稀有金属, 2015, 34(6): 400-406. doi: 10.1007/s12598-014-0361-9
Zhen-Liang Yang 1, , Li-Gen Wang 2, , Li-Min Wang {"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"简要介绍了冬瓜山矿床开采情况,探讨了冬瓜山矿床实现深井安全、高效、合理开采所需解决的难题,并提出了解决问题的措施和建议.","authors":[{"authorName":"余茂杰","id":"72b67937-bfa2-4ad3-88ef-ee6ac15fa4c2","originalAuthorName":"余茂杰"},{"authorName":"孙坚刚","id":"9b261a1f-becb-4697-99c7-c7393f1adead","originalAuthorName":"孙坚刚"}],"doi":"10.3969/j.issn.1001-1277.2006.11.007","fpage":"22","id":"dda08d88-eafc-4a3d-b095-8ee1409be862","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"2ab6e43b-5f2b-4ae2-81d7-31e08e581ab7","keyword":"冬瓜山矿床","originalKeyword":"冬瓜山矿床"},{"id":"bdad33d2-a968-437b-b2af-bcac1f97f69e","keyword":"深井开采","originalKeyword":"深井开采"},{"id":"e2956675-f5ce-410d-8f54-8779693c29ae","keyword":"安全生产","originalKeyword":"安全生产"}],"language":"zh","publisherId":"huangj200611007","title":"冬瓜山矿床深井开采安全生产问题的探讨","volume":"27","year":"2006"},{"abstractinfo":"冬瓜山矿床是铜陵矿集区内一个大型的斑岩?矽卡岩型铜(金)多金属矿床，矿区内的燕山期青山脚中酸性侵入岩体与成矿有直接的成因联系。在对青山脚岩体地质特征研究的基础上，进行了详细的岩相学观察和系统的岩石化学、微量元素和稀土元素地球化学研究。分析了岩浆起源、成岩动力学环境及岩体的成岩作用过程，并对青山脚岩体的成岩机制进行了探讨。结果表明，青山脚岩体为高钾钙碱性岩石，具有富集轻稀土元素、Th、Rb和Sr，亏损重稀土元素、Ba、Nb和Ta的特征。形成成矿岩体的原始岩浆来源于地幔玄武质岩浆和下地壳部分熔融产生的正长岩岩浆的混合，其成岩动力学环境为挤压到伸展的过渡环境。Harker图解和长石的混合结构表明，岩浆在演化过程中发生了自身的分离结晶作用，岩石化学及微量元素、稀土元素特征表明成岩过程中受到了地壳物质的混染。本区岩体是由壳幔混合岩浆在碰撞后的伸展环境中经过自身的分离结晶作用和与地壳的同化混染作用而形成的。","authors":[{"authorName":"刘忠法","id":"0630807c-356b-47a7-bd1a-affbc11c3724","originalAuthorName":"刘忠法"},{"authorName":"邵拥军","id":"5157c337-171d-4c4a-9072-e99356722ed5","originalAuthorName":"邵拥军"},{"authorName":"隗含涛","id":"4622c20d-333e-476e-a695-93f679bd333e","originalAuthorName":"隗含涛"},{"authorName":"汪程","id":"31bcbff9-d8ac-4013-bd6a-35c409b3a2be","originalAuthorName":"汪程"}],"doi":"10.1016/S1003-6326(16)64365-0","fpage":"2449","id":"9aeebe9e-7f8c-4a04-b906-25baea4f7903","issue":"9","journal":{"abbrevTitle":"ZGYSJSXBEN","coverImgSrc":"journal/img/cover/ZGYSJSXBEN.jpg","id":"757390d2-7d95-4517-96f1-e467ce1bff63","issnPpub":"1003-6326","publisherId":"ZGYSJSXBEN","title":"中国有色金属学报(英文版)"},"keywords":[{"id":"f537a6e6-edf0-48fa-9c4d-3f14e87db9f3","keyword":"青山脚岩体","originalKeyword":"青山脚岩体"},{"id":"0b1aad97-4710-4152-932b-2c8c3e6372fb","keyword":"地质地球化学特征","originalKeyword":"地质地球化学特征"},{"id":"6a393eca-913c-4c3d-ae42-3272360377e6","keyword":"成岩动力学环境","originalKeyword":"成岩动力学环境"},{"id":"77b31efb-8ec8-4ecf-acf3-e289d17e93cc","keyword":"岩浆起源","originalKeyword":"岩浆起源"},{"id":"e063e8ff-ac10-4bfd-b49d-f033f9a2f1ef","keyword":"成岩作用","originalKeyword":"成岩作用"},{"id":"18e2ed75-f98f-424e-96d8-f99a9889726c","keyword":"冬瓜山铜(金)多金属矿床","originalKeyword":"冬瓜山铜(金)多金属矿床"}],"language":"zh","publisherId":"zgysjsxb-e201609022","title":"安徽铜陵冬瓜山矿床青山脚岩体的成岩机制","volume":"26","year":"2016"},{"abstractinfo":"冬瓜山铜矿大团山矿床开采设计生产能力为1800 t/d,其中- 580 m中段开采系统于2006年底投产.