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| 1 | 个旧—大厂地区地质构造演化及锡多金属成矿显示文摘个旧—大厂锡多金属矿床不是简单的燕山晚期地台环境的'花岗岩岩浆期后气液矿床',矿区地处三大板块的交接部位附近的个旧-大厂锡矿,前泥盆纪区域构造岩浆活动及锡多金属成矿作用强烈,泥盆纪—三叠纪裂谷作用和锡多金属成矿特点突出。泥盆纪受北西向同沉积断裂控制,在南丹 河池一带裂谷作用明显,发生了海底喷流成矿,加上印支—燕山期构造岩浆改造,形成了大厂锡矿。三叠纪受北东向个旧—兴义—晴隆同沉积断裂控制,在个旧、兴义一带发生的裂谷作用,伴随基性火山成矿、喷流热水沉积成矿和燕山晚期花岗岩改造(叠加)成矿,从而形成了个旧锡矿。 | 秦德先 谈树成 范柱国 黎应书 陈爱兵 李连举 刘光亮 党玉涛 童祥 武俊德 李玉新 | 2004 | 矿物学报2004，24，2： | 41 |
| 2 | Isotopic Ages of the Carbonatitic Volcanic Rocks in the Kunyang Rift Zone in Central Yunnan,China显示文摘The Mesoproterozoic Kunyang rift, which is located on the western margin of the Yangtze platform and the southern section of the Kangdian axis, is a rare massive Precambrian iron-copper polymetallic mineralization zone in China. The Mesoproterozoic Wulu (Wuding(Lufeng) basin in the middle of the rift is an elliptic basin controlled by a ring fracture system. Moreover, volcanic activities in the basin display zonation of an outer ring, a middle ring and an inner ring with carbonatitic volcanic rocks and sub-volcanic dykes discovered in the outer and middle rings. The Sm-Nd isochron ages have been determined for the outer-ring carbonatitic lavas (1685 Ma) and basaltic porphyrite of the radiating dyke swarm (1645 Ma) and the Rb-Sr isochron ages for the out-ring carbonatitic lavas (893 Ma) and the middle-ring dykes (1048 Ma). In combination of the U-Pb concordant ages of zircon (1743 Ma) in trachy-andesite of the corresponding period and stratum (1569 Ma) of the Etouchang Formation, as well as the Rb-Sr isochron age (1024 Ma) and K-Ar age (1186 Ma) of the dykes in the middle ring, the age of carbonatites in the basin is preliminarily determined. It is ensured that all of these carbonatites were formed in the Mesoproterozoic period, whereby two stages could be identified as follows: in the first stage, carbonatitic volcanic groups, such as lavas, pyroclastic rocks and volcaniclastic sedimentary rocks, were formed in the outer ring; in the second stage, carbonatitic breccias and dykes appeared in the middle ring. The metamorphic age of the carbonatitic lavas in the outer ring was determined to be concurrent with the end of the first stage of the Neoproterozoic period, corresponding to the Jinning movement in central Yunnan. | ZHANGYongbei WANGGuilan NIEJianfeng ZHAOChongshun XUChengyan QIUJiaxiang WangHao | 2003 | Acta Geologica Sinica(English Edition)2003，77，2： | 2 |
| 3 | 辽宁省重要矿产成矿系列与成矿谱系显示文摘辽宁省是全国重要的矿产资源生产基地,为国家建设提供了大量的矿产资源。运用成矿系列的理论和方法,以辽宁省区域构造演化为基础,充分研究省内在一定的时间和环境中,与一定成矿作用有关的重要矿产的成矿地质背景、成矿环境、成矿时代、成矿作用、成矿演化规律,以及与矿床形成有关的地层、岩浆岩、构造、围岩蚀变等特征。重新厘定了辽宁省重要矿产成矿系列,划分了16个成矿系列、17个成矿亚系列。从成矿环境、成矿时代的横向上与构造单元、矿集区的垂向上,结合成矿作用、矿床组合划分了成矿谱系。最后阐述了成矿系列及成矿谱系的特征。辽宁省重要矿种成矿系列和成矿谱系的划分,对深入研究辽宁省区域成矿规律和指导矿产勘查工作具有深远的意义。 | 刘长纯 | 2017 | 地质科技情报2017，36，1： | 2 |
| 4 | 遥感信息技术在德钦佛山找矿实践中的应用显示文摘基于成矿地质背景分析基础,采用遥感信息技术中图像处理增强、解译等方法,提取与成矿相关的线性、环形构造遥感信息,通过遥感影像上色彩的异常,指导该区地质找矿。 | 王亚萍 高建国 覃荣高 高星刚 | 2009 | 云南地质2009，28，2： | 0 |
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