Organic geochemistry and fluid inclusions of a fluorite deposit, Asturias, Spain

机译：西班牙阿斯图里亚斯萤石矿床的有机地球化学和流体包裹体

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The mineral paragenesis of the vein and stratiform fluorite-barite ore bodies is related to the evolution of the Triassic sequence in the N. Asturias Basin, and the underlying Namurian Limestones. The fluid inclusions show diverse types within the overall compositional range: Th 120-150 deg, salinity of 4 to 23 wt

机译：矿脉和层状萤石-重晶石矿体的矿物共生关系与北阿斯图里亚斯盆地三叠纪层序及其下的那慕尔石灰岩的演化有关。流体包裹体在整个组成范围内显示出多种类型：Th 120-150 deg，盐度为4至23 wt

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《Biennial SGA meeting;Quadrennial IAGOD symposium》|1999年|p.279-282|共4页
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B.Spiro; F.Tornos; A.Kim;
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Organic geochemistry and fluid inclusions of a fluorite deposit, Asturias, Spain

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