mineral characteristics of a diamond

Chemical Geology, 186, 2002, pp. Harris, H. (1994) Fancy Color Diamonds. Uitgeverij Artis, Brussel (in Dutch). Shatsky, V.S., Sobolev, N.V., and Vavilov, M.A. : 43; Sterrett, Douglas Bovard (1907), Precious stones: Mineral Resources U.S., 1906, part 2: 1217; Murdoch, Joseph & Robert W. Webb (1966), Minerals of California, Centennial Volume (1866-1966): California Division Mines & Geology Bulletin 189: 170. (1991) High internal-pressures in diamond fluid inclusions determined by infrared-absorption. Bol. Sidorov, E. G., Tolstykh, N. D., Podlipsky, M. Y., & Pakhomov, I. O. London; Harper Brothers, first edition. Fibrous diamonds from the placers of the northeastern Siberian Platform: carbonate and silicate crystallization media. Yana Fedortchouk, Dante Canil and Jon A. Carlson (2005) Dissolution forms in Lac de Gras diamonds and their relationship to the temperature and redox state of kimberlite magma. Tolansky, S. (1962) The History and Use of Diamond. Shigley, J. E., Dirlam, D. M., Laurs, B. M., Boehm, E. W., Bosshart, G., & Larson, W. F. (2000). Diamond should be able to scratch a mirror with no problems. Mineralium Deposita, 33, 238-254. Cairncross, B. Stroud, December, 2001. Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. Book&Media Publishing, 156 pp. This section is currently hidden. (in Dutch). Silliman, Benjamin, Jr. (1867c), On new localities of diamonds in California: American Journal of Science, 2nd. Meen, V.B. 2. (2000). Wiley 844pp, http://www.museum.hu-berlin.de/min/mitarbeiter/mitarb/ralf/diamante.html, GSA Special Paper 384 (2005) pp 299-314; http://www.museum.hu-berlin.de/min/mitarbeiter/mitarb/ralf/diamante.html, Schmitt RT, Lapke C, Kenkmann T, Stöffler D (1999): Impaktdiamanten aus dem Nördlinger Ries.- Ber. Kuznetsova, A.N. Economic Geology, 88(1), 44-54. A diamond ranks a 10 on the Mohs Hardness Scale. Distribution and characteristics of diamonds from Myanmar. Pham Van Long, Gaston Giuliani, Virginie Garnier, Daniel Ohnenstetter (2004) Gemstones in Vietnam. Diamonds from … Mining Annual Review (1985): 390.; Melton, C. E. (1981). Geochimica et Cosmochimica Acta: 58: 761-771.; Mineralogical Magazine 73,43-50 (2009). Science 290, 320-325. and L.F. Semenova (1997) On the Selection of Chondrites for Studying Interstellar Diamond. O'Neil, P. (1983) Planet Earth - Gemstones. (1996) A carbon and nitrogen isotope study of diamond from primitive chondrites: Meteoritics & Planetary Science 31(3):343-355. Clark, Andrew, Stokman, A.H.W. The diamonds are easily weathered out of their kimberlite host rock and are washed away by streams and rivers. Petrology, 14(3), 299-317. (July 1996). Nature: 353: 746-748. Time-Life Books, Arlington, Virginia, USA, 176 pages. Lithology and Mineral Resources, 33(6), 525–538. Report 4, 410 pp. (1994) Hydrous and carbonatitic mantle fluids in fibrous diamonds from Jwaneng, Botswana. Ontario Geological Survey (2014), Mineral Deposit Inventory file No. physica status solidi (b) Vol 244, #11 (Special Issue: Electronic Properties of Novel Nanostructures), 3955–3959. P. Dikov, S. L. Molodtsov (2007). Newton, C.M. ; All gemstones have some characteristics falling short of perfection though; even the seemingly perfect Diamond has four directions of cleavage. Jeannine and Jacques Cassedanne : "Présence d'eskolaite dans les alluvions stannifères de la Chapada Diamantina (Bahia-Brésil), Bull. Diamond is a mineral with unique properties and many gem and industrial uses! Meyer, Eds., Kimberlites, Diatremes and Diamonds: their Geology and Petrology and Geochemistry, Vol. Field, M., Stiefenhofer, J., Robey, J., and Kurszlaukis, S. (2008): Ore Geology Reviews 34, 33-75.; Westerlund, K. J., & Gurney, J. J. Petrology and geochemistry of diamondiferous Mesoproterozoic kimberlites from Wajrakarur kimberlite field, Eastern