早子沟金矿矿石质量特征、选矿试验研究及选别效果   总被引：1，自引：0，他引：1  

刘春先  陈耀宇  柳生祥  梁志录  金鼎国 《甘肃地质》2012,(2):57-62

本文依据早子沟金矿矿区勘查及选矿工艺矿物学研究资料,从金矿石的结构构造、矿石类型、矿物成分、金的赋存状态及其主要载体矿物的嵌布特征、共伴生组分等方面综述了矿石质量特征,重点分析了以上矿石质量特征要素对选矿的影响;简述了选矿试验研究的成果及选别效果。矿区矿石工艺类型属少硫化物微细粒浸染型含金矿石,金的赋存状态复杂,利用重选—浮选中矿再磨的重浮联合流程可获得较理想的选冶回收指标。  相似文献   

阿尔泰南缘中泥盆统北塔山组火山岩的矿物学研究   总被引：2，自引：0，他引：2  

张贺  张招崇 《矿物学报》2012,32(3):386-397

阿尔泰山南缘中泥盆统北塔山组火山岩极为发育。本文对富辉橄玄岩和玄武岩中的单斜辉石和橄榄石斑晶进行了矿物化学分析,并结合矿物的地质温压计和岩浆结晶模拟,约束了两种岩石中矿物的形成过程,推测了原始岩浆的演化过程。提出富辉橄玄岩和玄武岩的原始岩浆属于拉斑玄武系列,富辉橄玄岩中的高压单斜辉石来源于深部（40～50 km）,其结晶早于橄榄石;玄武岩中单斜辉石大多属于岩浆房结晶产物（30～40km）,其结晶晚于橄榄石;两种岩石中橄榄石均属于岩浆房结晶产物（30～40 km）。  相似文献   

贵州威宁沉积型赤铁矿矿石工艺矿物学研究     

刘贞才  谯文浪  安亚运  陈武  王波 《贵州地质》2012,29(1):62-67

对贵州威宁沉积型赤铁矿石进行了工艺矿物学研究,重点研究了该矿石的矿物组成、主要矿物嵌布特征和主要含铁矿物赤铁矿的单体解离情况。研究表明,该矿石属于低磷、低硫、微细粒嵌布的赤铁矿石;矿石中主要铁矿物以赤铁矿为主,其次为磁铁矿和褐铁矿,主要脉石矿物以石英为主,其次为绿泥石、云母、高岭石等粘土矿物;赤铁矿嵌布粒度极细,平均粒度0.015mm,且赤铁矿与脉石矿物嵌布关系复杂。本研究为该矿石的开发利用提供基础资料。  相似文献   

SCI收录的矿物学类核心期刊介绍     

王彦 《矿物学报》2012,32(2):316-320

以表格的形式汇总介绍了SCI收录的20种矿物学类目核心期刊的刊名、国际标准刊号（ISSN）、出版地和最新影响因子,并详细介绍了这20种期刊的出版周期、出版者、联系地址、最新期刊网址及期刊描述等全方位的期刊信息。期刊描述内容包括：期刊的创刊年以及期刊的发展,期刊刊载的主要内容,网站可免费获取的该刊目次和文摘及全文信息等,以便为相应学科的科研工作者提供参考。  相似文献   

西藏尼雄矿田日阿铜矿床矽卡岩矿物学特征及地质意义   总被引：3，自引：1，他引：2  

于玉帅  杨竹森  刘英超  田世洪  赵灿  高原  纪现华  胡为正  曹圣华 《矿床地质》2012,31(4):775-790

尼雄矿田位于冈底斯成矿带西段中部隆格尔南木林岩浆岩带的北侧.日阿铜矿床位于尼雄矿田的东南端,矿体产于晚白垩世侵入岩与下拉组灰岩接触带的矽卡岩或矽卡岩化大理岩中,主要矽卡岩矿物有石榴子石、透辉石、蛇纹石、金云母、绢云母、硅镁石、阳起石、透闪石、绿帘石、绿泥石等.电子探针分析表明,矿区石榴子石主要为钙铁榴石,次为钙铝榴石;辉石以透辉石为主;金云母明显富镁贫铁,且富含挥发分F;闪石类矿物属钙角闪石系列;绿泥石富镁贫铁.推断成矿流体大致经历了5个演化阶段:①干矽卡岩阶段,高温(＞450℃)、低pH值、氧化-弱氧化;②湿矽卡岩阶段,温度降低,pH值和氧逸度逐渐升高;③氧化物阶段,温度进一步降低,pH值升高(碱性),氧逸度则呈降低趋势;④石英硫化物阶段,中等温度(200～300℃),高pH值(碱性),低氧逸度;⑤碳酸盐阶段,低温(160～203℃),低pH值,低氧逸度.此外,矿区还存在多金属矿化的可能.  相似文献   

