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Relevant bibliographies by topics / Kimberlito

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Academic literature on the topic 'Kimberlito'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Kimberlito"

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Kargin, Alexey Vladimirovich, Anna Andreevna Nosova, Ludmila Vyacheslavovna Sazonova, Vladimir Vasilievich Tretyachenko, Yulia Olegovna Larionova, and Elena Vladimirovna Kovalchuk. "Ultramafic Alkaline Rocks of Kepino Cluster, Arkhangelsk, Russia: Different Evolution of Kimberlite Melts in Sills and Pipes." Minerals 11, no. 5 (2021): 540. http://dx.doi.org/10.3390/min11050540.

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To provide new insights into the evolution of kimberlitic magmas, we have undertaken a detailed petrographic and mineralogical investigation of highly evolved carbonate–phlogopite-bearing kimberlites of the Kepino cluster, Arkhangelsk kimberlite province, Russia. The Kepino kimberlites are represented by volcanoclastic breccias and massive macrocrystic units within pipes as well as coherent porphyritic kimberlites within sills. The volcanoclastic units from pipes are similar in petrography and mineral composition to archetypal (Group 1) kimberlite, whereas the sills represent evolved kimberlit

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Chaves, Mario Luiz de Sá C., Paulo Roberto Gomes Brandão, Antonio Carlos Girodo, and Leila Benitez. "Kimberlito Canastra-1 (São Roque de Minas, MG): geologia, mineralogia e reservas diamantíferas." Rem: Revista Escola de Minas 61, no. 3 (2008): 357–64. http://dx.doi.org/10.1590/s0370-44672008000300014.

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A pesquisa de fontes diamantíferas primárias no Brasil iniciou-se na década de 1960, culminando com a descoberta da mineralização no kimberlito Canastra-1, que representa a primeira fonte primária com teores economicamente viáveis do país. O kimberlito aflora na região da Serra da Canastra, nas cabeceiras do rio São Francisco. A intrusão é constituída de dois blows alinhados segundo NW-SE, o trend estrutural da região definido em metassedimentos do Grupo Canastra. O blow menor (NW), quase circular e com ±0,8 ha de área, possui teores desprezíveis em diamantes. O outro (SE), com quase 1 ha, é m

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Jones, T. J., J. K. Russell, L. A. Porritt, and R. J. Brown. "Morphology and surface features of olivine in kimberlite: implications for ascent processes." Solid Earth 5, no. 1 (2014): 313–26. http://dx.doi.org/10.5194/se-5-313-2014.

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Abstract. Most kimberlite rocks contain large proportions of ellipsoidal-shaped xenocrystic olivine grains that are derived mainly from disaggregation of peridotite. Here, we describe the shapes, sizes and surfaces of olivine grains recovered from kimberlite lavas erupted from the Quaternary Igwisi Hills volcano, Tanzania. The Igwisi Hills kimberlitic olivine grains are compared to phenocrystic olivine, liberated from picritic lavas, and mantle olivine, liberated from a fresh peridotite xenolith. Image analysis, scanning electron microscopy imagery and laser microscopy reveal significant diffe

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Chen, Yunfeng, Yu Jeffrey Gu, Larry M. Heaman, Lei Wu, Erdinc Saygin, and Shu-Huei Hung. "Reconciling seismic structures and Late Cretaceous kimberlite magmatism in northern Alberta, Canada." Geology 48, no. 9 (2020): 872–76. http://dx.doi.org/10.1130/g47163.1.

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Abstract The Late Cretaceous kimberlites in northern Alberta, Canada, intruded into the Paleoproterozoic crust and represent a nonconventional setting for the discovery of diamonds. Here, we examined the origin of kimberlite magmatism using a multidisciplinary approach. A new teleseismic survey reveals a low-velocity (−1%) corridor that connects two deep-rooted (&gt;200 km) quasi-cylindrical anomalies underneath the Birch Mountains and Mountain Lake kimberlite fields. The radiometric data, including a new U-Pb perovskite age of 90.3 ± 2.6 Ma for the Mountain Lake intrusion, indicate a nort

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Eccles, D. Roy, Robert A. Creaser, Larry M. Heaman, and Jeff Ward. "Rb–Sr and U–Pb geochronology and setting of the Buffalo Head Hills kimberlite field, northern AlbertaThis article is one of a selection of papers published in this Special Issue on the theme Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers." Canadian Journal of Earth Sciences 45, no. 5 (2008): 513–29. http://dx.doi.org/10.1139/e07-050.