Dharwar craton, southern India: genesis and constraints on mantle source regions. PRO 99-09. Merapi Volcano, Indonesia. Geological and Mines Dept. Gems & Gemology 49, 188-222. (2011). Luster is adamantine to waxy. Shigley, J. E., Chapman, J., & Ellison, R. K. (2001). and L.F. Semenova (1997) On the Selection of Chondrites for Studying Interstellar Diamond. #5227. A fake diamond will reveal the dot at the bottom of the diamond. Diamonds are usually coloures, some are tinged yellow, some blue, brown, green, pink and even black. A diamond ranks a 10 on the Mohs Hardness Scale. Sutton, J.R. (1928) Diamond, a descriptive treatise. Earth and Planetary Science Letters: 105(1-3): 1-12. American Mineralogist, 98(4), 574-581. Mineralogical Review pp 28-34. ; Wilson, M. G. C., Henry, G., & Marshall, T. R. (2006). ; (2000). Terra Scientific, Tokyo. (2010). C. Lemanski, Jr. (re-entry of lost Mindat data). ; Alekseenko, A.V. (March 2000), Minerals of Virginia, 1990 by R. V. Dietrich, Cannon, B. in Abdurrahman, A., J. C. Ø. Andersen, and B. J. Williamson. Airiyants, E. V., Zhmodik, S. M., Ivanov, P. O., Belyanin, D. K., & Agafonov, L. V. (2014). Sauer, J.R. (1982) Brazil, Paradise of Gemstones. in Impact Cratering: Processes and Products, First Edition. In R.G. Zapiski RMO (Proceedings of the Russian Mineralogical Society) 140, 92-99 (in Russian). Mineral inclusions in Fe-Pt solid solution from the alluvial ore occurrences of the Anabar basin (northeastern Siberian Platform). Giuliani, A., Kamenetsky, V.S., Phillips, D., Kendrick, M.A., Wyatt, B.A., and Goemann, K. (2012) Nature of alkali-carbonate fluids in the sub-continental lithospheric mantle. (1990) Diamonds from Kimberley, Western Australia. Ruiz-Cruz, M. D., & De Galdeano, C. S. (2012). Minerals form in many ways. Buchester K.J. The Kimberlites and Lamproites of Western Australia: Geol. Economic Geology, 94(5), 749-758. Journal of Petrology 40:79-104l; R&M 81:278-283; Goldschmidt Conference Abstracts (2011) Mineralogical Magazine p1894, http://74.125.95.132/search?q=cache:g3e0AupWVgMJ:www.infomine.com/index/properties/ARTEMISIA_-_CORONATION_GULF.html+Artemisia+pipe&cd=3&hl=en&ct=clnk&gl=us&client=firefox-a, http://www.allbusiness.com/mining-extraction/mines-mining/5931474-1.html. G.M.Yatsenko, Ye.M.Slyvko, A.I.Rosykhina(2000) Allied Mantle Components Of The Klyntsi Gold Zone And The Rivne Explosive Structures (the central part of the Ukrainian shield). Mineral, 5, 659-675. Blackwell Publishing Ltd. Verchovsky et al., (1999) Presolar Diamonds from Efremovka & Boriskino: C, N and Noble Gas Isotopes in Grain Size Fractions and Implications for the Origin of Diamonds (abs). In Doklady earth sciences (Vol. 624p [p.151-152], Lacroix, A. China. Hall, C. (1998) Identifying Gems & Precious Stones (The new compact study guide and identifier). (pp. Mineral inclusions in diamonds from Komsomolskaya and Krasnopresnenskaya pipes, Yakutia: Evidence for deep lithospheric heterogeineties in Siberian craton [ext. A review of the alluvial diamond industry and the gravels of the North West Province, South Africa. ; Walsh, K.L. Dana 6:A3:32. Industrial diamonds are embedded in large steel drill bits to drill into rock for wells to find water, oil, and natural gas. Bow River Alluvial Diamond Deposit; VW Fazakerley; AusIMM, Melbourne, mono 14, V2, pp1659-1664. (2011) Nature of different compositions of inclusions in diamond. Borneo: its geology and mineral resources. Mining Annual Review (1985) 147.; Zinchuk, N.N., and Koptil, V.I. Meteoritics 27 (3):267–268. Science: 261(5117): 66-68. ]), Letseng-La-Terae Mine (Letseng Mine; Lets'eng Mine), Tenoumer concession (Tenoumer kimberlite), Allende meteorite (Pueblito de Allende meteorite; Qutrixpileo meteorite [NHM cat. Het dagelijkse leven in de "Diamond Square Mile". Rocks & Minerals (xxxx) 21, 199; 23, 