Mineralogy and Mineral Chemistry of the Cretaceous Duolong Gold‐Rich Porphyry Copper Deposit in the Bangongco Arc,Northern Tibet     

Jinxiang LI  Guangming LI  Kezhang QIN  Bo XIAO  Lei CHEN  Junxing ZHAO 《Resource Geology》2012,62(1):19-41

The Early Cretaceous Duolong gold‐rich porphyry copper deposit is a newly discovered deposit with proven 5.38 Mt Cu resources of 0.72% Cu and 41 t gold of 0.23 g t^?1 in northern Tibet. Granodiorite porphyry and quartz diorite porphyrite are the main ore‐bearing porphyries. A wide range of hydrothermal alteration associated with these porphyries is divided into potassic, argillic and propylitic zones from the ore‐bearing porphyry center outward and upward. In the hydrothermal alteration zones, secondary albite (91.5–99.7% Ab) occurs along the rim of plagioclase phenocryst and fissures. Secondary K‐feldspar (75.1–96.9% Or) replaces plagioclase phenocryst and matrix or occurs in veinlets. Biotite occurs mainly as matrix and veinlet in addition to phenocryst in the potassic zone. The biotite are Mg‐rich and formed under a highly oxidized condition at temperatures ranging from 400°C to 430°C. All the biotites are absent in F, and have high Cl content (0.19–0.26%), with log (X_Cl/X_OH) values of ?2.74 to ?2.88 and IV (Cl) values of ?3.48 to ?3.35, suggesting a significant role of chloride complexes (CuCl₂^‐ and AuCl₂^‐) in transporting and precipitating copper and gold. Chlorites are present in all alteration zones and correspond mainly to pycnochlorite. They have similar Fe/(Fe+Mg), Mn/(Mn+Mg) ratios, and a formation temperature range of 280–360°C. However, the formation temperature of chlorite in the quartz‐gypsum‐carbonate‐chlorite vein is between 190°C and 220°C, indicating that it may have resulted from a later stage of hydrothermal activity. Fe³⁺/Fe²⁺ ratios of chlorites have negative correlation with Al^IV, suggesting oxygen fugacity of fluids increases with decreasing temperature. Apatite mineral inclusions in the biotite phenocrysts show high SO₃ content (0.44–0.82%) and high Cl content (1–1.37%), indicating the host magma had a high oxidation state and was enriched in S and Cl. The highest Cl content of apatite in the propylitic zone may have resulted from pressure decrease, and the lowest Cl content of apatite in the argillic zone may have been caused by a low Cl content in the fluids. The low concentration of SO₃ content in the hydrothermal apatite compared to the magmatic one may have resulted from the decrease of oxygen fugacity and S content in the hydrothermal fluid, which are caused by the abundant precipitation of magnetite.  相似文献   

The Rumuruti chondrite group     

Addi Bischoff  Nadia Vogel  Julia Roszjar 《Chemie der Erde / Geochemistry》2011,(2):101-133

Since 1994, the Rumuruti (R) chondrites have been recognized as a new, well-established chondrite group differing from carbonaceous, ordinary, and enstatite chondrites. The first R chondrite, Carlisle Lakes, was found in Australia in 1977. Meanwhile, the number has increased to 107 (December, 2010). This group is named after the Rumuruti meteorite, the first and so far the only R chondrite fall. Most of the R chondrites are breccias containing a variety of different clasts embedded in a clastic matrix. Some textural and mineralogical characteristics can be summarized as follows: (a) the chondrule abundance in large fragments and in unbrecciated rocks is ∼35–50 vol%; (b) Ca,Al-rich inclusions are rare; (c) the olivine abundance is typically 65–78 vol%; (d) the mean chondrule diameter is ∼400 μm; (e) in unequilibrated R chondrites, low-Ca pyroxene is dominating, whereas in equilibrated R chondrites it is Ca-rich pyroxene; (f) the typical olivine in a metamorphosed lithology is ∼Fa_38–40; (g) matrix olivine in unequilibrated, type 3 fragments and rocks has much higher Fa (∼45–60 mol%) compared to matrix olivines in type 4–6 lithologies (∼Fa_38–41); (h) spinels have a high TiO₂ of ∼5 wt%; (i) abundant different noble metal-bearing phases (metals, sulfides, tellurides, arsenides) occur. The exception is the metamorphosed, type 5/6 R chondrite La Paz Icefield 04840 which contains hornblende, phlogopite, and Ca-poor pyroxene, the latter phase typically occurring in low-grade metamorphosed R chondrites only.In bulk composition, R chondrites have some affinity to ordinary chondrites: (a) the absence of significant depletions in Mn and Na in R chondrites and ordinary chondrites is an important feature to distinguish these groups from carbonaceous chondrites; (b) total Fe (∼24 wt%) of R chondrites is between those of H and L chondrites (27.1 and 21.6 wt%, respectively); (c) the average CI/Mg-normalized lithophile element abundances are ∼0.95 × CI, which is lower than those for carbonaceous chondrites (≥1.0 × CI) and slightly higher than those for ordinary chondrites (∼0.9 × CI); (d) trace element concentrations such as Zn (∼150 ppm) and Se (∼15 ppm) are much higher than in ordinary chondrites; (e) the whole rock Δ¹⁷O of ∼2.7 for R chondrites is the highest among all meteorite groups, and the mean oxygen isotope composition is δ¹⁷O = 5.36 ± 0.43, δ¹⁸O = 5.07 ± 0.86, Δ¹⁷O = +2.72 ± 0.31; (f) noble gas cosmic ray exposure ages of R chondrites range between ∼0.1 and ∼70 Ma. More than half of the R chondrites analyzed for noble gases contain implanted solar wind and, thus, are regolith breccias. The 43 R chondrites from Northern Africa analyzed so far for noble gases seem to represent at least 16 falls. Although the data base is still scarce, the data hint at a major collision event on the R chondrite parent body between 15 and 25 Ma ago.  相似文献   

