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- W2912856952 abstract "Mamuju is a Miocene volcanic complex and become thelocation of the exploration of radioactive and rare earthelements. These area composed by basaltic and volcanicrocks up to intermediate with ultra potassic and soshonitic afinity. Magmatism processes in this area is a multi-phase process, there by producing a hydrothermal flows through rock porosity and fracturation zone. Hydrothermal fluid interacts with the rock side. Hydrothermal process is very influential volcanic central area of and areas with intensive fracturation. The rocks in these areas experiencing strong alteration to produce a very thick layer of soil, and in some places formed is very intensive mineralization and sulfidation and oxidation. Alteration encountered in the form of the potassic alteration minerals such as biotite paragenesis, actinolite and plagioclase, and formed titanite and adularia. Mineralization and levels of radioactive elements and rare earth elements have a higherconcentration on the fracture-fracture and the autoclastic breccia." @default.
- W2912856952 created "2019-02-21" @default.
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- W2912856952 date "2017-09-28" @default.
- W2912856952 modified "2023-09-26" @default.
- W2912856952 title "Implication of Hydrothermal Process on Radioactive and Rare Earth Element Enrichment in Mamuju, West Sulawesi." @default.
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