608. http://benonicitytimes.co.za/wp-content/uploads/sites/26/2013/10/Benoni-History-23.pdf?9187d3. Marshall, J.M. Rocks & Min. MAIK Nauka/Interperiodica. (1996) Diamonds and carbonadoof Primorskii Krai: mineralogy, crystal; chemistry and genesis, - Geologiya Rudnyh Mestorozhdenii, v.38, №6, p.485-499 (in Russian). New York: John Day Co., first edition. Division of Mines, Mining, and Geology, Ream, Lanny R. 2004. Khar'kiv, A. D., Levin, V. I., Mankenda, A., & Safronov, A. F. (1992). ; Dissanayake, C.B., Chandrajith, R., Tobschall, H.J. The presence of a ... A crystal is a tiny bit of mineral, diamond or other matter found within a diamond. Petrology of two diamondiferous eclogite xenoliths from the Lahtojoki kimberlite pipe, eastern Finland. 5, s. 442-449. American Mineralogist: 75: 1110–1119. Wiley & Sons, 235 pp. A high-chromium corundum (ruby) inclusion in diamond from the Sao Luiz alluvial mine, Brazil. : 43; Murdoch, Joseph & Robert W. Webb (1966), Minerals of California, Centennial Volume (1866-1966): California Division Mines & Geology Bulletin 189: 171. In Extended Abstracts of 9th International Kimberlite Conference. The fall, recovery, orbit, and composition of the Tagish Lake meteorite: A new type of carbonaceous chondrite. Durnez, E. (2008) Antwerpen, zuivere diamant. In Mineral Deposit Research: Meeting the Global Challenge (pp. Diamond is the only gem made of a single element: It is typically about 99.95 percent carbon. ; Roesener, H. (2000). Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences. The Geological Society of South Africa; Cairncross, B. Diamond is the hardest natural material known and is often used for industrial cutting and polishing tools. Hawthorne, F.C., Lussier, A.J., Ball, N.A., Henry, D.J., Shimizu, R., Ogasawara, Y., Ota, T. (2016): Maruyamaite, K(MgAl2)(Al5Mg)Si6O18(BO3)3(OH)3O, from the ultrahigh-pressure Kokchetav massif, northern Kazakhstan: Description and crystal structure. Meteoritics 7 (4) 547-552.; Marvin, U. Sutherland, D.G. Fetherston, J.M., Stocklmayer, S.M., Stocklmayer, V.C. (1990) Silicon carbide cluster entrapped in a diamond from Fuxian, China. For a colorless stone such as D or E on the color scale, fluorescence is not benefi… West. A Half-century monopoly (1880-1930s): the black diamonds (carbonados) of Bahia and Jewish Merchants. Journal of Metamorphic Geology, 35(5), 541-564. Hwang, T.F. Pronunciation Icon - Sound file Courtesy Photo Atlas of Minerals. ; Softer minerals can be scratched by harder minerals because the forces that hold the crystals together are weaker and can be broken by the harder mineral. (2000). Published by the Geological Survey of New South Wales. (2013) Gemstones of Western Australia. Gübelin, E., Wolgensinger, M. (1976) Edelstenen. Barricade Books, Fort Lee, NJ, 236 pp. Mining Annual Review (1985) 147.; Uitgeverij Artis, Brussel (in Dutch). Used for the windows on the Venera spacecraft to photograph Venus' surface. Geological Survey of New South Wales, Sydney, 576pp. Time-Life Books, Arlington, Virginia, USA, 176 pages. Gübelin, E., Wolgensinger, M. (1976) Edelstenen. Geological Survey of Western Australia, Bulletin No. Bulletin of the Geological Society of Finland, 72(1-2), 5-20. Fleischer, R. (1998) Mineralium Deposita, 33, 238-254. Hanks, Henry Garber (1882b), Diamonds in California: California Mining Bureau. 6th orogenic lherzolite conference 2014 Morocco; Yang, J., Meng, F., Xu, X., Robinson, P. T., Dilek, Y., Makeyev, A. Pouclet A. D. A. Zedgenizov, A. Shatskiy, A. L. Ragozin, H. Kagi and V. S. Shatsky (2014): Merwinite in diamond from São Luiz, Brazil: A new mineral of the Ca-rich mantle environment. Izraeli, E.S., Harris, J.W., and Navon, O. 18). The markets for gem-grade and industrial-grade diamonds value diamonds differently. (1982): Alnö Diamonds. 