经过几年开采,- 580 m以上开采的资源逐渐枯竭,为了保证矿山生产衔接,实现大团山矿床安全、高效开采,对大团山矿床-580 m以下矿体采矿方法的科学、合理选择显得尤为重要.在分析大团山矿床开采技术条件及开采实践经验基础上,对大团山-580 m以下矿床开采提出了大直径深孔和中深孔落矿的阶段空场嗣后充填采矿法,详述了盘区划分、回采工艺以及开采时应注意的安全措施.","authors":[{"authorName":"黄浩辉","id":"9d351431-547d-457a-86a6-a8fe8f84eb25","originalAuthorName":"黄浩辉"},{"authorName":"苏卫宏","id":"0870e530-e17e-454e-8a21-148c23417551","originalAuthorName":"苏卫宏"},{"authorName":"古绪球","id":"1d74ec55-4eae-47d0-99d2-3389b4ae3adf","originalAuthorName":"古绪球"}],"doi":"10.3969/j.issn.1001-1277.2011.09.008","fpage":"32","id":"4ffaeffc-3771-41d1-90e7-b74daf8b8609","issue":"9","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"d14e6620-57f1-44db-b55c-17247e39b7f5","keyword":"大团山矿床","originalKeyword":"大团山矿床"},{"id":"62dd60d5-1d23-42a4-bc63-e69f1cf02ebc","keyword":"大盘区","originalKeyword":"大盘区"},{"id":"27eea72d-08bb-4954-b191-34da5cbb58b2","keyword":"中、深孔落矿","originalKeyword":"中、深孔落矿"},{"id":"e91dbb62-b067-410e-8a3c-4b701a43cc4e","keyword":"阶段空场","originalKeyword":"阶段空场"},{"id":"041f4474-b98b-4aca-a4bc-1b97cfe1a161","keyword":"嗣后充填","originalKeyword":"嗣后充填"}],"language":"zh","publisherId":"huangj201109008","title":"大团山矿床-580m以下矿体采矿方法选择的探讨","volume":"32","year":"2011"},{"abstractinfo":"有些开采多年的老矿山,矿床开采完了,矿床外围又发现新矿床.新矿床的开采又借用了老矿床的井口、提升、排水等设施.但老矿床几十年开采形成的采掘空间,往往涌水量较大,增加了新矿床的开采成本.如何兴利除弊,对老矿床封水?沂南金矿做了大胆实践,效果很好.","authors":[{"authorName":"袁封传","id":"56d909c3-6b56-4dce-93e0-46d0208f3420","originalAuthorName":"袁封传"},{"authorName":"丛顺明","id":"1cf0bf90-bd2c-405f-94bf-b3d71bdf2674","originalAuthorName":"丛顺明"},{"authorName":"高乃宝","id":"56ac3de9-2e81-4d75-b1c2-44f7abfe6e81","originalAuthorName":"高乃宝"},{"authorName":"张文国","id":"6c7b64fb-fc3d-4100-91d1-c1c07a37aede","originalAuthorName":"张文国"}],"doi":"10.3969/j.issn.1001-1277.2002.04.005","fpage":"31","id":"f9ec60b6-09e1-4fd7-9b98-8c9e5182b660","issue":"4","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"b5d5cacb-11ef-424c-b27c-b4f08f06f14e","keyword":"矿床","originalKeyword":"矿床"},{"id":"968c28f9-e06f-43cf-ac60-791eac0a84f4","keyword":"封水","originalKeyword":"封水"},{"id":"9d36151c-69cc-4b17-a23c-06869bb4df3e","keyword":"实践","originalKeyword":"实践"}],"language":"zh","publisherId":"huangj200204005","title":"山子涧矿床封水实践","volume":"23","year":"2002"},{"abstractinfo":"松树南沟金矿床位于祁连造山带北祁连加里东造山亚带南缘,靠近达坂山深大断裂带,成矿地质条件非常有利.