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Geochemical Characteristics of the Yanqian High-F Granite and Its Relationship with the New-Type Bamianshan Fluorite Deposit in Northwest Zhejiang Province
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摘要
ft; WIDOWS: 2; TEXT-TRANSFORM: none; BACKGROUND-COLOR: rgb(244,244,244); TEXT-INDENT: -5px; DISPLAY: inline !important; FONT: 12px/22px Arial, 宋体; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(36,36,36); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px"> ft; PADDING-BOTTOM: 0px; WIDOWS: 2; TEXT-TRANSFORM: none; BACKGROUND-COLOR: rgb(244,244,244); TEXT-INDENT: -5px; MARGIN: 0px; PADDING-LEFT: 0px; PADDING-RIGHT: 0px; FONT: 12px/22px Arial, 宋体; WHITE-SPACE: normal; ORPHANS: 2; LETTER-SPACING: normal; COLOR: rgb(36,36,36); WORD-SPACING: 0px; PADDING-TOP: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px" id=EnChDivSummary name="EnDivSummary">The Bamianshan super-large fluorite deposit in Zhejiang Province is a new-type fluorite deposit.Petrological and geochemical studies undertaken in this paper reveal that the Yanqian granite is rich in volatile components,with high-F and SiO2,and low CaO,TiO2 and P2O5.The Bamianshan fluorite orebodies in the ore field are located close to the Yanqian granite spatially and temporally.The granite not only offers ore-forming element F for the Bamianshan ore field,but also provides space for ore precipitation after the magma invaded.

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