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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書目名稱Geology of Tin Deposits in Asia and the Pacific影響因子(影響力)

書目名稱Geology of Tin Deposits in Asia and the Pacific影響因子(影響力)學(xué)科排名

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書目名稱Geology of Tin Deposits in Asia and the Pacific網(wǎng)絡(luò)公開度學(xué)科排名

書目名稱Geology of Tin Deposits in Asia and the Pacific被引頻次

書目名稱Geology of Tin Deposits in Asia and the Pacific被引頻次學(xué)科排名

書目名稱Geology of Tin Deposits in Asia and the Pacific年度引用

書目名稱Geology of Tin Deposits in Asia and the Pacific年度引用學(xué)科排名

書目名稱Geology of Tin Deposits in Asia and the Pacific讀者反饋

書目名稱Geology of Tin Deposits in Asia and the Pacific讀者反饋學(xué)科排名

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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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