共查询到17条相似文献,搜索用时 80 毫秒
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冀东长城式金矿稳定同位素研究 总被引:3,自引:0,他引:3
长城式金矿是近年在冀东地区发现的一种新的金矿床类型,本文阐述了金矿床Pb、H、O、C同位素地球化学特征,研究揭示了这一新类型金矿床的某些独到特点。 相似文献
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冀东地区新发现一批产在中元古代碳酸盐岩层中的金矿床(点),文中对该类矿床的容矿围岩特征及其成因、产出的区域构造背景进行了讨论,提出容矿角砾岩是液压致裂角砾岩,是一种矿控构造岩。 相似文献
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"长城式"金矿是产于中元古界长城系碳酸盐岩地层中的一种新类型金矿。含矿带长约50 km,宽4~5km,由多个矿区,几十个矿体构成,一般单个矿体规模较小,矿体厚度变化系数26%,品位变化系数74%,矿体产出受地层和构造控制明显。 相似文献
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冀东地区是我国重要的金矿床密集区之一.根据金矿床形成的地质环境和后期的活化改造作用特征,将本区金矿床划分为两大系列、五大类型,两大系列为以太古宙花岗岩-绿岩带为容矿岩的金矿床系列和以中新元古界碎屑岩-碳酸盐岩为容矿岩的金矿床系列.以太古宙花岗岩-绿岩带为容矿岩的金矿床系列又划分为绿岩带同构造期初生型金矿床和绿岩带后构造期与中生代壳源深熔花岗岩有关的再生型金矿床.以中新元古界碎屑岩-碳酸盐岩为容矿岩的金矿床系列再细分为与造山带岩浆隐爆作用有关的金矿床,与造山带碰撞型壳源深熔花岗岩有关的金矿床和与造山带伸展构造作用有关的金矿床.同时分别叙述了冀东地区各类金矿床的地质特征. 相似文献
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新疆东准噶尔地区金矿床类型、地质特征 总被引:1,自引:1,他引:1
东准噶尔地区构造上位于哈萨克斯坦-准噶尔板块之巴尔喀什-准噶尔微板块北缘古生代陆缘活动带, 晚古生代是该区构造变形、岩浆活动和成矿作用的主要阶段。区内金矿可分为3个主要类型: 产于晚古生代凝灰岩、杂砂岩、浊积岩中的金矿, 产于海西期中酸性(偏碱性)侵入岩及其接触带中金矿, 产于晚古生代火山岩系中的金矿, 典型的代表性矿床分别为双泉金矿、黄羊山西金矿、双峰山金矿。三类金矿在赋矿围岩、控矿构造、矿床(体)规模/品位、围岩蚀变、金属矿物组合、成矿元素组合等多个方面均存在差异, 其原因是三者成矿作用过程中主要控矿因素、成矿机理的不同。 相似文献
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冀东、冀西广泛分布着以深变质绿岩带为主的变质基底,同时也是中生代岩浆活动十分发育的地区.剧烈的岩浆隐爆作用,对区内早期的绿岩带和其中的金及金矿床进行了强烈的活化改造,形成一批与岩浆隐爆作用有关的绿岩带再生型金矿床.该类金矿床由于赋存在不同的隐爆构造,具有多样性的矿化特征,可再细分为隐爆震碎角砾岩型金矿床、隐爆角砾岩筒型金矿床和隐爆侵入角砾岩墙型金矿床.文中较详细地阐述了各类金矿床的地质-地球化学特征,它们相互间的空间分布关系及与成矿有关的浅成侵入岩的特征.指出隐爆角砾岩型金矿床常与重熔岩浆有关的脉状-细脉浸染状金矿床、斑岩型金矿床共同产出,组成矿床组合,并具有垂直分带的分布特征,这对认识矿床的成矿机制和指导找矿有重大意义.最后,还讨论了成矿模式. 相似文献
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Gold is one of the most important mineral resources in China with its rich mineral resources. In recent years,significant progress has been made on the process of gold resource exploration. Some large and giant gold deposits were newly found and some important expansions in the main mining regions were also been completed. Studies on metallogenic regularity of gold deposits in China also have made achievements with a long–term work. This review aims to conclude the achievements of research on gold metallogenic regularity in China. Based on the data of about 2000 gold deposits and other ore(mineralized) occurrences,gold deposits in China were classified into five prediction types: gold deposits genetically related to granite–greenstone formation,gold deposits related to sedimentary formation(including the Carlin type and the metamorphosed clastic rock related vein gold deposit),gold deposits genetically related to volcanic rocks(including the continental and marine types),gold deposits genetically related to intrusions(including the porphyry type and the inner intrusion and contact zone related gold deposit),gold deposits of supergenesis(including fracture zone–altered rock gold deposit,placer gold deposit,gossan type gold deposit and soil type gold deposit). Statistics on precise chronology data of gold deposits indicate that there occurred 5 main periods of gold–mineralization in geological history of China. They were Neoarchean to Paleoproterozoic,Meso–Neoproterozoic,Paleozoic,Mesozoic,and Cenozoic. Gold deposits in China mainly formed in the Mesozoic and the Cenozoic. On the studies of the spatial–temporal distribution characteristics of gold deposits,53 gold–forming belts were delineated in China. The metallogenic regularity of gold deposits was preliminarily summarized and 71 gold metallogenic series were proposed in China. This suggests that it is necceary to deepen the study on metallogenic regularity of gold deposits and to provide the theory guide for the ore–prospecting for gold resources in China. 相似文献
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Zhao Hailing Deng Jinfu Li Kaiming Xu Liquan Department of Geology Mineral Resources China University of Geosciences Beijing 《中国地质大学学报(英文版)》1999,10(1):67-71
TheeasternHebeiProvinceofChinaisoneofthemajorconcentratingareasofgoldmineralizationineasternChina,whichisanimportantpartofthe... 相似文献
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胶东型金矿是不同于国际已知类型的独特金矿类型, 深入研究其成矿系列有助于深化理解矿床成因和指导找矿。本文综合分析了胶东金(银)、有色金属矿床的类型、空间分布、形成时间和成因, 划分了成矿系列, 列举了应用成矿系列指导找矿的案例。将胶东地区早白垩世与壳幔混合岩浆活动有关的金矿床、金及多金属矿床和有色金属矿床划归为胶东型金矿成矿系列, 进一步划分了Au(Ag)矿床成矿亚系列(125~115 Ma)和Cu-Pb-Zn-Mo矿床成矿亚系列(118~110 Ma), 认为两个成矿亚系列为连续发生、且有时间重叠的成矿事件。成矿系列理论有效指导了胶东地区的找矿工作, 根据石英脉型金矿和蚀变岩型金矿的成因联系在玲珑金矿田发现了台上—水旺庄巨型金矿床, 受胶莱盆地东北缘金矿床类型的启示发现了辽上黄铁矿碳酸盐脉型金矿, 在荣成有色金属成矿小区外围发现了大邓格金多金属矿床, 根据五莲七宝山金铜矿床探明了敞沟—杏山峪银铅锌矿床。 相似文献