1: 1-15. (1997) Metallogenic Study and Mineral Deposit Data Sheets: Inverell Metallogenic Map (SH/56-5). ^ 4^ 0Ar-^ 3^ 9Ar Dating of the Kodomali Pipe, Bastar Craton, India: A Pan-African (491+/-11 Ma) Age of Diamondiferous Kimberlite Emplacement. Canadian Mineralogist (2000) Vol. Springer, Berlin, Heidelberg. White, J.S. Back cover photographs:-(anti-clockwise from top left) 1. Vdovykin, G.P. Sauer, J.R. (1982) Brazil, Paradise of Gemstones. 27th Annual Report of Geology and Natural Resources: 46. Geology and mineral resources of San Diego County, California. Shkodzinsky, V.S. Ges., Eur. Geological Survey of British Guiana Bulletin, 17. Klein-BenDavid, O., Izraeli, E.S., and Navon, O. Carlson, E.H. (1991) Minerals of Ohio: Ohio Department of Natural Resources, Bulletin 69, First Edition: 101. American Mineralogist, 101, 355-361.; Ogasawara, Y., Fukasawa, K., & Maruyama, S. (2002). 63-410), and miscellaneous observations on mineral products): 168, 169; Kunz, George Frederick (1905a), Gems, jewelers’ materials, and ornamental stones of California: California Division Mines Bulletin 37, 171 pp. Natural occurrence of pure nano-polycrystalline diamond from impact crater. Goeppert, H.R. Jingsui Yang, Zhongming Zhang, Xiangzhen Xu, Yuan Li, Jinyang Li, Yi Jia, hao Liu, and Dengzhu Ba (2010): Goldschmidt Conference Abstracts 2010. Patchen, A. D., Taylor, L. A., & Pokhilenko, N. (1997). Proceedings of the 7th International Kimberlite Conference, 1999, p.625-636. Matheys, F. G., (1990), The alluvial diamond deposits of the lower Vaal river between Barkly West and the Vaal-Harts confluence in the Northern Cape Province, South Africa. ; Feuchtwanger, L. (1872) A popular treatise on gems : in reference to their scientific value : a guide for the teacher of natural sciences, the jeweller, and amateur : together with a description of the elements of mineralogy, and all ornamental and architectural materials. Kvasnytsya, V., Wirth, R., Dobrzhinetskaya, L., Matzel, J., Jacobsen, B., Hutcheon, I., ... & Kovalyukh, M. (2013). : 42: 413-417; Kunz, G.F. & C.W. Overstreet, William C. (1967) The Geologic Occurrence of Monazite. Ureilites. ? (1922): Mineralogie de Madagascar, Tome I. Géologie-Minéralogie descriptive. Naturally occurring - Minerals occur in nature. Abstracts of the Lunar and Planetary Science Conference, volume 22, page 1439, (1991), Bulletin of the Imperial Institute - Geology and Mineral Resources of Kenya (1948) p297. Electronic state of carbon in carbonaceous chondrite meteorites. 10). : 44; Pemberton, H. Earl (1983), Minerals of California; Van Nostrand Reinholt Press: 54. Geochimica et Cosmochimica Acta: 58: 761-771. Williams, Alpheus F. (1932) The Genesis of the Diamond. (in Dutch). Russian Journal of Earth Sciences, 7, 1–45, doi:10.2205/2005ES000189; Grachev, A.F., Borisovsky, S.E., and Grigor'eva, A.V. 36, No. Geology. Journal of Metamorphic Geology, 34, 265-291. Generally, industrial diamonds are irregularly shaped anddefective.They are very important in modern metal processing and mining.Theyare naturally found in three varieties. Consider a diamond that has flat facets and sharp edges. & Kitajima, F. (2008). Diamond has a very high melting point of 4000°C which is 2.5 times hotter than the melting point of steel. i have to do a project and i needed to pick a mineral..i picked diamond and now i need to answer that...if anyone can help me wiht that because i odnt get it. ; Minerals 10, 18. Contributions to Mineralogy and Petrology, 26, 75-123.; Dampak perubahan lingkungan sungai terhadap kondisi sosial ekonomi petani di Kelurahan Bangkal Kecamatan Cempaka Kota Banjarbaru (Doctoral dissertation, Universitas Gadjah Mada). (2003) Fluid inclusions in diamonds: the Carbonatitic connection. Microstructures in Pyroxenes from the Martian Meteorites Zagami and the Achondrites Bishopville (Aubrite), Hammadah Al Hamra 064, and