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New Rb–Sr phlogopite and U–Pb perovskite age determinations for 12 of 38 known ultramafic bodies in the Buffalo Head Hills area of north-central Alberta show that kimberlitic magmatism occurred in at least two separate episodes during Late Cretaceous and Paleocene time. Nine kimberlites yield Coniacian to Campanian ages of between 88 ± 5 Ma (U–Pb perovskite, K5A) and 81.2 ± 2.3 Ma (Rb–Sr phlogopite, K252). A Danian U–Pb perovskite isochron age of 63.5 ± 0.7 Ma was obtained for the BM2 kimberlite, and Selandian Rb–Sr ages of 59.6 ± 2.8 and 60.3 ± 0.8 Ma were determined for the K1A and K19 bodie

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Kopylova, Maya G., and Patrick Hayman. "Petrology and textural classification of the Jericho kimberlite, northern Slave Province, Nunavut, Canada." Canadian Journal of Earth Sciences 45, no. 6 (2008): 701–23. http://dx.doi.org/10.1139/e08-011.

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The paper presents data on petrology, bulk rock and mineral compositions, and textural classification of the Middle Jurassic Jericho kimberlite (Slave craton, Canada). The kimberlite was emplaced as three steep-sided pipes in granite that was overlain by limestones and minor soft sediments. The pipes are infilled with hypabyssal and pyroclastic kimberlites and connected to a satellite pipe by a dyke. The Jericho kimberlite is classified as a Group Ia, lacking groundmass tetraferriphlogopite and containing monticellite pseudomorphs. The kimberlite formed during several consecutive emplacement e

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Chaves, Mario Luiz de Sá C. "Kimberlito vargem-1 (Coromandel, MG): bulk sample confirma mineralização diamantífera." Rem: Revista Escola de Minas 65, no. 4 (2012): 509–11. http://dx.doi.org/10.1590/s0370-44672012000400011.

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O kimberlito Vargem-1, a sudeste de Coromandel (MG), ocorre sob o leito e margens do Rio Santo Inácio, o qual possui depósitos aluvionares lavrados desde longa data. Entretanto, a presença de diamantes na intrusão foi sempre questionada, pois teria uma química mineral desfavorável à mineralização. Agora, amostragem de grande volume, em execução por firma mineradora, revelou a presença de diamantes, com pesos inferiores a 1 ct, em um dos poços pesquisados. Esse fato "abre" nova perspectiva exploratória em dezenas de intrusões já identificadas em tal região.

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Heaman, Larry M., David Phillips, and Graham Pearson. "Dating Kimberlites: Methods and Emplacement Patterns Through Time." Elements 15, no. 6 (2019): 399–404. http://dx.doi.org/10.2138/gselements.15.6.399.

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Key to deciphering the origin and tectonic setting of kimberlite magmatism is an accurate understanding of when they formed. Although determining absolute emplacement ages for kimberlites is challenging, recent methodological advances have contributed to a current database of &gt;1,000 precisely dated kimberlite occurrences. Several profound findings emerge from kimberlite geochronology: kimberlites were absent in the first half of Earth history; most kimberlites were emplaced during the Mesozoic; kimberlite magma formation may be triggered by a variety of Earth processes (deep mantle plum

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Tukiainen, Tapani, and Leif Thorning. "Detection of kimberlitic rocks in West Greenland using airborne hyperspectral data: the HyperGreen 2002 project." Geological Survey of Denmark and Greenland (GEUS) Bulletin 7 (July 29, 2005): 69–72. http://dx.doi.org/10.34194/geusb.v7.4845.

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Previous investigations by the Geological Survey of Denmark and Greenland (GEUS) and exploration companies have demonstrated that some of the kimberlites in West Greenland are diamond bearing, making the region an important target for diamond prospecting. High-resolution hyperspectral (HS) remote sensing data have been successfully used for the location of kimberlitic rocks, e.g. in Australia and Africa. However, its potential as a viable method for the mapping of kimberlite occurrences in Arctic glaciated terrain with high relief was previously unknown. In July–August 2002, GEUS conducted an

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Zurevinski, S. E., L. M. Heaman, R. A. Creaser, and P. Strand. "The Churchill kimberlite field, Nunavut, Canada: petrography, mineral chemistry, and geochronology." Canadian Journal of Earth Sciences 45, no. 9 (2008): 1039–59. http://dx.doi.org/10.1139/e08-052.

