720 Ma and have been interpreted to be representative of a rifted-arc to back-arc tectonic setting. Despite a common inferred tectonic setting and broad similarities, these greenstone belts have a significantly different metallogeny as evidenced by different endowments in volcanogenic massive sulphide (VMS), magmatic sulphide, and orogenic gold deposits. In this paper, we examine differences in geodynamic setting and crustal archite

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Anhaeusser, C. R. "The geology and tectonic evolution of the northwest part of the Barberton Greenstone Belt, South Africa: A review." South African Journal of Geology 122, no. 4 (2019): 421–54. http://dx.doi.org/10.25131/sajg.122.0033.

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AbstractFormations on the northwestern flank of the Barberton Greenstone Belt have hosted over 85% of all the gold recovered from the ca. 3550 to 3000 Ma Barberton Supergroup since early discoveries in 1872. This sector of the greenstone belt also happens to coincide with a complex tectonic architecture resulting from successive stages of folding and faulting superimposed onto a complex lithostratigraphy. Of particular importance has been the influence of two diapiric granitoid intrusions that caused added structural complexity following their emplacement ca. 3227 to 3250 Ma. Of these the larg

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Pouclet, André, Siaka Doumbia, and Max Vidal. "Geodynamic setting of the Birimian volcanism in central Ivory Coast (western Africa) and its place in the Palaeoproterozoic evolution of the Man Shield." Bulletin de la Société Géologique de France 177, no. 2 (2006): 105–21. http://dx.doi.org/10.2113/gssgfbull.177.2.105.

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Abstract Palaeoproterozoic volcanic formations having different geochemical features are described in the Katiola-Marabadiassa area (Central Ivory Coast). They consist of (i) metamorphic mafic rocks belonging to the greenstone belts, (ii) rhyodacites intruded into the greenstone belts and interpreted as sub-volcanic apophyses of TTG plutons, and (iii) calc-alkaline andesitic lava interbedded in the lower sedimentary pile of the Bandama Basin. The greenstone belt rocks have a magmatic signature of ocean floor tholeiites. They were generated from moderate partial melting of a fairly depleted spi

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Dostal, J., C. Dupuy, and J. L. Poidevin. "Geochemistry of Precambrian basaltic rocks from the Central African Republic (Equatorial Africa)." Canadian Journal of Earth Sciences 22, no. 5 (1985): 653–62. http://dx.doi.org/10.1139/e85-072.

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The two Archaean greenstone belts (Bandas and Bogoin) in the Central African Republic (Equatorial Africa) are 250 and 150 km long. The metavolcanic rocks in the belts are predominantly komatiitic and tholeiitic basalts. Komatiites include both Al-depleted and Al-undepleted types. The komatiites and light-REE-depleted tholeiites were probably derived from a similar upper mantle source. However, the tholeiitic basalts enriched in light REE from the upper volcanic strata of the Bandas belt were generated from a different source. The dolerites from Proterozoic dyke swarms and sills differ from the

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Phillips, G. Neil, David I. Groves, and Isobel J. Brown. "Source requirements for the Golden Mile, Kalgoorlie: significance to the metamorphic replacement model for Archean gold deposits." Canadian Journal of Earth Sciences 24, no. 8 (1987): 1643–51. http://dx.doi.org/10.1139/e87-158.

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The Golden Mile at Kalgoorlie represents a giant Archean hydrothermal gold system localized by ductile shear zones and hosted mainly by a differentiated tholeiitic sill. Chlorite, carbonate, and pyrite alteration zones cover the whole mineralized area (1 km × 3 km), and calculations suggest that for the Golden Mile (production around 1200 t Au), the amounts of components added to these alteration zones are 340 Mt CO2, 20 Mt K, and 5 Mt S. If one adopts a metamorphic-replacement model for gold mineralization in which all ore components derive from devolatilization of greenstones at amphibolite

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EVINS, P. M., and K. LAAJOKI. "Early Proterozoic nappe formation: an example from Sodankylä, Finland, Northern Baltic Shield." Geological Magazine 139, no. 1 (2002): 73–87. http://dx.doi.org/10.1017/s0016756801006094.

