Banpo antimony deposit is a typical fracture - controlling and hydrothermal fluid filling deposit.

半坡锑矿床是典型的断裂控矿,热液充填型矿床.

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The ore - genesis belonging to deep resource hydrothermal fluid cryptoexplosi on metasomatism was put forward.

提出银矿床属深源热流体隐爆 - 交代型矿床.

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Subvocanics is the final carrier of hydrothermal fluid of magmatism thus is the prospecting target.

次火山岩是岩浆体系分熔侵入-喷发过程中最后集中成矿热液的载体,具有直接的找矿意义.

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The studies show that U - bearing pneumato hydrothermal fluid is a reductive and acidic medium.

研究表明,含铀气成热液为还原性质的酸性介质,铀在其中主要以形式迁移.

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