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Seventy-nine kimberlite intrusions have been identified in the Churchill Province, Nunavut, the result of an aggressive diamond exploration program by Shear Minerals Ltd. and their partners. This is one of Canada’s newest and largest kimberlite districts, situated immediately west of Hudson Bay between the communities of Rankin Inlet and Chesterfield Inlet. This study documents the occurrence of bonafide kimberlite rocks, classified as mainly sparsely macrocrystic, oxide-rich calcite evolved hypabyssal kimberlite and macrocrystic oxide-rich monticellite phlogopite hypabyssal kimberlite. Electr

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Dissertations / Theses on the topic "Kimberlito"

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Costa, Vicente Sérgio. "Estudos mineralógicos e químicos do Kimberlito Batovi 6 (MT) em comparação com as intrusões Três Ranchos 4 (GO) e Limeira 1(MG)." [s.n.], 1996. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287190.

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Orientador: Bernardino Ribeiro de Figueiredo, Ricardo Kalikowski Weska<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-17T06:31:03Z (GMT). No. of bitstreams: 1 Costa_VicenteSergio_M.pdf: 5783649 bytes, checksum: cd9d1ac684f6489b6324815f761d849f (MD5) Previous issue date: 1996<br>Resumo: As características texturais da intrusão Batovi 6 (MT), a sua composição mineralógica à base de olivina. granada, ilinenita, espinélio, flogopita e perovskita, e as suas assinaturas geoquímica e isotópica ('oNdf'"Nd = 0.512701; 87S

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Adrião, Álden de Brito. "Heterogeneidade mantélica na fonte da Província Magmática Paraná : nova evidência de 128 Ma da Província kimberlítica Rosário do Sul, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/131915.

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O presente trabalho representa um e estudo petrográfico detalhado, as primeiras análises de elementos maiores e traços de rocha total, dados isotópicos Sr-Nd e idade U-Pb em CaTi-perovskitas para o kimberlito Rosário-6 da Província Kimberlítica de Rosário do Sul (PKRS). Esta área está localizada na borda da Bacia do Paraná, sul do Brasil e representa o melhor afloramento de PKRS, sendo a única com amostras de rocha coesa. Mineralogia primária do kimberlito Rosário-6 compreende duas gerações de cristais de olivina: fenocristais (<2 mm) e macrocristais (>2 mm), alem de microcristais de CaTi-pero

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Donatti, Filho Jose Paulo 1981. "Petrogênese do campo kimberlítico Brauna, Cráton do São Francisco." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287306.

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Orientador: Elson Paiva de Oliveira<br>Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-19T05:31:18Z (GMT). No. of bitstreams: 1 DonattiFilho_JosePaulo_D.pdf: 4183333 bytes, checksum: fdab4641a69f3e0cb09bddeb14a2dedf (MD5) Previous issue date: 2011<br>Resumo: A presente tese concentrou-se na classificação do magmatismo kimberlítico do Campo Kimberlítico Brauna no nordeste do Craton do São Francisco, e sua relação com as rochas encaixantes, xenólitos (e.g. crustais e mantélicos), mineralizações diamantíferas e contexto tectô

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Carniel, Larissa Colombo. "Heterogeneidade mantélica na Região Sul do Brasil evidenciada por mineraloquímica de kimberlitos." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2017. http://hdl.handle.net/10183/171433.

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Kimberlitos são rochas vulcânicas que, frequentemente, contêm diamante, grafite e/ou carbonato, sendo a presença destes componentes diretamente influenciada pela variabilidade da fugacidade de oxigênio (fO2) do magma durante a sua ascenção. Segundo Chakhmouradian and Mitchell (2000), CaTiO3-perovskitas podem ser usadas para revelar as condições de alguns dos múltiplos estágios de cristalização da história magmática destas rochas. No intuito de estabelecer a fugacidade de oxigênio de magmas kimberlíticos naturais, CaTiO3-perovskitas foram cristalizadas experimentalmente em equilíbrio com um líq

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Provenzano, Carlos Augusto Silva. "Caracterização petrográfica, química mineral e petrogênese do Kimberlito Alfeu I - Canguçu/RS e uma revisão conceitual de magmatismo e rochas kimberlíticas." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/150904.