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The Central Lapland Greenstone belt comprises rift-related metavolcanic and metasedimentary rocks representing one of the largest supracrustal belts in the Baltic Shield. The Sodankylä area in the central part of the belt represents a complex thrust duplex within a nappe overlying Belomorian Archaean basement and autocthonous Luirojoki calc-silicate rocks. Here, an early D1 schistosity is axial planar to at least three coaxial generations of southward-verging, subhorizontal, E–W-plunging D1 folds associated with major southwards thrusting. D2 is represented by broad, map-scale, upright, NE-tre

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Inza, Coulibaly, Kouamelan Alain Nicaise, Djro Sagbrou Chérubin, and Coulibaly Yacouba. "Petrographie Des Volcanites Et Plutonites De La Partie Sud Du Sillon Volcano-Sedimentaire De Toumodi-Fetekro (Cote D’ivoire)." European Scientific Journal, ESJ 13, no. 30 (2017): 199. http://dx.doi.org/10.19044/esj.2017.v13n30p199.

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The southern part of Toumodi-Fètêkro greenstone belt is located in the Center - Southeast of Ivory Coast. Petrographic study of volcanic and plutonic rocks shows three units. The first unit is composed of basaltic to rhyolitic lavas which imply effusive character. Then we have volcanosedimentary unit composed of pyroclastic formations (lapilli tuff, breccia, ash deposit and ignimbrites) and the pillow-lavas. Indeed, the presence of this last shows clearly that an explosive volcanism and a submarine effusive volcanism have occurred during during the setting of Toumodi-Fètêkro belt. Plutonic uni

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Dissertations / Theses on the topic "Greenstone belt"

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Silva, Katherine E. "Komatiites from the Belingwe Greenstone Belt, Zimbabwe : constraints on the development of Archaean Greenstone Belts." Thesis, Royal Holloway, University of London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.263522.

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Brake, Chris. "Tholeiitic magmatism in the Belingwe greenstone belt, Zimbabwe." Thesis, University of Edinburgh, 1996. http://hdl.handle.net/1842/12669.

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The Belingwe greenstone belt in southern Zimbabwe contains one of the most well preserved Archean volcanic successions in the world. The komatiites in this succession have been studied in great detail, but the associated basalts have received much less attention. A detailed study of these basalts in the Zeederbergs Formation has revealed the existence of a previously unrecognised lava type which has important implications for the petrogenesis of the suite. The Zeederbergs Formation and the underlying Reliance Formation form the 2.7 Ga Ngezi Group volcanics, which are underlain by thin, general

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Hunter, Morag. "The tectonic setting of the Belingwe Greenstone Belt, Zimbabwe." Thesis, University of Cambridge, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.245104.

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Diergaardt, Byron Nico. "Rhyolitic volcanism in the Onverwacht Group, Barberton Greenstone Belt." Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/80255.

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Thesis (MSc)--Stellenbosch University, 2013.<br>ENGLISH ABSTRACT: The source of the K2O in the K2O-rich ~3.45 Ga felsic intrusive rocks of the H6 unit in the Hooggenoeg Formation of the Onverwacht Group in the Barberton Granite Greenstone Terrain (BGGT) is examined in this study. This is of particular research interest because the Paleoarchaean rock record is considered to lack K2O-rich magmatic rocks. Previous studies on the felsic igneous rocks of the H6 unit have proposed that these rhyolites are K-metasomatised eruptive equivalents of the sodium-rich ~3.45 Ga TTGs of the BGGT and that the

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Dai, Tianhuan. "Kinematics and deformation history of the Cross Lake Greenstone Belt." College Park, Md. : University of Maryland, 2004. http://hdl.handle.net/1903/2162.

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Thesis (M.S.) -- University of Maryland, College Park, 2004.<br>Thesis research directed by: Dept. of Geology. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.

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Lafleur, Pierre Jean. "The Archean Round Lake Batholith, Abitibi Greenstone Belt a synthesis." Thesis, University of Ottawa (Canada), 1986. http://hdl.handle.net/10393/5049.

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Jurkowski, Jacek. "U-Pb geochronology study of Lynn Lake greenstone belt, Manitoba." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0011/MQ52583.pdf.

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Chiarini, Alexandre Patricio. "Geologia da porção basal do \"Greenstone Belt\" de Piumhi-MG." Universidade de São Paulo, 2001. http://www.teses.usp.br/teses/disponiveis/44/44135/tde-16072015-101156/.