文章在阐述成矿地质背景的基础上,详细论述了松树南沟金矿床的地质特征,并对矿床成因进行了探讨.认为晚华力西-印支期陆内碰撞造山活动叠加,沿达坂山深大断裂带旁侧形成规模较大的北西向韧性剪切带,并发生中酸性岩浆侵入活动,使原有成矿物质活化、迁移、富集、沉淀,形成了松树南沟造山型金矿床.","authors":[{"authorName":"伊有昌","id":"060d2fb3-8552-4545-897e-979812b4e54f","originalAuthorName":"伊有昌"},{"authorName":"陈树云","id":"d86fe74c-a7c6-4385-9b8d-80c4cf107dd7","originalAuthorName":"陈树云"},{"authorName":"文雪峰","id":"89afa6d9-bb1f-45ca-a56d-c7c9cee31959","originalAuthorName":"文雪峰"}],"doi":"10.3969/j.issn.1001-1277.2006.10.004","fpage":"16","id":"5b739b40-3ee3-4cb6-9ab3-5a7dab3d3103","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"ba584b1c-fd4d-463a-9dfa-aa78669e37b4","keyword":"矿床地质特征","originalKeyword":"矿床地质特征"},{"id":"d6468f9c-aa03-4d48-85d7-ff68208a3be2","keyword":"矿床成因","originalKeyword":"矿床成因"},{"id":"a8bbadb4-d2e7-4a63-b0ca-71981239af13","keyword":"北祁连","originalKeyword":"北祁连"},{"id":"a7e897e3-b760-4dd1-b7db-261b7ae3f3f5","keyword":"松树南沟金矿床","originalKeyword":"松树南沟金矿床"},{"id":"516272ad-bced-4dcc-afb8-9562ce332e68","keyword":"造山型金矿床","originalKeyword":"造山型金矿床"}],"language":"zh","publisherId":"huangj200610004","title":"青海北祁连松树南沟造山型金矿床地质特征及矿床成因","volume":"27","year":"2006"},{"abstractinfo":"三山岛金矿床位于胶东西北部，属于典型的“焦家式”（破碎带蚀变岩型）金矿床。对矿区内主成矿阶段石英中的流体包裹体进行了岩相学、显微测温、氢氧同位素及单个包裹体成分激光拉曼光谱研究。研究表明，矿石中流体包裹体主要有纯CO2单相包裹体、气液二相包裹体和含CO2三相包裹体3种类型；矿石石英中流体包裹体普遍富含CO2；成矿过程中，流体经历了CO2－NaCl－H2 O体系的不混溶作用；成矿流体具有低盐度（3．85％～11．60％）、低密度（0．70～0．96 g／cm3）的特点；主成矿温度集中为260～320℃，成矿压力范围为70～110 MPa，相应（成矿）深度范围为6．78～8．69 km。结合流体包裹体氢氧同位素分析认为，三山岛金矿床成矿流体以地幔流体为主，并有少量的岩浆流体。确定矿床成因类型为为幔源流体参与成矿的中温热液脉型金矿床。","authors":[{"authorName":"桂飞","id":"ce43e1e9-b020-4a06-8918-518f51a38f39","originalAuthorName":"桂飞"},{"authorName":"王力","id":"62612c2f-731a-482d-b2c3-d3ee6c468243","originalAuthorName":"王力"},{"authorName":"马芳","id":"d3098ceb-8729-4758-89cf-1b03a670ecc6","originalAuthorName":"马芳"}],"doi":"10.11792/hj20141106","fpage":"27","id":"d70e911b-4f0c-4e0e-8fda-8909ccd26202","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"8395b497-710e-481d-a1f2-19efde1f6ba9","keyword":"流体包裹体","originalKeyword":"流体包裹体"},{"id":"38b9fcff-430c-4c57-bd9d-3d180e46fc38","keyword":"成矿流体","originalKeyword":"成矿流体"},{"id":"0bb37973-ce37-416b-b595-51ca7ef2f8bc","keyword":"氢氧同位素","originalKeyword":"氢氧同位素"},{"id":"f214160f-4c4d-467f-b811-310debe321be","keyword":"三山岛金矿床","originalKeyword":"三山岛金矿床"},{"id":"4d719f41-a62d-4bdf-9c54-71f0e7208622","keyword":"胶西北","originalKeyword":"胶西北"}],"language":"zh","publisherId":"huangj201411006","title":"三山岛金矿床流体包裹体研究","volume":"","year":"2014"},{"abstractinfo":"哀牢山构造带是西南三江地区最重要的金多金属成矿带之一,也是世界上著名的构造岩浆带之一.