东天山哈密地区赤湖钼铜矿区斜长花岗斑岩锆石SHRIMP U-Pb年龄

东天山赤湖斑岩钼铜矿床的形成时代和成矿地质背景至今尚存在争议,前人根据同一成矿带中土屋-延东斑岩铜矿的同位素地质年龄信息,认为赤湖钼矿的形成时代为中-晚泥盆世,系塔里木板块北部活动陆缘泥盆纪岛弧火山-深成作用的产物;近期一些研究者根据赤湖斑岩钼铜矿区斜长花岗斑岩锆石U-Pb和谐曲线年龄,认为矿化斜长花岗斑岩的侵位时代为晚石炭世,成矿作用与哈萨克斯坦-准噶尔板块南部活动陆缘晚石炭世汇聚阶段钙碱性岩浆侵入作用有关.在前人研究基础上,笔者对赤湖斑岩钼铜矿区矿化斜长花岗斑岩体进行了锆石SHRIMP U-Pb定年研究,获得322Ma±10Ma(95%可信度)的年龄值,表明赤湖斑岩铜矿床的形成时代为晚石炭世,成矿作用与晚石炭世钙碱性岩浆浅成侵位有关.     

天津蓟县雾迷山组高频旋回沉积特征

天津蓟县剖面的中元古界雾迷山组是一套厚达3 300 m的碳酸盐岩地层,其中广泛发育具有近似对称相序组构的雾迷山旋回层,属于特殊的环潮坪型碳酸盐米级旋回层序。在对旋回层内部岩石成因单元的类型及组合分析的基础上,建立了雾迷山旋回层的基本模式和沉积环境模式,并对成因单元的岩石磁化率特征及其对高频旋回的反映进行了探索。认为雾迷山旋回层为沉积环境的水深由较浅—较深—较浅—暴露条件下的沉积,可能代表真正的沉积旋回;其成因单元之间具有明显的有序叠置形态,表明它有可能是与米兰柯维奇旋回具有成因关联的高频率海平面变化所控制的自旋回沉积作用的产物。     

地球化学勘查在吉林前山金矿发现中的作用

前山金矿床位于吉林省珲春市北东72km处,属珲春市春化镇管辖。前山金矿床已经发现四条金矿体。Ⅰ号金矿体产在蚀变花岗岩株内,矿体呈不规则球形,矿体长轴方向长90m,短轴方向长50m,平均金品位11·59×10-6。矿体属浅埋藏,地表下4m~5m即见到矿体头部。Ⅱ号金矿体产于华力西晚期闪长岩与黑云母斜长花岗岩接触部的黑云母斜长花岗岩体内。控制延长430m,斜深20m~170m,平均斜深83m。矿体平均垂直厚度0·89m,平均金品位8·83×10-6。前山区地处长白山脉老爷岭南端,地形切割深度最大可达500m以上,相对高度一般在300m~700m,沟深谷长,山势险峻,属中山地…     

What Happened in the Trans-North China Orogen in the Period 2560-1850 Ma？

The Trans-North China Orogen （TNCO） was a Paleoproterozic continent-continent collisional belt along which the Eastern and Western Blocks amalgamated to form a coherent North China Craton （NCC）. Recent geological, structural, geochemical and isotopic data show that the orogen was a continental margin or Japan-type arc along the western margin of the Eastern Block, which was separated from the Western Block by an old ocean, with eastward-directed subduction of the oceanic lithosphere beneath the western margin of the Eastern Block. At 2550-2520 Ma, the deep subduction caused partial melting of the medium-lower crust, producing copious granitoid magma that was intruded into the upper levels of the crust to form granitoid plutons in the low- to medium-grade granite-greeustone terranes. At 2530-2520 Ma, subduction of the oceanic lithosphere caused partial melting of the mantle wedge, which led to underplating of mafic magma in the lower crust and widespread mafic and minor felsic volcanism in the arc, forming part of the greenstone assemblages. Extension driven by widespread mafic to felsic volcanism led to the development of back-arc and/or intra-arc basins in the orogen. At 2520-2475 Ma, the subduction caused further partial melting of the lower crust to form large amounts of tonalitic-trondhjemitic-granodioritic （TTG） magmatism. At this time following further extension of back-arc basins, episodic granitoid magmatism occurred, resulting in the emplacement of 2360 Ma, -2250 Ma 2110-21760 Ma and -2050 Ma granites in the orogen. Contemporary volcano-sedimentary rocks developed in the back-arc or intra-are basins. At 2150-1920 Ma, the orogen underwent several extensional events, possibly due to subduction of an oceanic ridge, leading to emplacement of mafic dykes that were subsequently metamorphosed to amphibolites and medium- to high-pressure mafic granulites. At 1880-1820 Ma, the ocean between the Eastern and Western Blocks was completely consumed by subduction, and the dosing of the ocean led to the continent-arc-continent collision, which caused large-scale thrusting and isoclinal folds and transported some of the rocks into the lower crustal levels or upper mantle to form granulites or eclogites. Peak metamorphism was followed by exhumation/uplift, resulting in widespread development of asymmetric folds and symplectic textures in the rocks.     