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A porção da seqüência metavulcano-sediemntar (SVS) de Piumhi enfocada neste trabalho representa a parte basal de um greestone belt arqueano a paleoproterozóico, e foi estudada em seus aspectos estruturais, petrográficos, geoquímicos e metalogenéticos. A análise estrutural propiciou uma melhor compreensão da evolução tectônica geométrica/estratigráfica, e da cinemática interna da SVS, e da relação com as outras unidades precambrianas justapostas em contato direto. A SVS ocorre cavalgando o corpo granítico TTG a norte, em zonas de cisalhamento com forte milonitização junto ao contato. Este conju

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Hamman, Jurgens Petrus Eden. "Geotechnical assessment of a kimberlite pipe in Greenstone belt granites." Diss., University of Pretoria, 2008. http://hdl.handle.net/2263/24842.

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The potentially hazardous nature of open pit mining requires the application of sound geotechnical engineering practice to mine design, for the purpose of permitting safe and economic mining of any commodity within any rock mass. The Lerala Diamond Project is situated in the south west of Botswana near the Martin’s Drift Border Post. A 2m-soil cover made surface mapping of geological features impossible, so a number of geotechnical holes were drilled to evaluate the characteristics of the kimberlite pipes and the Granite/gneiss host rock. The Lerala Diamond Project is a typical example of the

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Burke, Shyne Duncan Caleb Padraig. "On carbonate alteration zones in a greenstone keel of the East Pilbara Terrane (Doolena Gap Greenstone Belt)." Thesis, Queensland University of Technology, 2017. https://eprints.qut.edu.au/107570/1/Duncan_Burke%20-%20Shyne_Thesis.pdf.

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This thesis examines the origin and relative timing of carbonate alteration zones in the poly-deformed Doolena Gap Greenstone Belt in the East Pilbara Terrane, the type locality of Archaean dome-and-keel-terranes. The key findings are: [1] shear-assisted carbonate alteration occurred throughout the entire tectonic history of the greenstone belt; and [2] weak pre- and syntectonic carbonate minerals make up 40 to 60% of the examined greenstone rocks. These outcomes imply that carbonate minerals likely controlled the strength of Archaean lithosphere.

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Books on the topic "Greenstone belt"

1

MacTavish, A. D. Precambrian geology: Montcalm Greenstone belt. Ontario Geological Survey and the Ministry of Northern Development and Mines, 1996.

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Ayer, John Albert. Precambrian geology: Northern Swayze Greenstone belt. Ontario Geological Survey, 1995.

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1942-, Lowe Donald R., and Byerly Gary R. 1948-, eds. Geologic evolution of the Barberton Greenstone Belt, South Africa. Geological Society of America, 1999.

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Osmani, Ikramuddin Ahmad. Geology and mineral potential: Greenwater Lake area, west-central Shebandowan Greenstone Belt. Ontario Ministry of Northern Development and Mines, 1997.

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Lafleur, Pierre Jean. The Archean Round Lake batholith, Abitibi greenstone belt: A synthesis. University of Ottawa, 1986.

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Jensen, L. S. Geology and petrogenesis of the Archean Abitibi Belt in the Kirkland Lake area, Ontario. Ontario Ministry of Natural Resources, 1985.

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Baldock, J. W. The geology of the Harare Greenstone Belt and surrounding granitic terrain. Zimbabwe Geological Survey, 1991.

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Subrahmanyam, V. Geochemistry, ore petrology, and genesis of gold mineralisation Kolar Greenstone Belt, Karnataka. Geological Survey of India, 1991.

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Geza, Kisvarsanyi Sheldon K. Grant, ed. Structural Control of Gold in the South Pass Granite-Greenstone Belt, Wyoming. University of Missouri-Rolla, 1988.

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W. Dan Hausel. Economic geology of the South Pass granite-greenstone belt, southern Wind River Range, western Wyoming. Geological Survey of Wyoming, 1991.

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Book chapters on the topic "Greenstone belt"

1

Arndt, Nicholas. "Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2022. http://dx.doi.org/10.1007/978-3-642-27833-4_676-5.

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Arndt, Nicholas. "Barberton Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_148.

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Arndt, Nicholas. "Barberton Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_148.

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Arndt, Nicholas. "Barberton Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_148-4.

