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中国东部沿海和西藏南部广泛分布有中、新生代的花岗岩类岩石。为了研究它们H-O同位素体系的纬度和高度效应,我们首先研究了现代大气降水δD,δ~(18)O值的高度和纬度效应。在此基础上,我们研究了西藏拉萨-亚东地带花岗岩类岩石中羟基矿物的δD值。它们具有明显的高度效应。根据黑云母δD值计算出来的西藏高原在20—40Ma期间的年平均隆起速度为0.1mm。中国东部沿海燕山晚期晶洞花岗岩全岩δ~(18)O,δD值具有明显的纬度效应。每个岩体中δ~(18)O-δD值之间的负相关关系代表在热水-岩石相互作用体系中ω/r比相同条件下温度与岩石δ~(18)_O,δD值的关系。 相似文献
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The H and O isotope compositions of 41 whole rocks and 24 separated minerals of theNianzishan miarolitic alkaline granite and 3 local meteoric water samples have been meas-ured. The results indicate that the meteoric-hydrothermal convective system might have beendeveloped in this stock. The distributions of δ~(18)O values of whole-rock samples formed anapproximateIy δ~(18)O contours with the characteristic of kighest values in the midst and de-creasing toward the outer zones. The water/rock ratio (W/R) contours were also calculated.This phenomenon might have common significance for stocks or plutons. 相似文献
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Multi-constraints are used in this paper to discuss the ΣCO_2 source in oreforming hydrothermal solution of granite-type uranium deposit in South China. The studies show that highly acidic and uraniferous granitic magma cannot produce the fluid rich in ΣCO_2. Controlled by three periods of crust extension and corresponding to three major periods of U-mineralization in South China respectively, the ΣCO_2 in each ore-forming hydrothermal solutions is all mantle-derived. Our studies reasonably explain why the mineralization did not occur immediately after the end of differentiation of the granitic magma rich in uranium, and why the ore-forming time of granite-type uranium deposit focuses on the time of crust extension after the formation of the uraniferous granites. 相似文献
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SR-O ISOTOPE SYSTEM OF SOME GRANITOIDS IN CHINA 总被引:1,自引:0,他引:1
Four of Sr- O isotope types can be observed in the graphs of δ~(18)O vs. (~(87)Sr/~(86)Sr)_i accord-ing to our data: (i) closed-system crystallization type: nearly short- vertical line withsimilar initial Sr isotope ratios and small changes of δ~(18)O values(<3‰); (ii) sialic materialremelting type: negative correlations without mantle end member; (iii) crust-mantle contam-ination type: a variety of mixing hyperbolas or straight lines with positive slopes: (iv)water-rock exchange type: irregular distribution. 相似文献
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“南永1井”礁相碳酸盐C,O,Sr,Pb同位素组成及其古环境意义探讨 总被引:5,自引:0,他引:5
“南永1井”礁相碳酸盐的O,C同位素组成可分为四段,它们的δ~(18)O(‰)和δ~(13)C(‰)平均值分别为:(Ⅰ)-5.0,-0.5;(Ⅱ)-7.7,-5.3;(Ⅲ)-6.4,-2.8;(Ⅳ)1.3,2.1.(Ⅱ)段的δ~(18)O值波动曲线以变化频率低、幅度小为特征,与布容期冰期-间冰期存在对应关系;(Ⅲ)和(Ⅳ)段的δ~(18)O和δ~(13)C值之间有正相关,在成因上与白云石化有关。△~(87)Sr和Pb同位素组成同样存在四分的特点。整个钻孔岩芯中△~(87)Sr的最大值和最小值以及全部正值都出现在第Ⅱ段。第Ⅳ段的Pb,sr同位素均呈现变化波动频繁的特点,在白云石化阶段有高μ值的Pb带入。礁相碳酸盐的O,C,Sr和Pb同位素组成记录了南海第四纪古气候、古环境变迁的历史。 相似文献
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The correlation between δD and H_2O content in granitoid can be divided into threetypes: closed-system crystallization type (Darongshan type): a flat positive linear corre-lation; open-system degassing type (Laoshan type): a nearly vertical linear positive cor-relation; meteoric hydrothermal exchange type (Gabug type): an irregular negative trendcorrelation. 相似文献
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