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The historical geography of tin mining, Seward Peninsula, Alaska /Hawn, Barbara Jean. January 1956 (has links)
Thesis (M.S.)--Oregon State College, 1956. / Typescript. Mounted photographs. Includes bibliographical references (leaves 51-54). Also available on the World Wide Web.
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Försök til en chemisk och metallurgisk afhandling om tennets och dess malmers beskaffenhetGadd, Pehr Adrian, Nordenskiöld, August, January 1900 (has links)
Dissertation (doctoral)--Åbo akademi, 1772. / At head of title: I.J.N. Reproduction of original from Kress Library of Business and Economics, Harvard University. Goldsmiths'-Kress no. 10859.3-1.
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An evaluation of investments in tin or alternative projects on the future foreign exchange earnings of BoliviaBurke, Thomas Edward, January 1968 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1968. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliography.
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Reclamation of land disturbed by tin miningTanavud, Charlchai Unknown Date (has links)
No description available.
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Reclamation of land disturbed by tin miningTanavud, Charlchai Unknown Date (has links)
No description available.
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The geology and alteration-mineralisation of the Gamigab Tin Prospect, Damaraland, NamibiaWalraven, Felix Caspar January 1990 (has links)
The stratigraphy at the Gamigab Sn prospect consists of two mainly schistose units separated by a thick marble unit which have been assigned to the Orusewa, the Karibib and the Kuiseb Formations respectively. Four phases of folding affected the lithologies with the south-south-west trending F2 folds defining the main structures in the region. The area underwent low grades of metamorphism. Temperatures were in the range 420° to 500°C and pressures less than 2 kbars. The effects of contact metamorphism are seen in the south-east and south-west. Regional metamorphism outlasted the deformation and contact metamorphism started late during deformation. Two Karoo-age intrusions penetrated the metasediments north of the mineralisation. One is an altered porphyry plug and the other is a weathered dolerite plug, the latter containing xenoliths of undeformed Karoo sediments. Cassiterite is hosted within east-west trending quartz veins that cross-cut previously altered schistose country rocks. The alteration types include sericitisation, tourmalinisation, carbonatisation and ferruginisation. Preliminary Rb/Sr dating on muscovite from the alteration zone suggests an age of 509 ± 11 Ma. Breccias of probable hydrothermal origin are spatially associated with the mineralisation. These hydraulic breccias occur in antiformal structures within the marble and developed in response to a sudden pressure release due to a build up of fluids at the contact between the schistose Orusewa and carbonate Karibib Formations.
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Development of rehabilitation techniques to reclaim tin-mined lands for low-cost housing in MalaysiaIsmail Said. January 1985 (has links)
Call number: LD2668 .T4 1985 S24 / Master of Landscape Architecture
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