斑岩铜矿
地质学
矿化(土壤科学)
地球化学
矽卡岩
铜
成矿作用
火山
多金属置换矿床
陆上
热液循环
古生物学
流体包裹体
冶金
闪锌矿
黄铁矿
材料科学
土壤水分
土壤科学
作者
Kezhang Qin,Shunsō Ishihara
标识
DOI:10.1080/00206819809465223
摘要
Why no porphyry copper deposit has been discovered thus far in the islands of Japan remains a perplexing question. A new attempt is made to address this question in this paper, with eight prerequisites for the formation of porphyry copper deposits being presented. The authors then review certain unfavorable conditions for formation of porphyry coppers, discussing especially the spacetime relationship between Kuroko-type and porphyry copper-type deposits, and suggest that there should be some inherent linkage between them. The possible existence of porphyry copper in the islands of Japan cannot be ruled out. Indeed, in some uplifted areas in the subaerial volcanic belt, porphyry coppers probably were formed and will be found in the deeper parts of the alteration zone of some high-sulfidation-type epithermal Au deposits or vein Pb-Zn-Cu deposits, or even at the periphery of some skarn Pb-Zn-Cu deposits.
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