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金矿矿石手标本-黄铁矿、黄铜矿、方铅矿、闪锌矿
sphalerite 英 ['sfæləraɪt] 美 ['sfæləˌraɪt] 名词. 【矿】闪锌矿
Granite porphyry ['pɔ:fərɪ ] 花岗斑岩
granite 英 ['ɡrænɪt] 美 ['ɡrænɪt] 花岗岩
porphyry ['pɔ:fərɪ ] 美['pɔrfərɪ ] n斑岩,波菲利
quartz porphyry ['pɔ:fərɪ ] 石英斑岩
Granite is a light-colored igneous rock with grains large enough tobe visible with the unaided eye. It forms from the slow crystallization ofmagma below Earth's surface. Granite is composed mainly of quartz and feldspar with minor amountsof mica, amphiboles, and other minerals.
The mineral-bodies of the two mineral deposits are mainly existed in the contacting zone of granite-porphyry andadjoining rock.
Py-pyrite ['paɪraɪt]黄铁矿;
Gn-galena [ɡəˈli:nə]方铅矿 ;方铅矿
Sp-sphalerite ['sfæləraɪt];闪锌矿
Ccp-chalcopyrite英 [,kælkə(ʊ)'paɪraɪt] 美 [,kælkə'paɪraɪt].黄铜矿
Aluminum Corporation of China Limited (CHALCO)中国铝业
[ə'luːmɪnəm]
引自胶东蚀变岩型金矿金矿物微区地球化学特征胶东蚀变岩型金矿金矿物微区地球化学特征.pdf
结晶学与矿物学实验及肉眼鉴定指导书-骆少勇。感谢老师给我一本他自己编著的书籍。
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