西北某铬矿床中铂族元素赋存状态及铂族矿物的研究

产于太古界斜长角闲片岩中的某超基性岩体上盘的甲矿体和下盘的乙矿体中普遍含有铂族元素。     

Proterozoic East Gondwana： supercontinent assembly and breakup

The editors of this volume assembled a remarkable group of contributors to discuss both the geology of East Gondwana and also many related issues. The 19 papers in this book provide a wealth of information on East Gondwana, the assembly of Gondwana as a supercontinent, the configuration of Rodinia,and general problems of the origin of continental crust and movement of continental plates. They also illustrate some of the controversies, with most papers having at least some points of difference in both fact and interpretation from other oaoers in the book.     

北祁连中西段与超基性岩有关的金矿化特征及成因探讨

北祁连中西段发育三套早古生代蛇绿岩及相应的基性、超基性岩,呈北、中、南三条带状分布。区内金的活化、迁移主要受控于超基性岩带和与其分布近于一致的两条韧性剪切带,金矿化主要发生在强蚀变超基性岩体内、岩体与围岩接触带、断裂破碎蚀变带内。根据包裹体测温及成分测定、稳定同位素特征资料及超基性岩中金丰度值等分析,金矿物质主要来自超基性岩,流体来源于深部,其成因属与超基性岩有关的韧性剪切带型金矿床。     

星际分子正—NH3和He的超精细跃迁碰撞截面和速率系数的理论计算

本文采用Ｒ矩阵传播方法，通过求解ＣＳ近似下的耦合方程，计算了星际分子云条件下正－ＮＨ３分子和Ｈｅ碰撞的超精细跃迁碰撞截面和速率系数，为研究天体的信息提供需用的基础数据。     

视超光速源中3C454.3的特殊性

本文从简要总结迄今所发现的视超光速源开始。介绍近年来探测到的视超光速源之一——类星体3C 454.3的VLBI多频段,多历元观测及其主要结果。采用列表对比方式表明此源相对其他视超光速源的一般特征呈现的特殊性。最后对此特殊的视超光速源的可能解释作初步讨论。 本文可以看作是对3C453.3观测已有报导[12]和[13]的进一步补充。     

某含镍超基性岩侵入体的地球化学

Chemical variations, geochemical behaviors and other problems such as element assemblages and relative abundances of elements during and after various geologic processes (magmatism, assimilation, hydrothermal alteration as well as tectonic movements) have been discussed for a nickel-bearing ultrabasic intrnsion. Particular emphasis is placed on aspects concerning the geochemical behavior of nickel. Conclusions have been reached about the environment and possible mechanism for the emplacement of this massive and for the origin of Ni sulfides. A “assimilation-immiscibility“ hypothesis is proposed for formation of copper-nickel sulfide deposits in ultrabasic intrnsives.     

我国W区超镁铁-镁铁杂岩体钯、铂元素地球化学研究

我国W区岩体产在上古生代凹陷西北边缘与中间隆起交接处,北东向深大断裂带东侧。区内地层主要由石炭纪砂板岩、片理化酸性火山碎屑岩;二迭纪砂页岩、中酸性火山岩、火山碎屑岩及第四纪松散沉积物所组成。本区侵入岩异常发育,属海西年代,包括两     

REE Characteristics of the Kalatongke Cu-Ni Deposit, Xinjiang, China

On the basis of the study on the REE geochemistry of the ore minerals and host rocks of the Kalatongke Cu-Ni deposit, Xinjiang, it is indicated that the major ore minerals, sulfides, were sourced from the host mafic-ultramafic magma. Characterized by low REE content of sulfide, such a Cu-Ni sulfide deposit occurring in the orogen is obviously different from that on the margin of the craton. Because the mafic-ultramafic rocks from the Cu-Ni sulfide deposit occurring in the orogen is water-rich and the REEs of some sulfides show a particular "multiple-bending" pattern, which suggests coexistence of multiple liquid phases (fluid and melt), the sulfide melt possibly contains a great deal of hydrothermal fluids and increasingly developed gases and liquid-rich ore-forming fluids after the main metallogenic epoch (magmatic segregation stage).     

内蒙古察哈尔右翼后旗永生村超贫型铁矿成因分析

位于乌兰察布市察哈尔右翼后旗白音察干镇以西30km2永生村铁矿区,通过详查工作的研究,对矿区元素富集特征、赋矿层位、控矿因素等地质特征和成矿条件有了很好地认识。全区共圈定8条矿体,矿体赋存于加里东晚期辉石、斜长角闪岩体中,矿体走向35°～55°,倾向125°～145°,倾角76°～88°,呈脉状、似层状产出。矿体与围岩岩性一致,呈渐变过渡关系,界线靠化验结果区分。根据矿石结构、围岩特征及成矿元素赋存特征等分析,认为永生村铁矿区为火山~岩浆建造变质超贫型磁铁矿床。