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Fluid inclusion geochemistry and rare earth element distributions in the Oka carbonatite, Quebec.

机译:魁北克奥卡碳酸盐岩中的流体包裹体地球化学和稀土元素分布。

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摘要

Two types of primary, aqueous fluid inclusions are present in monticellite, apatite and calcite from the Oka carbonatite: (1) liquid-vapour (LV) inclusions, and (2) liquid-vapour-halite (LVH) inclusions. LV inclusions have salinities of 4.3 to 24.7 wt.% and densities of 0.75 to 1.04 g/cm$sp3,$ and homogenize to the liquid phase between 95 and 435$spcirc$C. The observed crystallization sequence of the host minerals was monticellite-apatite-calcite. Systematic variation in homogenization temperatures, salinities and densities of LV inclusions, combined with the crystallization sequence, suggests that type 1 fluids evolved from high to low salinity and probably from high to low temperature. The minimum pressure at which monticellite, apatite and calcite crystallized is estimated to have been about 7 to 10 kb. The nature of the trapped minerals in the inclusions and data from leachate and decrepitate analyses indicate that the fluids in the inclusions are principally composed of Na, Cl and S (sulphate?), and contain Ca, Mg, K, Fe, Si (silicate?) in subordinate amounts. LV fluid have high Ca/Na, K/Na, and Mg/Na ratios and lower Fe/Na ratios than LVH fluid. REE concentrations and La/Lu ratios of apatite increase with decreasing inclusion abundance in apatite and LV inclusion-rich apatites have higher REE concentrations but lower La/Lu ratios than LVH inclusion-rich apatites. This suggests that hydrothermal fluids may have removed LREE from the magma, and that the chemistry of fluids may have had an influence on REE distribution in the magma. The rare earth elements substitute for Ca in the apatite structure through the coupled substitution: $m REEsp{3+}+Sisp{4+}o Casp{2+}+Psp{5+}.$ Saline, aqueous, hydrothermal fluids were present during crystallization of monticellite, apatite and calcite from some of the carbonatite magmas. (Abstract shortened by UMI.)Dept. of Geology and Geological Engineering. Paper copy at Leddy Library: Theses u26 Major Papers - Basement, West Bldg. / Call Number: Thesis1993 .L588. Source: Masters Abstracts International, Volume: 32-02, page: 0564. Adviser: I. M. Samson. Thesis (M.Sc.)--University of Windsor (Canada), 1993.
机译:Oka碳酸盐岩的蒙脱石,磷灰石和方解石中存在两种主要的含水流体包裹体:(1)液态蒸气(LV)包裹体,和(2)液态蒸气-卤石(LVH)包裹体。 LV夹杂物的盐度为4.3至24.7 wt。%,密度为0.75至1.04 g / cm 2 / sp 3,并且在95至435 / sp C之间均化为液相。观察到的主体矿物的结晶顺序是蒙脱石-磷灰石-方解石。 LV夹杂物的均质温度,盐度和密度的系统变化,再加上结晶顺序,表明1型流体从高盐度演化为低盐度,并可能从高温演化为低盐度。蒙脱石,磷灰石和方解石结晶的最小压力估计约为7至10 kb。夹杂物中捕获的矿物的性质以及渗滤液和碎屑分析的数据表明,夹杂物中的流体主要由Na,Cl和S(硫酸盐?)组成,并且包含Ca,Mg,K,Fe,Si(硅酸盐) ?)的下级金额。 LV流体比LVH流体具有较高的Ca / Na,K / Na和Mg / Na比,并且具有较低的Fe / Na比。磷灰石的REE浓度和La / Lu比值随着磷灰石中夹杂物丰度的降低而增加,而富含LV夹杂物的磷灰石比LVH富含夹杂物的磷灰石具有更高的REE浓度,但La / Lu比却较低。这表明热液可能已经从岩浆中去除了LREE,并且流体的化学性质可能对岩浆中的REE分布产生了影响。稀土元素通过耦合置换来代替磷灰石结构中的Ca:$ rm REE sp {3 +} + Si sp {4 +} 到Ca sp {2 +} + P sp {5+ }。从某些碳酸盐岩浆岩中蒙脱石,磷灰石和方解石结晶期间,存在盐水,水热流体。 (摘要由UMI缩短。)地质与地质工程学院。莱迪图书馆的纸质副本:论文主要论文-西楼地下室。 /电话号码:Thesis1993 .L588。资料来源:国际硕士摘要,第32卷,第0564页。顾问:萨姆森(I. M. Samson)。论文(理学硕士)-温莎大学(加拿大),1993年。

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    Liu Weining.;

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