内蒙古黄岗锡铁矿床夕卡岩矿物学特征及其成矿指示意义   总被引：5，自引：1，他引：4       下载免费PDF全文

周振华  刘宏伟  常帼雄  吕林素  李涛  杨永军  张瑞军  纪显合 《岩石矿物学杂志》2011,30(1):97-112

为进一步查明黄岗锡铁矿矿床成因、夕卡岩矿物成分与金属矿化类型之间的联系,利用电子探针对研究区主要夕卡岩矿物的化学成分进行了详细的分析。测试结果表明,成矿早期石榴石的端员组分以钙铁榴石为主,主成矿期石榴石的端员组分以钙铝榴石为主;辉石端员组分变化较大,主要为透辉石和钙铁辉石。石榴石和辉石的矿物组分分别为Adr28.69～96.44Grs2.00～67.38(Prp+Sps)0.67～5.69和Di11.8～94.12Hd4.08～81.28Jo1.79～20.02,其较大的成分变化特征反映出夕卡岩不是在一个完全封闭的平衡条件下形成的。角闪石大多为镁铁钙角闪石,个别属于铁角闪石,成分变化较大的原因可能是由于氧化还原条件改变导致不同程度的AlⅥSi←→(Na,K)的置换作用,属于一种固相线下的转变。角闪石中四次配位的Si、Al及六次配位的Al、Ti和A位置的阳离子数变化范围很大,可能是由于接触交代作用过程中岩浆的成分差异或结晶时的物理化学条件改变所引起的。富锰的辉石夕卡岩是岩浆流体顺层间破碎带渗滤交代形成的,富锰辉石可作为本区寻找Sn、Cu、Zn等多金属的找矿标志,外接触带夕卡岩和其附近的大理岩中是多金属成矿的有利部位。  相似文献   

乳腺炎症及增生症病灶中钙化的矿物学研究     

熊翠娥  王长秋  鲁安怀  李艳  梅放  柳剑英 《岩石矿物学杂志》2011,30(6):1014-1020

选取9例乳腺炎症、7例乳腺增生的钙化样品,利用光学显微镜(OM)、环境扫描电镜(ESEM)、微区X射线衍射(μ-XRD)等矿物学分析方法对样品进行了原位形貌观察、分离后结构及成分的测试分析,探讨了病灶中钙化的矿物学特征及其组成成分和形成机制。研究结果表明,发生在炎症病灶中的钙化主要类型是脂肪坏死后的钙化,其发生和死亡的脂肪细胞和周围病变后期修复性Ⅲ型胶原有直接关系。增生症中的钙化主要有发生在扩张的导管内和在束状深度交联胶原中的坏死型钙化,扩张的导管边缘处Ⅳ型胶原和大片变性Ⅲ型胶原为钙化提供了成核位点,继而参与无机矿物的形成过程,最后形成较为致密的钙化。乳腺炎症和增生症中的钙化的主要成分均为碳羟磷灰石。  相似文献   

A Systematic Spectroscopic Study of Four Apollo Lunar Soils     

凌宗成  Bradley L Jolliff 《中国地质大学学报(英文版)》2011,(5)

A systematic spectroscopic study including Raman,Mid-IR,NIR,and VIS-NIR,is used to investigate four endmember lunar soils.Apollo soils(<45 μm) 14163,15271,67511,and 71501 were selected as endmembers to study,based on their soil chemistry,maturity against space weathering,and the sampling locations.These endmembers include an anorthositic highlands soil(67511),a low-Ti basaltic soil(15271) ,a high-Ti basaltic soil(71501),and a mafic,KREEPy,impact-melt-rich soil(14163) .We used a laser Raman point-counting pr...  相似文献