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Arndt, Nicholas. "Barberton Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_148-3.

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O’Neil, Jonathan. "Nuvvuagittuq Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2022. http://dx.doi.org/10.1007/978-3-642-27833-4_1089-4.

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Hofmann, Axel. "Barberton Greenstone Belt, Sedimentology." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_149.

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Hofmann, Axel. "Barberton Greenstone Belt, Sedimentology." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_149.

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Hofmann, Axel. "Barberton Greenstone Belt, Sedimentology." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_149-3.

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Hofmann, Axel. "Barberton Greenstone Belt, Sedimentology." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-642-27833-4_149-4.

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Conference papers on the topic "Greenstone belt"

1

Holmes, H., P. A. Gledhill, J. C. Chatupa, and P. Akanyang. "Geophysics In The Maitengwe Greenstone Belt." In 3rd SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.224.048.

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Mathieu, Lucie, Baptiste Madon, Alexandre Crépon, Patrick Berthoty, and Daniel Kontak. "Magmatic Evolution of a Neoarchean Greenstone Belt." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1742.

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Silva*, Ezequiel Costa e., Adalene Moreira Silva, Catarina L. B. Toledo, and David Otterman. "Gold Prospectivity Mapping of Andorinhas Greenstone Belt, Para." In 12th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 15-18 August 2011. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2011. http://dx.doi.org/10.1190/sbgf2011-245.

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de Araújo Vieira, M., and S. Lima da Silva. "Caracterizaçăo Geológico-Geofísica do Greenstone Belt Rio das Velhas." In 4th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609-pdb.313.159.

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Paiva De Oliveira, Elson, and Gabriel Sombini Dos Santos. "Geochemistry of chemical sediments from Piumhi greenstone belt - MG." In XXIII Congresso de Iniciação Científica da Unicamp. Galoá, 2015. http://dx.doi.org/10.19146/pibic-2015-37278.

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Touboul, Mathieu, Caroline Fitoussi, and Jonathan O'Neil. "Exotic Mo isotope composition in the Nuvvuagittuq Greenstone belt." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7475.

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Фролов, Петр, Вера Ильина, Александр Завёрткин, Екатерина Климовская, and Александр Савицкий. "Karelian talc as a raw material: practical application and potential contribution to Russian mineral raw material reserves." In Mineralogical and technological appraisal of new types of mineral products. Karelian Research Center of RAS, 2019. http://dx.doi.org/10.17076/tm13_6.

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Talc is a unique natural material. Some talc-bearing rocks, e.g. soapstone, are also useful minerals. There are talc deposits on the Fennoscandian Shield. The main potential talc resources and reserves are in the Karelian Craton, which is part of the shield. Talc deposits in the Finnish extension of the craton are being mined in the Kainuu Schist Belt and soapstone deposits in the Suomussalmi-Kuhmo Greenstone Belt. The Karelian portion of the craton seems to be more promising for talc-bearing deposits, because favourable rock complexes of greenstone belts are more common there. The revival of

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Hoover, D. B., and W. D. Heran. "Geophysics in Gold Exploration: Application to Greenstone Belt Gold Deposits." In 3rd International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1993. http://dx.doi.org/10.3997/2214-4609-pdb.324.451.

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Nube, A., U. Weckmann, O. Ritter, et al. "Magnetotelluric Measurements Across the Southern Barberton Greenstone Belt: Data Analysis." In 11th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.241.nube_abstract.

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Retallack, Gregory J., and Nora Noffke. "PALEOSOL FROM THE 3.7 GA ISUA GREENSTONE BELT, SOUTHWEST GREENLAND." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-315250.

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Reports on the topic "Greenstone belt"

1

Jackson, S., and A. Fyon. Regional Geology - Abitibi Greenstone Belt. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132293.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Sultan, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210453.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Gogama, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210455.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Westree, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210456.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Biscotasing, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210458.

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Fyon, A., and S. Jackson. District Geology - Central Abitibi Greenstone Belt. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132294.

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Henderson, J. R., M. N. Henderson, J. A. Kerswill, and J. F. Dehls. Geology, High Lake greenstone belt, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211530.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Rollo Lake, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210450.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Rush Lake, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210451.

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Heather, K. B., and G. T. Shore. Geology, Swayze greenstone belt, Mattagami Lake, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210452.

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