哀牢山构造带由于受印度-欧亚大陆碰撞以及喜马拉雅造山带地质构造演化影响,成矿构造复杂,成矿条件优越,构造带内金矿床类型复杂.从矿床应用类型的角度,将哀牢山构造带的金矿床划分7种金矿床类型.袁牢山构造带金矿成矿作用具有以下突出特点:成矿地质背景统一性,成矿(矿化)类型多样性,成矿时代多期性,成矿物质多源性,矿床空间分布的集中性,成矿过程的复杂性.并总结了哀牢山构造带内金矿床的找矿标志.","authors":[{"authorName":"王治华","id":"a6a5b92b-921d-4fe8-8217-27c113542722","originalAuthorName":"王治华"},{"authorName":"阎家盼","id":"88deb9e4-fe92-4b62-a4a3-757d290f1fec","originalAuthorName":"阎家盼"},{"authorName":"郭晓东","id":"e5d5ddf0-7770-41bd-9c2f-4338f3850f52","originalAuthorName":"郭晓东"},{"authorName":"葛良胜","id":"2b03aefe-0018-4374-b66f-a179b3541449","originalAuthorName":"葛良胜"},{"authorName":"王梁","id":"68332ce2-0eb2-4b7e-a7ea-cf4953564261","originalAuthorName":"王梁"},{"authorName":"喻万强","id":"17645e84-53bb-4eae-80f0-07d58a462441","originalAuthorName":"喻万强"},{"authorName":"徐涛","id":"4a09e1db-8866-4d60-8648-4516199ad701","originalAuthorName":"徐涛"}],"doi":"10.3969/j.issn.1001-1277.2011.04.003","fpage":"7","id":"6155e3f7-eb83-4f60-9e29-10eddaa51329","issue":"4","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"f042c573-e514-4e02-b326-809e47f1615b","keyword":"金矿床类型","originalKeyword":"金矿床类型"},{"id":"e458a5e1-c663-4a74-b6dc-af711d6d69fa","keyword":"成矿规律","originalKeyword":"成矿规律"},{"id":"95d6d5e7-99a8-4419-9bce-55490c39f678","keyword":"找矿标志","originalKeyword":"找矿标志"},{"id":"541a2ba1-729a-4174-ae7d-2c1ad7816dd7","keyword":"牢山构造带","originalKeyword":"牢山构造带"},{"id":"570bcf80-ab6a-4f3c-828f-00803d3a0025","keyword":"西南三江","originalKeyword":"西南三江"}],"language":"zh","publisherId":"huangj201104003","title":"哀牢山构造带金矿床类型及成矿规律","volume":"32","year":"2011"},{"abstractinfo":"韧性剪切带型金矿床作为重要金矿床类型之一，对其进行深入研究具有重要的理论和实际意义。以辽宁排山楼金矿床和广东河台金矿床2个典型韧性剪切带型金矿床为例，对韧性剪切带型金矿床地质特征进行概括和总结。韧性剪切带型金矿床与其赋存的韧性剪切带往往具有形成时间上的滞后效应，矿体严格受韧性剪切带控制，但多分布在韧性剪切带的后期脆性断裂中。剥蚀程度低、长期演化的造山带环境是寻找韧性剪切带型金矿床的战略方向。","authors":[{"authorName":"陈冲","id":"32dad0c0-d39a-4831-b8ec-38ccd6ed1304","originalAuthorName":"陈冲"},{"authorName":"魏俊浩","id":"74ae43c5-e0d5-43ff-b60e-81d927b1e9ed","originalAuthorName":"魏俊浩"},{"authorName":"付乐兵","id":"e7344d4a-3dbd-4071-97a3-e9ac6e22e5ae","originalAuthorName":"付乐兵"}],"doi":"10.11792/hj20131004","fpage":"12","id":"e6bf401a-d8b5-4d0c-bed2-540209f5365c","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"6144e561-b71a-4269-8bd5-f4373b3a3eb1","keyword":"韧性剪切带型金矿床","originalKeyword":"韧性剪切带型金矿床"},{"id":"2d1d1ceb-83d8-45de-9b57-9b704fccf782","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"e6efb9c8-75c5-47f6-9dea-cacd4f385476","keyword":"排山楼金矿床","originalKeyword":"排山楼金矿床"},{"id":"a6a67657-f9aa-4511-9387-1123023a9940","keyword":"河台金矿床","originalKeyword":"河台金矿床"}],"language":"zh","publisherId":"huangj201310006","title":"韧性剪切带型金矿床地质特征研究--以辽宁排山楼金矿床与广东河台金矿床为例","volume":"","year":"2013"},{"abstractinfo":"蛇屋山金矿床是20世纪90年代初在鄂南地区发现的最大规模的卡林型金矿床,与其相邻的富水卡林型金矿床也属同种类型.