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O kimberlito Alfeu-I é uma chaminé vulcânica intrusiva na Suíte Pinheiro Machado no domínio Batólito Pelotas, que ocorre na porção leste do Escudo Sul Rio Grandense (ESRG). O corpo apresenta uma forma semicircular com diâmetro ≈20m. As feições texturais e estruturais primárias e a mineralogia encontradas nas rochas deste corpo indicam que, pelo nível de exposição atual, podem ser relacionadas ao fácie diatrema. A rocha é composta por fenocristais e megacristais/macrocristais de composição variada (micas, espinélio, granada, ilmenita e piroxênios), em matriz intersticial com clastos acrescionár

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Costa, Giulianna Vieira da. "Química mineral e geotermobarometria de xenólitos mantélicos do Kimberlito Canastra-01." reponame:Repositório Institucional da UnB, 2008. http://repositorio.unb.br/handle/10482/4871.

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Dissertação (mestrado)—Universidade de Brasília, Instituto de Geociências, 2008.<br>Submitted by Suelen Silva dos Santos (suelenunb@yahoo.com.br) on 2009-09-14T18:49:07Z No. of bitstreams: 1 2008_GiuliannaVieiraCosta.pdf: 3891774 bytes, checksum: be435ecd3b3e469c053943aa033cfc68 (MD5)<br>Rejected by Gomes Neide(nagomes2005@gmail.com), reason: Como dei a explicação dos erros. Beijinhos Kell on 2010-05-27T17:51:00Z (GMT)<br>Submitted by Suelen Silva dos Santos (suelenunb@yahoo.com.br) on 2010-05-27T18:37:28Z No. of bitstreams: 1 2008_GiuliannaVieiraCosta.pdf: 3694516 bytes, checksum: 7fb

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Thomaz, Leandro Vasconcelos. "Estudo petrográfico e química mineral da intrusão kimberlítica Régis, no oeste de Minas Gerais." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-19082009-094419/.

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O kimberlito Régis localiza-se no município do Carmo do Paranaíba, Minas Gerais. A intrusão possui formato elíptico e área aproximada de 1 km2. Com provável idade cretácea intrude rochas metassedimentares Neoproterozóicas do Grupo Bambuí. O ambiente geotectônico permanece em debate entre Faixa Brasília e Cráton do São Francisco. A presente dissertação contempla a descrição de afloramentos e de dois testemunhos de sondagem, com 250,6 e 316,4 metros. Através da caracterização macroscópica e petrográfica buscou-se subdividir a intrusão em fácies e compreender os mecanismos formadores destes depós

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Rocha, Lis Franco. "Inversão gravimétrica 3D e interpretação integrada dos métodos CSAMT, gravimétrico e magnetométrico no estudo do kimberlito Régis, MG, Brasil." Universidade do Estado do Rio de Janeiro, 2013. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=4892.

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Fundação Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro<br>Os diamantes são minerais raros e de alto valor econômico. Estes minerais se formam em condições mantélicas, numa profundidade aproximada de 150 a 200 km e ascendem à superfície englobada em magmas alcalinos e carbonatíticos, nos kimberlitos e lamproitos (depósitos primários). No presente trabalho objetivou-se o estudo da geometria do Kimberlito Régis, o qual pertence à província alcalina do Brasil Meridional, localizado no estado de Minas Gerais, na cidade de Carmo do Paranaíba. Para este estudo foi realizada uma

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Silva, Gisella Magalhães. "Análise geofísica do Distrito Diamantífero Abaeté (MG) e de suas possíveis fontes primárias." reponame:Repositório Institucional da UFOP, 2015. http://www.repositorio.ufop.br/handle/123456789/5414.