Jalanash (Ureilites). S. Mostefaoui, Ahmed El Goresy, P. Hoppe, P. Gillet & U. Ott (2001). Although light yellow tinting is frowned on, a deep yellow color renders the … Mineralogical evidence for the origin of diamond in ureilites. Mineralogy and Noble Gas Signatures of Desert Meteorite Shisr 007 (Ureilite), 5139.pdf. A. Diamantes do médio rio Jequitinhonha, Minas Gerais: qualificação gemológica e análise granulométrica - REM: R. Esc. Nano-Polycrystalline Diamond (or NPD) is a completely transparent, polycrystalline synthetic consisting of randomly oriented, very tightly bonded nanoscale-sized diamond crystallites. 2. Forms of carbon in the new Haverö ureilite of Finland. (2003): Journal of Metamorphic Geology 21, 425-437.; Erlich, E.I., and Hausel, D.W. (2002): Diamond Deposits: Origin, Exploration and History of Discovery. The Hamlyn Publishing Group Limited, 128 pages (page 101). In 8th International Kimberlite Conference, Extented Abstracts Vol., FLA0141. Meteoritics & Planetary Science, 40, 4, 609-625. du Plessis, J.H. (p. 16). Mineral inclusions in diamonds from the Panda kimberlite, Slave Province, Canada. Geologické výzkumy na Morave a ve Slezsku 18, 1, 35-38. Jinjie Yu, Pingan Wang, Jianping Huang, Hui Wang, and Xiaofeng Li (2006): Earth Science, Journal of China University of Geosciences 31(4), 520-526. London. Kunz, George Frederick (1896), Precious stones: Mineral Resources U.S., 1895: 896; Murdoch, Joseph & Robert W. Webb (1966), Minerals of California, Centennial Volume (1866-1966): California Division Mines & Geology Bulletin 189: 171. The Canadian Mineralogist Vol. The form… Izdatelstvo Akademii: Nauk, CCCP. (1985) Mineralen. Manufactured diamonds are all formed from carbon, which is really a mineral. Gübelin, E. and Wolgensinger, M. (1976) Edelstenen. Masaitis, V. L. (1998). Contributions to Mineralogy and Petrology, 151(2), 158-173. http://www.geologyontario.mndm.gov.on.ca/mndmfiles/afri/data/imaging/temp/2_57819/2_57819_10_DiamondDrillingReport_AkowLake2016.pdf, http://www.debeerscanada.com/files_2/victor_project/factsheet.html. Bruton, Eric (1978) Diamonds. Richmond, J.F. Inclusions are generally on the inside, and some might break the surface of the stone. Geochimica et Cosmochimica Acta 59 (1):115-160. : Mavlyanovite, a new mineral species from a lamproite diatreme, Chatkal Ridge, Uzbekistan. Dorothy M. Schlegal (1957) Gem Stones of the United States : USGS Bulletin 1042-G. Geochimica et Cosmochimica Acta, vol. 85, 2001 September. Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 839.; Hussak and Prior (1900) Mineralogical Magazine: 12: 244. Diamond and coesite in ultrahigh-pressure–ultrahigh-temperature granulites from Ceuta, Northern Rif, northwest Africa. The internal atomic structure of graphite and diamond, shown in Figures 3 and 5, explains the properties of the two minerals. Sauer, Jules Roger (1982) Brazil, Paradise of Gemstones. ; Nitze, Henry B. C., 1895, Monazite, and Monazite Deposits in North Carolina, Bulletin 9, North Carolina Geological Survey, pp. A variety of black bort from South Africa showing minute brilliant points possibly due to included diamonds. (Dec 2003). Journal of earth system science, 115(1), 161-183. Surv. Chew (Eds.) (1902) Gold and Diamonds in Indiana. Cairncross, B., Dixon, R. (1995) Minerals of South Africa. In XII International Conference «New Ideas in Earth Sciences» p77-78, 33rd International Geological Congress (2008) session AAA-11 Metallogeny of the Arctic region: Diamondiferous kimberlites of the East Eurorean Platform: Specific features. Diamonds, on the other hand, have only one type of atom: carbon. Inorganic - Minerals don't come from plants, animals, or other living organisms. Jones, A.P. Kamitani, M., Okumura, K., Teraoka, Y., Miyano, S., and Watanabe, Y. Gurney, J.J., Harris, J.W., and Rickard, R.S. Uitgeverij Artis, Brussel (in Dutch). Lithos: 70: 163-182. Revista de la sociedad española de mineralogia, 9, 205-206. First diamonds from placers in Primorie. Diamonds from the V. Grib pipe, Arkhangelsk kimberlite province, Russia. Reunert, Theodore (1893) Diamonds and Gold in South Africa. HIDAYAT, T., & Setiawan, I. Lindley, A.F., Capt. Fisenko, A.V. B. (2005): Diamondiferous kimberlites from the Garnet Lake http://www.portergeo.com.au/database/mineinfo.asp?mineid=mn948. 