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Phase reaction in the systems MgO-SiO₂-MgF₂, MgO-GeO₂-MgF₂ and MgO-GeO₂-Mg(OH)₂ /Lyon, Stephen Reed. January 1968 (has links)
Thesis (Ph. D.)--Ohio State University, 1968. / Includes vita. Includes bibliographical references (leaves 138-145). Available online via OhioLINK's ETD Center.
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A study of the mineralogy of selected cretaceous and tertiary kaolins of central and eastern GeorgiaFriddell, Michael Steven 12 1900 (has links)
No description available.
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Electro-osmotic dewatering of mineral ultrafinesGrant, Christine Sharon 05 1900 (has links)
No description available.
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Geochemistry of the Scotia nickel deposit in relation to exploration /Barry, John Michael. January 1974 (has links) (PDF)
Thesis (Ph.D.) -- University of Adelaide, Dept. of Economic Geology, 1974. / Original drawings in box.
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The preparation of certain inorganic and organic compounds which may be of use in mineralogical separationsBlack, Clarence Jay. January 1928 (has links) (PDF)
Thesis (M.S.)--University of Missouri, School of Mines and Metallurgy, 1928. / The entire thesis text is included in file. Typescript. Can find no evidence of student graduating with a Master's Degree in the "1874-1999 MSM-UMR Alumni Directory or in any of the annual catalogs. Title from title screen of thesis/dissertation PDF file (viewed Sept. 14, 2009). Includes bibliographical references (p. 22).
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Phase reaction in the systems MgO-SiO₂-MgF₂, MgO-GeO₂-MgF₂ and MgO-GeO₂-Mg(OH)₂ /Lyon, Stephen Reed January 1968 (has links)
No description available.
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Precious metal mineralization associated with the Coed-y-Brenin porphyry copper system, North WalesMiller, Owen David William January 1993 (has links)
The Coed-y-Brenin system is a diorite-hosted porphyry copper deposit of early Ordovician age (Tremadoc) situated on the south eastern side of the Harlech Dome: a thick sequence of Cambrian and Ordovician sediments and volcaniclastics that were subject to greenschist facies metamorphism during the Caledonian Orogeny. The copper mineralization occurs as disseminations, coatings on hairline fractures and in late-stage quartz-sulphide-calcite veinlets. Pyrite and chalcopyrite are the main opaque phases but sulphosalts, tellurides and electrum are also present. The copper mineralization is largely confined to the diorite and micro-tonalite dykes and sills associated with the Rhobell Fawr Volcanic centre. This study has shown that epithermal style precious-metal mineralization is also developed in the Coed-y-Brenin area in the shales and siltstones of the Maentwrog and Ffestiniog Flags Formations. It is characterised by pyritization, sericitization and silicification. The gold and silver occur as electrum in fractures and also as tellurides in late stage quartz-pyrite veins. Both styles of mineralization share a close spatial association and are characterised by propylitic and phyllic alteration. Argillic and potassic assemblages are not developed. Geochemical analysis of mineralized and unmineralized material has shown that the diorite-hosted mineralization is enriched in Cu, Au and Ag and depleted in Zn while the epithermal mineralization displays enrichments in Au, Ag, As, Sb and the base metals. Rb:Sr ratios increase with increasing alteration in both styles of mineralization. Sulphur isotope studies have shown that both styles of mineralization have a common, probably magmatic, sulphur source. Fluid inclusion data and 0 and H isotope studies indicate that following magma emplacement and development of the porphyry copper mineralization a low temperature-low salinity meteoric hydrothermal system was established. Fluid inclusion data and 0 and H isotope studies indicate that following magma emplacement and development of the porphyry copper mineralization a low temperature-low salinity meteoric hydrothermal system was established. This was responsible for the late-stage quartzsulphide-calcite veins in the diorites and for all the sediment-hosted mineralization. The association between epithennal and porphyry deposits has become apparent in recent years but the Coed-y-Brenin system is unusual due to its Lower Palaeozoic age and because both styles of mineralization are developed at the same structural level. This study of the Coed-y-Brenin porphyry system demonstrates the potential for the development and preservation of epithermal mineralization in porphyry systems and also in older orogenic belts.
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Atomic substitution in the tetrahedrite-tennantite seriesBraun, Gerald Eugene, 1945- January 1969 (has links)
No description available.
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A thermochemical study of alunite and copper-arsenic sulfosalt depositsKnight, Jerry Eugene, 1951- January 1976 (has links)
No description available.
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Experiments in the vapour transport of SnO2 and MoS2.Beaudry-Sizgoric, Marthe. January 1968 (has links)
No description available.
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