高喜马拉雅板块的槽流和韧性喷出:以锡金喜马拉雅Kangchenjunga-Darjeeling剖面为例

锡金西部和孟加拉北部的高喜马拉雅变质层序Kangchenjunga-Darjeeling剖面,是一个厚约15~20km、向南喷出的韧性槽,其以藏南折离和主中央冲断层之间的韧性剪切带为界。在Yok-sam-Kangchenjunga剖面,整个岩块由混合岩或淡色花岗岩岩片组成。淡色花岗岩巨大的岩床,或近水平状到略北倾的岩片组成整个Kangchenjunga地块,并西延到Jannu。剪切方向标志显示出纯剪切扁平组构和非共轴向南的单一剪切组构。在Singallila山脊和Darjeeling飞来峰南缘一带可见充填了熔融物质的槽的熔融壳,已证实呈由夕线石-钾长石级向下经蓝晶石和十字石至石榴子石-黑…     

LA-ICPMS U-Pb Ages of Zircon from Metaleucosomes, Olongbuluke Microcontinent, North Qaidam, and Implications on the Response to the Global Rodinia Supercontinent Assembly Event in NW China

INTRODUCTION The Olongbuluke microcontinent , which wasdisintegratedfromthe northern margin of the Qaidamblock (Lu,2002) ,is composed of a two-fold base-ment with cover strata . The lower basement is themedium- to high-grade Delingha complex and theDakendaban Group, and the upper is the low-gradeWandonggou Group. The Wandonggou Group of theupper basement experienced a Late Mesoproterozoicmetamorphic event (see Yu et al .,1994) ,consistentwith the early isotopic geochronological respo…     

阿尔金碰撞造山带西段的构造特征

根据阿尔金山西段前早古生代变质岩的岩石组成、沉积建造、变形变质作用改造历史、岩石地球化学特征等研究,将阿尔金碰撞造山带西段划分为3个构造单元:北阿尔金地块、中阿尔金地块(包括英格里克构造-蛇绿混杂岩带、肖鲁克·布拉克高压变质岩带和塔什萨依玉石矿高绿片岩相—低角闪岩相变质岩带)和南阿尔金地块(包括南阿尔金中—新元古界隆起带和阿尔金南缘复合构造-蛇绿混杂岩带)。提出该碰撞造山带经历了前长城纪古陆核形成阶段、长城纪—青白口纪不同基底联合阶段和早古生代洋陆转换阶段3个阶段的构造演化。     

陈列在阿拉套山东端南麓的花岗岩雕琢工艺品——博乐怪石沟

每逢六月，是博尔塔拉大草原最美丽的季节，广阔无垠的草原上盛开着各种鲜花，争奇斗妍。湛蓝的湖面上映衬着雪山倒影、浑然一体。饱览眼前美仑美奂的胜景过后，总忘不了博乐市东北角那片神秘奇特的花岗岩地质景观。     

太行山北段燕山期花岗岩成因类型及其成矿作用

根据地质及岩石学、岩石化学、地球化学、同位素资料综合分析，太行山北段燕山期花岗岩成因类型为壳幔混源的Ⅰ型花岗岩。区内成矿作用与该类花岗岩关系密切，具体表现在矿床（点）与岩体具有时空上的一致性，成矿物质与成岩物质具有同源性和深源性以及岩体内Cu、Pb、Zn、Mo、Au、Ag元素丰度值较高等特点。矿化类型或成矿系列严格受岩石类型、化学成分、岩浆活动性质等因素控制，表现出明显的成矿专属性。部分熔融作用使下地壳物质形成熔浆的同时，还可以使下地壳中的成矿元素重新活化、迁移并富集在熔浆中，然后与深部上来的富含成矿元素的幔源岩浆一起混合形成壳幔混源的含矿母岩浆。因此，区内燕山期Ⅰ型花岗岩应该是成矿物质的主要提供者。并进一步指出软流圈物质大规模上涌是导致本区Ⅰ型花岗质岩浆活动及成矿作用的最根本的原因。     

在花岗岩体中寻找钼矿的建议

伊春一延寿多金属成矿带是小兴安岭地区最重要的成矿带，成矿带赋存有60多个大中小型的多金属矿床、矿点，究其成矿机制，多为岩浆热液和矽卡岩型，产出部位基本上位于零星分布的元古界和古生界地层中，或地层与侵入岩的内外近接触带，而分布面积占伊春一延寿70％的花岗岩区以往甚少发现矿床。2000年以来，新一轮新方法化探扫面工作在花岗岩区发现大型的钼矿床。花岗岩区钼矿的发现让人们找矿理念为之一新。