20, pp.96–98; Mikhno A, Korsakov A (2014) Immiscible sulfide and silicate melts in UHP gneisses from the Kokchetav Massif (Northern Kazakhstan). Diamonds are made of pure carbon in a crystallised form, although they often contain inclusions of other minerals and are an excellent refractor of light. Review (1985) 147, 415, 417.; Meteoritics 30 (1), 47-56. Report 2: 241-254; Kunz, George Frederick (1905a), Gems, jewelers’ materials, and ornamental stones of California: California Division Mines Bulletin 37, 171 pp. Few things in nature are absolutely perfect. Gemological Institute of America, 135 pp. Malkovets, V.G., Pokhilenko, L.N., and Pokhilenko, N.P. Djerfisherite in Kimberlites of the Kuoikskoe field as an indicator of enrichment of Kimberlite melts in chlorine. (2016). Journal of earth system science, 115(1), 161-183.; (1955) (A Treatise on the Diamond) Kristallgrafiya Almaza Redaktsiya Kommentarri Akadeika. Lithos, 196, 42-53. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences. 35,p p.587-595(1997). (2004). Earth and Planetary Science Letters: 18: 323-332. Investors Brief, Rex Diamond Mining Corp. Ltd.; http://users.pandora.be/Globaltrade/streetwire.html. Stroud, December, 2001. Diamond has a hardness of 10 on Mohs scale of mineral hardness, with 1 being the softest (talc) and 10 being the hardest. 114 pp., London: Murby & Co. Farrington, O.C. The most typical color used for Diamond jewelry is colorless. Hardness: 10 Mohs' scale, 56-115 Knoop hardness number (GPa), 10,000 Brooks identer scale. Also, lab-created diamonds in almost all of the cases do not have any imperfections since they’re created in controlled environments, and as stated above, they’re as real as the ones formed naturally. Jarnot, Bruce and Jarnot, Miranda (2004): "Gem Almandine from Colchester, Connecticut," in: abstracts of the 31st Rochester Mineralogical Symposium, April 15-18, 2004, pp 13-14. Ragozin, A.; Zedgenizov, D.; Shatsky, V.; Kuper, K.; Kagi, H. (2020) Deformation Features of Super-Deep Diamonds. R&M 73:11-12 pp 378-399 Wisconsin Mineral Locality Index, Cordua, W. (1998) Minerals of Wisconsin: Rocks and Minerals: 73 (6): 378 - 399. in abstracts of the 22nd IMA Meeting Melbourne p 129. Hayman, P., Kopylova, M., and Kaminsky, F. 2005. : 24: 677-680. & Pillinger, C. T. (1995). De Stefano, A., Lefebvre, N., & Kopylova, M. (2006). Subducted oceanic crust as diamond hosts revealed by garnets of mantle xenoliths from Nyurbinskaya, Siberia. A real diamond, when carefully dropped in a glass filled with clear water, will sink to the bottom due to its high density. The Mineralogical Record, 11(6), 351-360.; 1972. Alphen aan den Rijn: Atrium. Report 4, 410 pp. Marvin (1967a), Lonsdaleite, a new hexagonal polymorph of diamond. Breaking a mineral breaks its chemical bonds. Boyd and H.O.A. Minerals are not made or influenced by human activity. in abstracts of the 22nd IMA Meeting Melbourne p 136, Fetherston, J., Stocklmayer, S., Stocklmayer, V(2013): Gemstones of WA, Geological Survey of WA, Groom, F. (1896) Report of the Department of Mines for the Year 1895. 30 Kimberlite Pipe (Liaoning Province, North China Craton): Constraints on Diamond Potential. Viljoen, K.S., Harris, J.W., Ivanic, T., Richardson, S.H., Gray, K. (2014) Trace element chemistry of peridotitic garnets in diamonds from the Premier (Cullinan) and Finsch kimberlites, South Africa: Contrasting styles of mantle metasomatism. Mining Ann. Hutchison, M.T., Hursthouse, M.B., and Light, M.E. Boxer, G.L., Grice, J.D. Diamonds in lavas of the Tolbachik fissure eruption in Kamchatka. 