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通过研究热液蚀变,1975年在葡萄牙南部发现了萨尔加丁纽铜矿床。本文的目的是想论证这是一种新的矿床类型,并描述其热液蚀变。了解和利用与海底喷气矿床伴生的热液蚀变,可有效地指导块状硫化物矿床的寻找。这个矿床位于伊比利亚黄铁矿带西南出露有浅变
By studying hydrothermal alteration, the Sargadinian New-Cu deposit was discovered in southern Portugal in 1975. The purpose of this paper is to demonstrate that this is a new type of deposit and describes its hydrothermal alteration. Understanding and utilizing the hydrothermal alteration associated with the submarine jet deposits can effectively guide the search for massive sulfide deposits. This deposit is located in the Iberian pyrite belt southwest there is a slight change