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再论大兴安岭中东部六九山铜矿床成矿地质特征、成因与成矿地质背景 被引量:1
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作者 宫永吉 孙景贵 刘阳 《吉林地质》 2020年第4期1-10,共10页
六九山铜矿床产在大兴安岭中东部的突泉—龙江—岔路口斑岩-浅成热液Cu (Mo)-Pb-Zn成矿带中部,发育在中生代花岗闪长岩体与叠加之上的光华组酸性火山岩体系的NWW向断裂中。矿体呈椭圆似穹隆状,长轴近东西走向,矿体处于海拔-80^+300 m之... 六九山铜矿床产在大兴安岭中东部的突泉—龙江—岔路口斑岩-浅成热液Cu (Mo)-Pb-Zn成矿带中部,发育在中生代花岗闪长岩体与叠加之上的光华组酸性火山岩体系的NWW向断裂中。矿体呈椭圆似穹隆状,长轴近东西走向,矿体处于海拔-80^+300 m之间。矿体工业类型为角砾岩型,主要由隐爆热液胶结角砾岩和次要的热液充填角砾岩和网脉状热液充填震裂(碎)岩组成。原生围岩蚀变从早到晚依次发生强弱不同的钾长石-黑云母化→青磐岩化→泥化→绢英岩化→早阶段灰白色硅化(面状)→成矿阶段灰白色硅化(充填状)→晚阶段白色硅化(梳状+晶洞状+晶簇)→萤石+石膏(浸染状+晶洞+细脉状)→碳酸盐化。原生矿化依次是黄铁矿+辉钼矿→黄铁矿+黄铜矿→黄铜矿+闪锌矿。成矿过程经历乳白色脉状黄铁矿+石英±黄铜矿阶段、胶结状石英+黄铁矿+黄铜矿阶段、细脉+晶洞状石英+黄铁矿阶段和浸染+细脉状萤石+石膏阶段。将其与典型矿床成矿特征对比、并结合区域成岩成矿年代学研究成果,认为该矿床应是浅成热液高硫化型铜矿床。成矿作用适值早白垩世库拉板块向欧亚大陆俯冲的大陆边缘火山弧环境。 展开更多
关键词 成矿地质特征 矿床成因 成矿地质背景 六九山铜矿床 大兴安岭中东部
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Spatio-temporal Pattern and Spatial Heterogeneity of Ecotones Based on Land Use Types of Southeastern Da Hinggan Mountains in China 被引量:4
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作者 YU Lingxue ZHANG Shuwen +3 位作者 LIU Tingxiang TANG Junmei BU Kun YANG Jiuchun 《Chinese Geographical Science》 SCIE CSCD 2015年第2期184-197,共14页
Ecotones have received great attention due to its critical function in energy flux, species harbor, global carbon sequestration, and land-atmosphere interaction. This study investigated land use pattern and spatial he... Ecotones have received great attention due to its critical function in energy flux, species harbor, global carbon sequestration, and land-atmosphere interaction. This study investigated land use pattern and spatial heterogeneity of the ecotones among agricultural land, forest land, and grassland of the southeastern Da Hinggan Mountains in the northeastern China. The change of these delineated ecotones under different slopes and aridity conditions was analyzed by two landscape indices, edge density(ED) and core area percentage of landscape(CPL), to explore the inter-linkage between spatial structure of ecotones and socioeconomic development and land management. Specifically, the ecotones such as agriculture-forest(AF) ecotone, forest-grassland(FG) ecotone, and agriculture-forestgrassland(AFG) ecotone moved from the arid southeast to the humid northwest. The flat area with small slope is more edge-fragmented than the steep area since the ED decreases as the slope increases. The AF ecotone mostly found in the humid region is moving to more humid areas while the agriculture-grassland(AG) ecotone mostly found in the dry region is moving towards the drier region. 展开更多
关键词 ecotones core area percentage of landscape(CPL) edge density(ED) modified moving split window land use pattern spatial heterogeneity
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