棠甘山锰矿床属于典型的沉积-岩浆气液叠加型层控锰矿床。
The Tangganshan manganese ore deposit is a typical sedimentary-magmatic hydatopneuma-togenic superimposed manganese ore deposit.
煌斑岩岩浆晚期残余气液与成矿流体组成相近、沉淀次序相同，表明它们可能有成因联系。
The last remain fluid of lamprophyre magma is similar to metallogenetic fluid in composition and precipitating sequence, showing their genetic relationship.
该系统包括“三大”成矿体系，即：幔源岩浆体系、深穿透断裂构造体系、含矿气液流体体系。
The mineralization system has three giant system, namely mantle magmatic system, penetrability deep-fault and ore- bearing pneumato-hydrothermal system.
岩浆火山通道为主要气源体气藏的形成分成岩浆喷发前、岩浆喷发、火山通道埋藏与成藏三个阶段。
The reservoir based on magma volcanic conduit also has three phases: before magma effusion, effusion and volcanic conduit bury and reservoir-forming.
琼北第四纪火山区分布着为数众多、大小不一的射气岩浆喷发成因的低平火山口。
Maars of various scales produced by phreatomagmatic eruption are widely distributed in the Quaternary volcanic region of the Northern Hainan Island.
综合国内外研究资料并结合笔者的研究成果 ，评述了幔源岩浆去气形成富二氧化碳含金流体的可能性和现实性。
The reality and possibility of the formation of CO 2 rich and Au bearing fluids by mantle derived magmatic degassing are discussed.
综合国内外研究资料并结合笔者的研究成果 ，评述了幔源岩浆去气形成富二氧化碳含金流体的可能性和现实性。
The reality and possibility of the formation of CO 2 rich and Au bearing fluids by mantle derived magmatic degassing are discussed.
应用推荐