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Titlebook: Geology of Tin Deposits in Asia and the Pacific; Selected Papers from Charles S. Hutchison Conference proceedings 1988 United Nations New Y

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發(fā)表于 2025-3-21 19:47:00 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Geology of Tin Deposits in Asia and the Pacific
副標(biāo)題Selected Papers from
編輯Charles S. Hutchison
視頻videohttp://file.papertrans.cn/384/383395/383395.mp4
圖書封面Titlebook: Geology of Tin Deposits in Asia and the Pacific; Selected Papers from Charles S. Hutchison Conference proceedings 1988 United Nations New Y
描述This volume represents an edited selection of papers presented at the International symposium on the geology of tin deposits held in Nanning City in October 1984. It documents a great advance in our knowledge of tin deposits, particularly of the People‘s Republic of China. Details are presented in English for the first time on the major tin-polymetallic sulphide deposits of Dachang and Gejiu, which bear similarities to the deposits of Tasmania, but are little known to the geological community outside of China. The publication of this volume was sponsored by the United Nations ESCAP Regional Mineral Resources Development Centre (RMRDC), now a Regional Mineral Resources Development Project (RMRDP) within ESCAP. The Centre had previously published a report on the Symposium in Nanning City and the following field trip to the Dachang tin-polymetallic sulphide deposit of Guangxi, entitled "Report on the International Symposium on the Geology of Tin Deposits: Nanning and Dachang, China, 27 October - 8 November 1984". It is my privilege to acknowledge the help provided by Dr. J. F. McDivitt and Dr. H. W. Gebert, co-ordinator of ESCAP-RMRDC.
出版日期Conference proceedings 1988
關(guān)鍵詞Niob; Tantal; Titan; geochemistry; geology; metals; mineral; mineralogy; paper; structure; tin
版次1
doihttps://doi.org/10.1007/978-3-642-72765-8
isbn_softcover978-3-642-72767-2
isbn_ebook978-3-642-72765-8
copyrightUnited Nations New York 1988
The information of publication is updating

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https://doi.org/10.1007/978-3-319-78396-3 beryl, tourmaline and danalite, (V) Late stage chlorite + calcite + pyrite/marcasite..The predominant mineral residence of tin in the early skarn stages is as tin-bearing silicates, stanniferous andradite (stage I), stanniferous Fe-amphibole (stages IIA and IIB) and malayaite (stage III), although
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Digital Gaze and Visual Experience mineralised with copper and base metals..The granites of the Main Range in Malaysia provide a total contrast to those of the Andes in that they do not form super-units, they are invariably true granites and are mineralised with tin..The granitoids of the Eastern Belt in Malaysia are intermediate in
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Conference proceedings 1988ort on the International Symposium on the Geology of Tin Deposits: Nanning and Dachang, China, 27 October - 8 November 1984". It is my privilege to acknowledge the help provided by Dr. J. F. McDivitt and Dr. H. W. Gebert, co-ordinator of ESCAP-RMRDC.
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itled "Report on the International Symposium on the Geology of Tin Deposits: Nanning and Dachang, China, 27 October - 8 November 1984". It is my privilege to acknowledge the help provided by Dr. J. F. McDivitt and Dr. H. W. Gebert, co-ordinator of ESCAP-RMRDC.978-3-642-72767-2978-3-642-72765-8
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Genetic Modelling of Greisen-Style Tin Systemspward passage of post magmatic fluids which leach tin from the lower feldspathic horizon and precipitate cassiterite in the sericitic zone. This model currently holds dominance over concepts which invoke fluids derived from unspecified deeper sources ultimately concentrating in structural traps bene
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