406, No. (2013) Gemstones of Western Australia. (June 30, 1981). Report 4, 410 pp. Some diamonds have been found in the United States. Guthrie, G.D., Veblen, D.R., Navon, O., and Rossman, G.R. 7th edition, revised and enlarged, 834pp. Geochimica et Cosmochimica Acta 67 (24): 4823-4848. Mineralogicalcharacterization of the diamond of the alluvial placer from Icabaru River, Santa Elena de Uairén, Bolivar State, Venezuela. Volume III. Often, M. (1996): Diamanter i Norge ? Meteoritics & Planetary Science, 33(2), 349-359. European Journal of Mineralogy, 25(5), 825-834.; Space Science Reviews 10, #4, 483-510.; Vdovykin, G. P. (1970) Ureilites: Space Science Reviews 10(4): 483-510. Petrography of the carbonaceous, diamond-bearing stone “Hypatia” from southwest Egypt: A contribution to the debate on its origin. & M.G. Space Science Reviews 10, #4, 483-510. It is the hardest naturally-occurring mineral. Pratt,Joseph Hyde.,1933,Gems and Gem Minerals of North Carolina,American Mineralogist,Vol.18,No.4,April,1933, Pratt,Joseph Hyde.,1933,Gems and Gem Minerals of North Carolina:American Mineralogist,Vol.18,No.4,April,1933, Wilson,W.F and McKenzie,B.J,1978,Mineral Collecting Sites In North Carolina,Information Circular 24. Gondwana Research, 27(2), 459-485.; Shmelev V.R., Perevozchikov B.V., Moloshag V.P. ; Sierra Leone. area, west Greenland: exploration methodologies and petrochemistry, Workshop on Greenland ´s diamond potential, Danmarks og Grønlands Geologiske Undersøgelse Rapport 2005/68, 7-9 November 2005 in Copenhagen. World of Stone, 1, 11-20.; Doklady Earth Sciences, 422(7), 1065-1067; Grachev, A.F. Alam, I. 8th. Loz'ko, Y. Y. D. Bering - et al. Pronunciation Icon - Sound file Courtesy Photo Atlas of Minerals. Dana 7: I: 149.; 8th. Real argyle pink diamonds like any other diamond have radiolucent molecular structures. Report 4, 410 pp. 9, 124). They have a clear structure and chemical composition. Asoc. (1968) A descriptive catalog of the drift diamonds of the Great Lakes region, North America. ; Meteoritics, vol. The mineral halite, which is used as table salt, forms when water evaporates in a hot, shallow part of the ocean, leaving behind the salt it contained. Solids that are made in a chemistry lab don't count as minerals. London: Blackie & Son. New York: Knickerbocker Press. Diamond is considered a mineral, and individual diamonds in nature are individual mineral crystals. Science in China Series D: Earth Sciences, 41(1), 54-92. 49, 691-706. Chartwell Books, Inc., 80 pages (p. 18). (May 1996). Russell, S. S. & 7 others (2005). Blackwell Scientific, Cambridge, U.K. (2007): Mineral Resources Map of East Asia. Grossman, J. N. & Zipfel, J. ; Zedgenizov, D. A., Ragozin, A. L., Shatsky, V. S., Araujo, D., & Griffin, W. L. (2011). Abundances of Presolar Grains in Renazzo and Axtell: Implications for the Thermal Histories. Octahedral crystals, also dodecahedrons, cubes, tetrahedral. Chicago: Field Museum of Natural History Geology Leaflet 10. Pagel-Theisen, V. (1972) Diamanten-Fibel: Handbuch der Diamanten-Graduierung. Geological Survey of Japan. in Abstract Volume IAGR Conference Series No. Mr. Achimovich Interviewed, 03/02/1899, Western Mail newspaper (Perth) (1915), Gold and Diamonds. The Camafuca-Camazambo kimberlite pipe of Angola, the largest in the world. 53:305-309. (2013) Geochemistry of megacrystalline pyrope peridotites from the Udachnaya pipe, Siberian craton. Carlson, S. & G. Adams (1998) The diamondiferous Six-Pak Ultramafic Lamprophyre Diatreme, Kenosha, Wisconsin, U.S.A.: 43rd. 3d models and HTML5 code kindly provided by. Mineralogical Magazine, 58(392), 490-493.; Ragozin, A.; Zedgenizov, D.; Shatsky, V.; Kuper, K.; Kagi, H. (2020) Deformation Features of Super-Deep Diamonds. abs.]