某些铝土矿中稀土元素的地球化学特征   总被引：1，自引：0，他引：1  

刘长龄  覃志安 《地质与勘探》1991,27(11):49-53

本文对山西、河南、四川等地某些铝土矿中稀土元素的分布、配分、比值及其含矿岩系与基底岩石、古陆花岗岩和变质岩中稀土成分的相关系数作了对比研究.据此探讨了铝土矿的物质来源.  相似文献   

江西银山矿床岩石稀土地球化学研究   总被引：7，自引：0，他引：7  

林德松  杨斌 《矿产与地质》1991,5(5):349-356

银山矿区的三个旋回火山一次火山岩属同源产物,其原始物质的35%为沉积岩熔体和65%为玄武岩质熔依.是两者的混岩浆.因而.岩石的成因类型属幔壳混合型.根据矿床中蚀变围岩千枚岩的希土组成特征、认为不同矿化蚀变带稀土分配形式基本相似,从而揭示了各带成矿流体成因上的继承性和来源的一致性.  相似文献   

南Explorer洋脊块状硫化物—硫酸盐及铁帽的稀土元素地球化学     

Barr.  TJ 霍有光 《西北地质》1991,(A00):79-83

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广西大宁花岗闪长岩体中暗色...     

沙连坤  袁奎荣 《地球科学》1991,16(4):377-386

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80年代稀土元素地球化学分析进展     

雷剑泉 《地质地球化学》1991,(1):59-63

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如何开发我省风化壳淋积型稀土矿的几点意见     

何往  张驰 《福建地质科技情报》1991,(4):9-12

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REE Abundaces in Megacrysts and Host Basalts：REE Behavior of Magma at High Pressures     

肖森宏 《中国地球化学学报》1991,10(1):11-20

Based on REE abundances in megacrysts and host basalts and their equilibrium conditions,it has proved that megacrysts may have been produced from the magma derived from the host rocks or of more basic composition.The REE ratios of megacrysts to host rocks may be taken as partition coefficients when both are equilibrium with each other.The crystal fractionation of megacrysts has caused the evolution of REE in the magma.It is obvious that some host basalts are the product of magma evolution after crystal fractionation.According to REE abundances in the host rocks and the partition coefficients between crystal and liquid,the history of crystal fractionation of magma can be traced.  相似文献   

Petrochemistry,Age and Petrogenesis of the Shexian Pluton in Southern Anhui     

Xing Fengming  Xu Xiang  Ren Siming  Li Yingyun 《中国地球化学学报》1991,10(3):244-256

The Shexian gneissic granodiorite in southern Anhui trends NE 55° from Shexian in the west to Guitoujian in the east with a length of 22 km and an outcrop area of 32 km. It was considered formerly to be Caledonian on the basis of a biotite K-Ar age of 474 Ma (1982). However, new evidence indicates that it may be Early Jinning in age as shown by: (1) it is found intruding into the Mid-Proterozoic Shangxi Group and is unconformably overlain by the Sinian Xiuning Formation, and (2) a zircon U-Th-Pb age of 928 Ma is obtained for the pluton. The pluton is composed of plagioclase (An=27.37%), K-feldspar(14%), biotite(16%) and quartz(32%). Accessory minerals are ilmenite (150g/T), xenotime (15g/T). garnet(25g/T), monazite(10g/T), zircon (20g/T) and apatite (104g/T). Petrochemical characteristics of the intrusion are:(l) Al-enrichment (A/NKC=1.30); (2) H₂O enrichment (H₂O= 1.74%); and (3) low oxidation index (f ’=0.10). It belongs to the continental crust transformation type as evidenced by: (1) MF and Mg/Y values of biotite are 0.41 and 0.31 respectively; (2) (⁸⁷Sr/⁸⁶Sr)=0.71119; (3) δ Eu=0.52; and (4) A/NKC=130. The Shexian pluton is therefore considered as a product of melting of phyllite at depth in the light of similarities in trace element and REE contents with the phyllite of the Banxi Group. Calculations of REE batch partial melting indicate that it may have resulted from 75% melting of the Banxi phyllite.  相似文献   

内蒙古贺根山地区蛇绿岩稀土元素和Sm—Nd同位素研究   总被引：1，自引：0，他引：1  

《地球化学》1994,23(4):339-349

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江西凤凰岽含锡黄英岩脉特征及成因   总被引：1，自引：0，他引：1  

熊小林  朱金初 《矿物岩石》1994,14(1):28-35

江西会昌县岩背火山盆地密坑山含黄玉花岗岩体的北侧外接触带，产有数条含锡黄英岩脉。据野外产状、岩石结构构造等表明岩脉属岩浆成因。稀土元素研究表明，凤凰岽黄英岩ＲＥＥ含量极低，∑ＲＥＥ及配分曲线与脉侧黄玉石英化蚀变岩有着明显的区别。富氟花岗岩浆结晶晚期衍生的富Ｓｉ，Ａｌ，Ｆ含少量Ｋ，Ｎａ的残余熔浆沿断裂上侵因压力降低产生二次沸腾，使Ｋ，Ｎａ分离进入含水相，这是富Ｓｉ，Ａｌ，Ｆ；极贫Ｋ，Ｎａ的黄英岩形成的决定因素。  相似文献