共查询到16条相似文献,搜索用时 629 毫秒
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介绍GPS技术在龙脖河龙矿区控制测量中的特点与应用效果,并结合工程实践总结了GPS技术在有色金属矿产地质勘查基础测绘中首次应用的体会。 相似文献
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龙脖河铜矿区东矿带火山岩特征 总被引:3,自引:0,他引:3
龙脖河铜矿区东矿带铜矿资源量已达大型规模,其含矿母岩为一套深海相变钠质(含铜)基性火山岩,岩石学、岩石化学特征与大红山铜矿区火山岩相似,成矿地质环境相同,推测其深邯可能还赋存有大型块状硫化物型铜铁矿床,是较具找矿潜力的地区。 相似文献
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龙脖河铜矿区(北段)岩浆岩及矿化 总被引:3,自引:0,他引:3
龙脖河铜矿产于中三叠统个旧组灰岩及其下伏地层中下三叠统火山岩建造中。矿床的形成与以红河断裂和阿龙古断裂为界的深海红河裂陷槽海相火山活动及后期的热液蚀变关系密切,矿化受地层、火山活动构造控制。富钠细碧角斑岩、火山碎屑岩、基性侵入岩为该区的主要岩浆岩类型。上述不同岩浆岩均有矿化产出,本文就区内岩浆岩的特征及其与矿化的关系作一简略的探讨。 相似文献
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金平龙脖河矿区东带火山岩特征及含矿性研究 总被引:2,自引:0,他引:2
本文是笔者通过大量实际资料,对金平龙脖河地区一套海相喷发(溢)的火山岩岩石特征及含矿性分析,确定该区火山岩属细碧-角斑岩建造,其成矿作用和规模与岩浆活动强弱,火山机构,岩性,岩相变化密切相关。 相似文献
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冯开平 《有色金属矿产与勘查》1998,7(2):102-106
龙脖河铜矿带以红河断裂为界,分为东、西两个矿带,东矿带铜矿化赋存于五个层位中。本文系统地研究总结了这五个矿化层的磁、电、化参数特征,探讨了成矿成晕机理,提出了“一高、一中、一低、一多”的地球物理化学异常模式,并在具体的找矿实践中取得了较好的效果。 相似文献
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龙脖河地区构造——地层及成矿作用讨论 总被引:1,自引:0,他引:1
李采一 《有色金属矿产与勘查》1999,8(6):325-328
龙脖河地区地层系统是一套由印支(青藏滇)板块俯冲碰撞扬子板块造出时形成的混杂的构造复合地质体。其主体地层应为二叠纪的泥砂质-火山岩建造,混有元古宙岩块和三叠块岩块。基优矿作用主要受二叠纪火山岩相及火山机构控制。采用造山带区域针层学--非史密斯地层学方法来恢复其原始状态,有利于查明成矿作用、矿体产出规律、找矿才会有新的突破。 相似文献
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云南龙脖河铜矿区东带矿床成因及找矿方向探讨 总被引:1,自引:0,他引:1
古老的变钠质中基性火山杂岩--细碧-角斑岩是龙脖河矿区东带铜矿床的成矿基础,在经历了长期的构造变质变形作用后,它形成了两类最具工业开采价值的铜矿床,矿床的形成与火山喷发活动和后期构造作用关系密切,成矿作用多期次特征明显. 相似文献
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云南龙脖河铜矿区东矿带成矿条件、控矿规律研究 总被引:2,自引:1,他引:1
云南金平龙脖河铜矿区, 除铜外还伴有金、铁矿化,东矿带目前累计估算铜资源量已达100万t,具有矿床埋藏较浅、规模大、品位高、矿石质量好、交通便利、容易开采的特点,矿床受地层岩性、构造、海相中基性火山岩等因素控制特征明显,属海相火山块状硫化物型铜矿床,是云南三江南段找矿有较大突破的区带. 相似文献
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龙脖河铜矿床位于滇中地区红河成矿带南段,矿区火山岩发育、与铜矿化时空密切共生。区内火山岩遭受了不同程度的蚀变或区域变质作用,根据矿物组合可分为变安山岩、变次火山岩和变基性火山岩。三类变火山岩均相对富Na,在地球化学分类图解上样品主要位于碱性玄武岩区域。除个别微量元素外,三类岩石的微量元素含量相近,与各种构造环境玄武岩相比,本区变火山岩富集HFSE(Th、Nb等)、亏损LILE(Sr、Ba等),微量元素配分模式出现明显Th、Nb正异常和Sr、Ba负异常。三类岩石的REE含量范围相互重叠,除Eu异常外,其REE配分模式均为相似的LREE富集型。各种地球化学证据表明,本区三类变火山岩为同源岩浆不同演化阶段的产物,其原始岩浆为大陆板内拉张构造环境交代富集地幔部分熔融的产物,结晶分异作用在岩浆演化过程中具有重要地位。 相似文献
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大理-剑川地区分布一套新生代火山岩,称剑川组。以洱海断裂带为界,东侧主要为基性,超基性岩,西侧主要为粗面岩。据火山岩系沉积特征及所含植物化石判断,喷发期为中新世,原划分的双河组,剑川组应是同期产物。 相似文献
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H.A. Wanas 《地学前缘(英文版)》2011,2(4):491-507
Lower Paleozoic rocks exposed in various regions of Egypt (south central Sinai, north Eastern Desert and southwest Western Desert), in addition to occurring in the subsurface such as north Western Desert and the Gulf of Suez. The Lower Paleozoic rocks in Egypt include surface and subsurface rock units of formational status. The surface rock units are the Taba, Araba and Naqus formations. The subsurface rock units include the Shifa, Kohla and Basur formations.
The Infracambrian Taba Formation has been discovered recently in the outcrops of the south eastern Sinai in the Taba-Ras El-Naqab area. It is missing and/or not recognized in the subsurface. The Taba Formation consists mainly of reddish brown, unfossiliferous gravelly fine-to medium-grained sandstones cemented by kaolinite and have subordinate beds of paleosols. The Cambrian Araba Formation and its subsurface equivalent (the Shifa Formation) are essentially composed of reddish brown, fine-grained laminated sandstone and siltstone with abundant Skolithos and Cruziana sp. In contrast, the Ordovician-Silurian Naqus Formation and its subsurface equivalents (Kohla Formation and Basur Formation) are mainly composed of white, unfossiliferous, cross-bedded, medium- to coarse-grained sandstones with haphazardly distributed pebbles and cobbles. Sedimentological analysis indicates that the Araba Formation and its equivalents were deposited in a marginal-marine environment, whereas the Naqus Formation and its equivalents were laid down in a fluvio-glacial environment.
Integrated stratigraphic and sedimentological studies of the Lower Paleozoic rocks permit reconstruction of the paleogeography of Egypt at that time. Egypt has been largely controlled since the Cambrian by the pre-existing structural framework of the pre-Phanerozoic basement rocks inherited from the Late Proterozoic Pan-African event. Additionally, sedimentation processes were controlled during Cambro-Ordovician times by tectonic movements, whereas glacio-eustatic control predominated during the Late Ordovician-Silurian Period. These studies suggest that most areas of Egypt were exposed lands with episodically transgression by epicontinental seas related to the paleo-Tethys. These lands formed a part of a stable subsiding shelf at the northern Gondwana margin. 相似文献