. Hwang, S.-L., Shen, P., Chu, H.-T., Yui, T.-F., Liou, J.G., Sobolev, N.V., and Shatsky, V.S. Het dagelijkse leven in de "Diamond Square Mile". Diamond is the best known thermal conductor (heat transfer) among naturally occurring substances. Lower mantle diamonds from Rio Soriso (Juina area, Mato Grosso, Brazil). Survey of circumstellar grains in the unique circumstellar carbonaceous chondrite Acfer 094. (2007): Mineral Resources Map of East Asia. www.craterofdiamondsstatepark.com; American Mineralogist, Volume 85, pages 420–429, 2000; Rocks and Minerals, (1988) 63:104-125; Min News (1992) 8:3 pp 1,4,7; Rocks and Minerals, (1989) 64:308-310, U.S. Geological Survey. Diamond, a mineral composed of pure carbon. Howard Coopersmith, Vered Toledo, John Ward, Michiel De Wit, R Spaggiari, Emmanuel Fritsch: "Geology and Exploration of Gem Deposits at Mt. Galimov, E. M., Palazhchenko, O. V., Verichev, E. M., Garanin, V. K., & Golovin, N. N. (2008). Mining Annual Review (1985): 516.; A.V. Contributions to Mineralogy and Petrology (Historical Archives), V 110, N 1, March 1992, pp. (2014) South African Diamonds, Rocks & Minerals Diamond special issue 89(1) 76-86. 1, pp. Placer PGE minerals from the Filippa clinopyroxenite-dunite massif (Kamchatka). Vasilenko, L.G. Diamond’s characteristic chemical composition and crystal structure make it a unique member of the mineral kingdom. Rao, N. C., & Srivastava, R. K. (2009). Warwick – Tweed Heads Exploration Data Package Vol. Lithos, 112, 660-674.; Stachel, T., Harris, J., Aulbach, S., & Deines, P. (2002). Geological Survey of Victoria Bulletin No. Dunn, E.J.,(1913). Tadao Nishiyama, Hiroaki Ohfuji, Ukyo Nishi, Kazuki Harada, Kousuke Fukuba (2018) Origin of lowest temperature microdiamond in a metapelite from Nishisonogi, western Japan. Kunz, George Frederick (1905a), Gems, jewelers’ materials, and ornamental stones of California: California Division Mines Bulletin 37, 171 pp. Geological Publishing House (Beijing), 289 pp. Open-pit diamond mines are typically designed to recover as little as 100,000 to more than 10 Mt of ore per year. Gübelin, E. and Wolgensinger, M. (1976) Edelstenen. Mudrey (1981) The potential for diamond-bearing kimberlite in northern Michigan and Wisconsin: USGS Circular 842, 15 p. Cannon, W.F. Diamond Mining Along The Coast Of Namibia. Navon, O. (2006): Geology of Ore Deposits 48(4), 326-334. (p. 124). Tappert, R., Stachel, T., Harris, J. W., & Shimizu, N. (2005). Short-cut icons Legend; B: Valid Species (Bold) - All Minerals that are IMA approved or were considered valid prior to 1959 are in bold type. ]), Kyaukmedaung (Kyaukmedaung-Shwechaung area), Southern Coastal Mines (MA1; Mining Area 1), Jiddat al Harasis meteorite 054 (JaH 054), Mezö-Madaras meteorite (Fekete; Madaras; Maros; Mesö-Madarasz; Mezoe-Madaras; Weiler [NHM Cat. 133-138. with Programs: 11-12. Ureilites. Milesi, J. P., Toteu, S. F., Deschamps, Y., Feybesse, J. L., Lerouge, C., Cocherie, A., ... & Nicol, N. (2006). (1998): Evaluation de l’inventaire des ressources minérales de Guinée – Etude.- Direction nationale de la recherche géologique et minière (Conakry), BGR (Hannover).- Hannover: Bundesanstalt für Geowissenschaften und Rohstoffe.- 109 + 51 p.: ill. + atlas (12 cartes: en coul. , 112, 880-885. ; Kononova, V.A., Golubeva, Y.Y., Bogatikov,,! With descriptions of the Geological Society of South Africa showing minute brilliant points due! 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( 1911 ) the Potential for diamond-bearing kimberlite in Northern Michigan and:... ( Juina area, 11/06/1915, Gibb-Maitland, a, L.O weak birefringence.! Concept of ilmenite as an abrasive and in cutting and grinding applications 43 ( Supplement ): de!