Academic literature on the topic 'Greenstone'

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Journal articles on the topic "Greenstone"

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Scherstén, Anders, Henrik Stendal, and Tomas Næraa. "Geochemistry of greenstones in the Tasiusarsuaq terrane, southern West Greenland." Geological Survey of Denmark and Greenland (GEUS) Bulletin 15 (July 10, 2008): 69–72. http://dx.doi.org/10.34194/geusb.v15.5047.

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Tonalite-trondhjemite–granodiorite (TTG) gneisses and mela nocratic to ultramafic greenstones dominate the Arc haean basement of southern West Greenland. The greenstones are likely to represent different original environments, which is important as the mineral deposits they may host depend on this. For example, massive sulphide deposits associated with gold and base metals are commonly volcan og enic, while chrome, nickel and platinum group elements are more commonly associated with layered intrusions (Robb 2005). Cur rent investigations by the Geological Survey of Denmark and Greenland (GEUS)
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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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Rakovan, John. "Greenstone." Rocks & Minerals 83, no. 6 (2008): 553–56. http://dx.doi.org/10.3200/rmin.83.6.553-556.

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Fushimi, Marcela, Mariana Pichinini, Ana María Sanllorenti Sanllorenti, and Martín Williman. "Greenstone." RDBCI: Revista Digital de Biblioteconomia e Ciência da Informação 16, no. 2 (2018): 306–28. http://dx.doi.org/10.20396/rdbci.v16i2.8655870.

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Este artigo apresenta as características e a história do software para criar e gerenciar bibliotecas digitais Greenstone, desenvolvidas inicialmente pela Universidade de Waikato, Nova Zelândia, em 1997. Primeiro, a comunidade de usuários é descrita a nível global, com foco no uso atual que o software conseguiu na Argentina: o número de implementações disponíveis, sua evolução, o tipo, tamanho e variedade dos desenvolvimentos existentes, bem como a sua aplicação à gestão de repositórios digitais de ciência e tecnologia no campo das instituições científicas, tecnológicas e de ensino superior na
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Hofmann, A., H. Xie, L. Saha, and C. Reinke. "Granitoids and greenstones of the White Mfolozi Inlier, south-east Kaapvaal Craton." South African Journal of Geology 123, no. 3 (2020): 263–76. http://dx.doi.org/10.25131/sajg.123.0019.

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Abstract A Palaeoarchaean greenstone fragment and associated granitoid gneisses from an area south of Ulundi in KwaZulu-Natal is described. The fragment consists of an association of garnetiferous amphibolite and calc-silicate that was intruded at 3388 ± 4 Ma by tonalite and at 3275 ± 4 Ma by trondhjemite. Strong ductile deformation of the greenstones and granitoids under amphibolite facies conditions (7 kbar and 600 to 650°C) took place prior to uplift and emplacement of a granite batholith at ~3.25 Ga ago in which the granitoid gneiss-greenstone domain is now found. Magmatism 3.27 to 3.25 Ga
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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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Thurston, Phillips C. "Igneous Rock Associations 19. Greenstone Belts and Granite−Greenstone Terranes: Constraints on the Nature of the Archean World." Geoscience Canada 42, no. 4 (2015): 437. http://dx.doi.org/10.12789/geocanj.2015.42.081.

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Greenstone belts are long, curvilinear accumulations of mainly volcanic rocks within Archean granite−greenstone terranes, and are subdivided into two geochemical types: komatiite−tholeiite sequences and bimodal sequences. In rare instances where basement is preserved, the basement is unconformably overlain by platform to rift sequences consisting of quartzite, carbonate, komatiite and/or tholeiite. The komatiite−tholeiite sequences consist of km-scale thicknesses of tholeiites, minor intercalated komatiites, and smaller volumes of felsic volcanic rocks. The bimodal sequences consist of basal t
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Abbott, D. "Greenstone belts." Eos, Transactions American Geophysical Union 79, no. 10 (1998): 123. http://dx.doi.org/10.1029/98eo00089.

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Falkenström, Per. "Greenstone Dimensions." Lithic Technology 36, no. 2 (2011): 141–52. http://dx.doi.org/10.1179/lit.2011.36.2.141.

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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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Dissertations / Theses on the topic "Greenstone"

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Bennett, Erin Kay. "Re-designing Greenstone for Seniors." The University of Waikato, 2008. http://hdl.handle.net/10289/2278.

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The golden generation have a wealth of experience and knowledge from throughout their lifetimes that younger generations wish to retain. In our technology filled world an obvious means of collecting this information is electronically. Digital library col- lections are increasingly used by libraries and large institutions to record their large amounts of information but they can also be used for personal collections. Seniors are often willing and keen to impart their years of experience upon people of the younger generation but time is not always on their side as they grow older. Throughout a l
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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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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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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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SOUZA, Zorano Sérgio de Souza. "Geologia e petrogênese do “Greenstone Belt” identidade: implicações sobre a evolução geodinâmica do terreno granito - “Greenstone” de Rio Maria, SE do Pará." Universidade Federal do Pará, 1994. http://repositorio.ufpa.br/jspui/handle/2011/7665.

