FEATURES OF Pb ISOTOPIC COMPOSITION OF ORES AND EVOLUTION OF CONTINENTAL CRUST OF CHINA

Based on the Pb isotopic features, the ore leads in the continent of China can be dividedinto four types: (i) single-stage lead of low μ value derived from mantle, (ii) homogeneouslead of crustal source with high μ value, (iii) modern mixing lead between mantle andcrust, and (iv) residual lead of crustal source. As the leads from mantle had possessed single-stage features (μ = 7.8) before the Proterozoic, the ages of continental crust can be calculatedbased on the mixing Pb of type (iii). The results hidicate that the continental crust of Chinawas mainly generated during the Archaean, and the growth rates of crust reached the max-ima by the ages of 3.3-3.4, 2.6 and 1.6-1.7 b.y. The occurrences of residual crust Pbwith high ~(207)Pb/~(204)Pb and ~(208)Pb/~(204)Pb anomalies were associated with the remelting andreconstruction of crust since 1.6 b.y. ago. The lead sources in the continent of China showhigher Th/U ratios (3.3-6.5) and ~(207)Pb anomalies than those in other continents, indicationthe conti     

矿石铅同位素组成特征与中国大陆地壳的演化

本文根据壳幔混合铅的二阶段模式计算,表明大陆地壳主要派生于太古代,地壳增加速率在33—34,26和16—17亿年出现极大值.晚元古代后,中国大陆出现广泛的重熔再造,导致了高Pb~(207)/Pb~(204)与Pb~(208)/Pb~(204)异常铅的出现,表明其改造程度要比其他大陆强烈.中国大陆铅源普遍具有高Th/U比特征也可能反映原始地球的区域不均一性。     

“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

“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。