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Programa de Pós-Graduação em Evolução Crustal e Recursos Naturais. Departamento de Geologia. Escola de Minas, Universidade Federal de Ouro Preto.<br>Submitted by Oliveira Flávia (flavia@sisbin.ufop.br) on 2015-05-20T18:52:27Z No. of bitstreams: 2 license_rdf: 20592 bytes, checksum: 0c9b9c579af4cbbcf785ca803bd18d4b (MD5) DISSERTAÇÃO_AnáliseGeofísicaDistrito.pdf: 9181919 bytes, checksum: 3beb740f999273018f913b9b828d4be1 (MD5)<br>Approved for entry into archive by Gracilene Carvalho (gracilene@sisbin.ufop.br) on 2015-05-20T19:05:42Z (GMT) No. of bitstreams: 2 license_rdf: 20592 bytes, checksum:

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Almeida, Vidyã Vieira de. "Mineralogia e petrologia de xenólitos mantélicos das regiões de Ubatuba (SP) e Monte Carmelo (MG): evidências de fusão parcial e metassomatismo no manto superior do sudeste do Brasil." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-14102009-082110/.

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Estudos mineralógicos e petrológicos foram realizados em amostras de xenólitos do manto inclusos em dique de kaersutita lamprófiro de Ubatuba (SP) (Província Ígnea da Serra do Mar) e no Kimberlito Limeira 1 (Monte Carmelo, MG; Província Alcalina do Alto Paranaíba) utilizando petrografia e geoquímica de elementos maiores e traços em minerais por microssonda eletrônica e LA-ICPMS. Os espinélio lherzolitos de Ubatuba, para os quais foram estimadas temperaturas de equilíbrio entre 750 e 950°C, representam um manto fértil, afetado por proporções variáveis, mas sempre moderadas de empobrecimento. Ev

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Books on the topic "Kimberlito"

1

Kimberlites: Mineralogy, geochemistry, and petrology. Plenum Press, 1986.

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International Kimberlite Conference (4th 1986 Perth, W.A.). Kimberlites and related rocks: 4IKC : proceedings of the Fourth International Kimberlite Conference, Perth, 1986. Edited by Ross J and Geological Society of Australia. Published for the Geological Society of Australia Inc. by Blackwell Scientific, 1989.

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Ilupin, Iosif Petrovich. Kimberlity: Spravochnik. "Nedra", 1990.

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W. Dan Hausel. Geology of the Iron Mountain Kimberlite District: And Nearby Kimberlitic Indicator Mineral Anomalies in Southeastern Wyoming. Wyoming State Geological Survey, 2003.

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Mitchell, Roger H. Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0.

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M, Vladimirov B., ed. Geokhimicheskie osobennosti mineralov kimberlitov: Po dannym izuchenii͡a srednepaleozoĭskikh kimberlitov I͡Akutii. Izd-vo "Nauka," Sibirskoe otd-nie, 1986.

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Milashev, V. A. Kimberlity i glubinnai͡a︡ geologii͡a︡. "Nedra," Leningradskoe otd-nie, 1990.

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Bartoshinskiĭ, Z. V. Kristallomorfologii͡a︡ almaza iz kimberlitov. Nauk. dumka, 1991.

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Shkodzinskiĭ, V. S. Proiskhozhdenie kimberlitov i almaza. I͡A︡kutskiĭ nauch. t͡s︡entr SO RAN, 1995.

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Milashev, V. A. Ėnergeticheskie aspekty obrazovanii︠a︡ kimberlitov. VNIIOkeangeologii︠a︡, 2004.

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Book chapters on the topic "Kimberlito"

1

Mitchell, Roger H. "Postscript." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_10.

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Mitchell, Roger H. "Historical Aspects of Kimberlite Petrology." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_1.

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Mitchell, Roger H. "Kimberlite and Related Rocks." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_2.

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Mitchell, Roger H. "Kimberlite Magmatism and Textural Genetic Classifications of Kimberlite." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_3.

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Mitchell, Roger H. "Diatremes and Root Zones." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_4.

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Mitchell, Roger H. "Kimberlite Fields and Provinces: Their Tectonic Setting." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_5.

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Mitchell, Roger H. "Mineralogy of Kimberlites." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_6.

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Mitchell, Roger H. "Geochemistry of Kimberlites." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_7.

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Mitchell, Roger H. "Experimental Studies Relevant to the Formation and Crystallization of Kimberlite Magma." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_8.

