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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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《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

机译：高温岩浆流体和石灰石之间的相互作用解释了瑞典中部的巴斯德型 REE矿床
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

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