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Submitted by Edisangela Bastos (edisangela@ufpa.br) on 2017-02-14T12:12:11Z No. of bitstreams: 3 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Tese_GeologiaPetrogeneseGreenstone_V1.pdf: 71676863 bytes, checksum: 533a6c11ec5056e6d7d5e3c25ec0a9fc (MD5) Tese_GeologiaPetrogeneseGreenstone_V2.pdf: 25031034 bytes, checksum: a1f5f43677654e5f560b4c78f08e5e4f (MD5)<br>Approved for entry into archive by Edisangela Bastos (edisangela@ufpa.br) on 2017-02-14T12:28:05Z (GMT) No. of bitstreams: 3 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Tese_GeologiaPetr
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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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Books on the topic "Greenstone"

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J, De Wit Maarten, and Ashwal Lewis D, eds. Greenstone belts. Clarendon Press, 1996.

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Berwick-Emms, Patricia. Greenstone diamond. Heinemann Education, 1990.

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J, De Wit Maarten, and Ashwal Lewis D, eds. Greenstone belts. Clarendon Press, 1997.

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Hemingway, Amanda. The Greenstone grail. BCA, 2004.

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Crump, Barry. Gold and greenstone. B. Crump Associates, 1993.

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Hemingway, Amanda. The Greenstone Grail. Random House Publishing Group, 2005.

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Hemingway, Amanda. The Greenstone grail. Del Rey/Ballentine Books, 2005.

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

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Stulʹchikov, V. A. Zakonomernosti metamorfizma i metasimatoza zelenokamennykh poi͡a︡sov Ukrainskogo shchita: Na primere Verkhovt͡s︡evskoĭ sinklinali. Nauch. dumka, 1991.

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Fedchuk, V. I︠A︡. Metallogenicheskie osobennosti geneticheskikh tipov zelenokamennykh poi︠a︡sov. Moskovskiĭ gos. geologorazvedochnyĭ universitet, 2003.

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Book chapters on the topic "Greenstone"

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Arndt, Nicholas. "Greenstone Belts." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_676-3.

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Arndt, Nicholas. "Greenstone Belts." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_676.

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Arndt, Nicholas. "Greenstone Belts." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_676.

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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. "Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_676.

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Arndt, Nicholas. "Greenstone Belts." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-642-27833-4_676-4.

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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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O’Neil, Jonathan. "Nuvvuagittuq Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_1089.

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Arndt, Nicholas. "Barberton Greenstone Belt." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-65093-6_148.

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Conference papers on the topic "Greenstone"

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Witten, Ian H., Stefan J. Boddie, David Bainbridge, and Rodger J. McNab. "Greenstone." In the fifth ACM conference. ACM Press, 2000. http://dx.doi.org/10.1145/336597.336650.

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Bainbridge, David, and Ian H. Witten. "Greenstone digital library software." In the 2004 joint ACM/IEEE conference. ACM Press, 2004. http://dx.doi.org/10.1145/996350.996483.

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Cunningham, Sally Jo, and Erin K. Bennett. "Tailoring greenstone for seniors." In the 2009 joint international conference. ACM Press, 2009. http://dx.doi.org/10.1145/1555400.1555471.

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Witten, Ian H., David Bainbridge, Gordon Paynter, and Stefan Boddie. "The Greenstone plugin architecture." In the second ACM/IEEE-CS joint conference. ACM Press, 2002. http://dx.doi.org/10.1145/544220.544285.

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Bainbridge, David, Xiao Hu, and J. Stephen Downie. "A Musical Progression with Greenstone." In the 1st International Workshop. ACM Press, 2014. http://dx.doi.org/10.1145/2660168.2660170.

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Witten, Ian H., and David Bainbridge. "A retrospective look at Greenstone." In the 2007 conference. ACM Press, 2007. http://dx.doi.org/10.1145/1255175.1255204.

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Bainbridge, David, Steve Jones, Sam McIntosh, Matt Jones, and Ian H. Witten. "Running greenstone on an ipod." In the 8th ACM/IEEE-CS joint conference. ACM Press, 2008. http://dx.doi.org/10.1145/1378889.1378966.

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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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Witten, Ian H., and David Bainbridge. "Building digital library collections with greenstone." In the 5th ACM/IEEE-CS joint conference. ACM Press, 2005. http://dx.doi.org/10.1145/1065385.1065530.

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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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Reports on the topic "Greenstone"

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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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