在总结前人有关研究成果的基础上,综合分析蛇屋山与富水卡林型金矿床的成矿地质条件,认为二者具有相同的成矿地质背景和矿床地质特征,并且形成于同一时期.因此,认为鄂南地区具有较好的卡林型金矿床找矿远景,并以此为基础初步对鄂南地区卡林型金矿床的找矿标志进行了总结.","authors":[{"authorName":"刘蕴光","id":"a200699b-092f-4b8e-9723-be9ac8303c46","originalAuthorName":"刘蕴光"},{"authorName":"王敏芳","id":"41d4eb3e-fc20-4f41-92f3-2d243f09d640","originalAuthorName":"王敏芳"},{"authorName":"肖凡","id":"4ce514fb-bcf2-4387-8b45-b95d3aa7d3b8","originalAuthorName":"肖凡"}],"doi":"10.3969/j.issn.1001-1277.2012.03.004","fpage":"17","id":"0dce0aa6-0214-4ea3-89b9-cb1e1aa0bca4","issue":"3","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"2d551cb1-72ec-4b91-abde-0927da91f612","keyword":"矿床地质特征","originalKeyword":"矿床地质特征"},{"id":"743155ef-ef3a-4c74-a362-fb5a42d045f9","keyword":"找矿标志","originalKeyword":"找矿标志"},{"id":"edf27bbe-2994-4b80-bf1e-c10e2eef327e","keyword":"卡林型金矿床","originalKeyword":"卡林型金矿床"},{"id":"6e8ac59a-e52e-4f02-9e1c-5f85feb1da1c","keyword":"蛇屋山金矿床","originalKeyword":"蛇屋山金矿床"},{"id":"066875e1-ab77-493b-8c18-57ff0832b163","keyword":"富水金矿床","originalKeyword":"富水金矿床"},{"id":"01aa0b3c-f0c2-4933-a0ad-fef11ab7952e","keyword":"鄂南地区","originalKeyword":"鄂南地区"}],"language":"zh","publisherId":"huangj201203004","title":"鄂南地区蛇屋山与富水卡林型金矿床的矿床地质特征对比及找矿标志研究","volume":"33","year":"2012"},{"abstractinfo":"破碎带蚀变岩型金矿床是河南熊耳山矿集区最重要的金矿床类型，空间上常成群成带分布，且具有明显的方向性、等距性。矿集区内破碎带蚀变岩型金矿床的控矿构造主要是呈北东向展布的7条断裂破碎带，金矿化多集中出现于控矿断裂交汇复合部位及断裂的中央、局部拐折、弯曲、派生分支裂隙出现的地段。","authors":[{"authorName":"李国平","id":"6c17d613-9368-4c6f-8ec9-d74315d31961","originalAuthorName":"李国平"}],"doi":"10.11792/hj20130707","fpage":"22","id":"83d3c175-773b-4699-a585-81344ba3a528","issue":"7","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"fd64ac47-253e-467d-aee4-94ef19470016","keyword":"熊耳山矿集区","originalKeyword":"熊耳山矿集区"},{"id":"2fe4ab11-5294-43e6-b5ab-6d16918f23ca","keyword":"破碎带蚀变岩型金矿床","originalKeyword":"破碎带蚀变岩型金矿床"},{"id":"818a0941-ee32-45c0-aa30-0e136c40f0c3","keyword":"构造控矿规律","originalKeyword":"构造控矿规律"},{"id":"a1c41d49-0ed6-49b0-9968-9924bc5a32fc","keyword":"河南省","originalKeyword":"河南省"}],"language":"zh","publisherId":"huangj201307008","title":"河南熊耳山矿集区破碎带蚀变岩型金矿床构造控矿规律研究","volume":"","year":"2013"}],"totalpage":83,"totalrecord":830}