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Mitchell, Roger H. "Petrogenesis and Evolution of Kimberlite Magma." In Kimberlites. Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-0568-0_9.

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Conference papers on the topic "Kimberlito"

1

Rocha, Lis, Emanuele La Terra, and Paulo de Tarso Menezes. "Inversão gravimétrica 3D e interpretação integrada dos métodos CSAMT, gravimétrico e magnetométrico no estudo do Kimberlito Régis, MG, Brasil." In 13th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 26-29 August 2013. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2013. http://dx.doi.org/10.1190/sbgf2013-083.

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Andrews, Graham D. M., J. Kelly Russell, Brenna G. Cole, and Sarah R. Brown. "THE KIMBERLITE FACTORY: THE VOLCANIC NATURE OF KIMBERLITES." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-325914.

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Vasilyev, Prokopiy, Brent McInnes, and Tom Reddicliffe. "Evaluation of the Source of Diamonds and Other Kimberlitic Minerals from the Webb Kimberlite Field, Western Australia." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2667.

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Hamilton, M. P., and S. J. Webb. "Delineation of kimberlite pipes using ground geophysical techniques: A Case Study of two kimberlites near Kimberley, South Africa." In 8th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.144.37.

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Pandey, Ashutosh, and N. v. Chalapathi Rao. "Geochemical Insights into the Distinct Mantle Sources of Coeval Shoshonitic Lamprophyres and Kimberlites from the Wajrakarur Kimberlite Field, Dharwar Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2024.

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Willmott, G. R. "Shock Properties of Kimberlite." In SHOCK COMPRESSION OF CONDENSED MATTER - 2003: Proceedings of the Conference of the American Physical Society Topical Group on Shock Compression of Condensed Matter. AIP, 2004. http://dx.doi.org/10.1063/1.1780521.

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Pal, S. K., and S. Kumar. "Kimberlite mapping using Electrical Resistivity Tomography in Wajrakarur kimberlite field, Eastern Dharwar craton." In 1st Indian Near Surface Geophysics Conference & Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201979029.

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Fedortchouk, Yana, and Ingrid Chinn. "Crystallization Conditions of Kimberlite Magma." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.695.

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Tyler, Duncan, and S. Godden. "Geotechnical Modelling for Kimberlite Pipes." In First Southern Hemisphere International Rock Mechanics Symposium. Australian Centre for Geomechanics, Perth, 2008. http://dx.doi.org/10.36487/acg_repo/808_159.

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Symons, G., and S. Lowe. "Geophysical Response Over A Kimberlite." In 5th SAGA Biennial Conference and Exhibition. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.223.003.

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Reports on the topic "Kimberlito"

1

McClenaghan, M. B., I. M. Kjarsgaard, and B. A. Kjarsgaard. Indicator mineralogy of the KL-01 and KL-22 kimberlites, Lake Timiskaming kimberlite field, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225398.

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Sader, J. A., M. I. Leybourne, M. B. McClenaghan, and S. M. Hamilton. Geochemistry of groundwater from Jurassic kimberlites in the Kirkland Lake and Lake Timiskaming kimberlite fields, northeastern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214841.

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3

McClenaghan, M. B., I. M. Kjarsgaard, and B. A. Kjarsgaard. Kimberlite indicator mineral chemistry and till geochemistry around the Seed and Triple B kimberlites, Lake Timiskaming, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215911.

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4

McClenaghan, M. B., I. M. Kjarsgaard, and B. A. Kjarsgaard. Kimberlite indicator mineral chemistry of the Bucke and Gravel kimberlites and associated indicator minerals in till, Lake Timiskaming, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/289599.

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Kjarsgaard, B. A. Kimberlite-hosted diamond. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/208034.

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Kjarsgaard, B. A. Kimberlites. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/210935.

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Pell, J., B. Clements, H. Grütter, S. Neilson, and H. Grenon. Following kimberlite indicator minerals to source in the Chidliak Kimberlite Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/300291.

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Pell, J., B. Clements, H. Grütter, S. Neilson, and H. Grenon. Following kimberlite indicator minerals to source in the Chidliak Kimberlite Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292687.

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9

Kjarsgaard, B. A. Les kimberlites. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/210934.

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10

Kjarsgaard, B. A. Prairie kimberlites. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/210965.

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