SIGNIFICATION OF QUANTITATIVE ANALYSIS OF FLUID INCLUSIONS IN MAGMATIC HYDROTHERMAL DEPOSITS

机译：岩浆水热沉积物中流体包裹物定量分析的键入

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There is no doubt that the quantitative analysis of fluid inclusions would promote the quantitative study of the fundamental geochemistry conditions of the ore genesis, such as the temperatures, pressures, composition and the density of ore-forming fluids and the precipitation mechanism of ore minerals. Besides, the the economic parameters, including bulk ore grade, bulk metal ratios and total metal content can also be estimated quantitatively.

机译：毫无疑问，流体夹杂物的定量分析将促进矿石成因的基本地球化学条件的定量研究，例如矿石矿物质的温度，压力，组成和密度，矿石矿物质的沉淀机制。此外，还可以定量估算包括散装矿石等级，散装金属比和总金属含量的经济参数。

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《Asia Current Research on Fluid Inclusion Meeting》|2014年|1 CD-ROM|共2页
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Zeng G.P.;
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1. Formation and evolution of multistage magmatic-hydrothermal fluids at the Yulong porphyry Cu-Mo deposit, eastern Tibet: Insights from LA-ICP-MS analysis of fluid inclusions [J] . Chang Jia, Li Jian-Wei, Audetat Andreas Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society . 2018,第期

机译：玉龙斑岩铜钼矿床，东藏玉龙斑岩 - 水热流体的形成与演化：La-ICP-MS分析流体夹杂物的见解
2. Formation of a Magmatic-Hydrothermal Ore Deposit: Insights with LA-ICP-MS Analysis Of Fluid Inclusions [J] . Andreas Audetat, Detlef Gunther, Christoph A. Heinrich Science . 1998,第5359期

机译：岩浆热液矿床的形成：流体包裹体LA-ICP-MS分析的见解
3. Compositions of magmatic hydrothermal fluids determined by LA-ICP-MS of fluid inclusions from the porphyry copper-molybdenum deposit at Butte, MT [J] . Rusk BG, Reed MH, Dilles JH, Chemical geology . 2004,第1a4期

机译：通过LA-ICP-MS测定岩浆热液的组成，该岩浆来自MT的斑岩铜钼矿床
4. SIGNIFICATION OF QUANTITATIVE ANALYSIS OF FLUID INCLUSIONS IN MAGMATIC HYDROTHERMAL DEPOSITS [C] . Zeng G.P. Asia Current Research on Fluid Inclusion Fifth Meeting . 2014

机译：岩浆热液沉积物中流体包裹体定量分析的意义
5. Origin of the Boleo copper-cobalt-zinc deposit, Baja California Sur, Mexico: Implications for the interaction of magmatic-hydrothermal fluids in a low-temperature hydrothermal system. [D] . Conly, Andrew George. 2003

机译：墨西哥下加利福尼亚州苏里南的Boleo铜钴锌矿床的起源：岩浆-热液在低温热液系统中的相互作用。
6. Interaction between high-temperature magmatic fluids and limestone explains ‘Bastnäs-type’ REE deposits in central Sweden [O] . Fredrik Sahlström, Erik Jonsson, Karin Högdahl, -1

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7. Trace elements in fluid inclusions of sediment-hosted gold deposits indicate a magmatic-hydrothermal origin of the Carlin ore trend [O] . Simon J.E. Large, Edine Y.N. Bakker, Philipp Weis, 2016

机译：沉积物托管金沉积物的流体夹杂物中的微量元素表明了Carlin矿石潮流的岩石 - 热热源

SIGNIFICATION OF QUANTITATIVE ANALYSIS OF FLUID INCLUSIONS IN MAGMATIC HYDROTHERMAL DEPOSITS

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