{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"采用敏化–活化两步法对云母粉进行预处理后再化学镀银。研究了镀液pH、银含量和云母粉与AgNO3质量比对镀银云母粉导电性的影响。通过红外光谱仪和X射线衍射仪表征了镀银云母粉的组织结构。通过表面形貌分析，研究了粗化预处理对云母粉化学镀银效果的影响。结果表明，粗化可提高粉体表面的粗糙度，使后续银镀层更致密。当AgNO3投加量为15 g/L，云母粉与AgNO3质量比为2.5∶1，pH为12时，银沉积率最高，镀银云母粉的表面形貌和导电性最好(体积电阻率约0.088?·cm)。化学镀银云母粉有望替代部分银粉作为导电填料，并在涂料或塑料等高分子材料中应用。","authors":[{"authorName":"李祝","id":"8309a22a-d146-49b0-868d-88f54f8dc322","originalAuthorName":"李祝"},{"authorName":"李红","id":"8994f130-b80d-4087-b1c4-507d89e5b102","originalAuthorName":"李红"},{"authorName":"<span style=\"color:red\">洪</span><span style=\"color:red\">旭</span><span style=\"color:red\">城</span>","id":"de0910a3-35d5-4145-be8e-ed0385e56d52","originalAuthorName":"洪旭城"},{"authorName":"张志伟","id":"7faba7a2-de35-4467-836a-3d009a0f1149","originalAuthorName":"张志伟"}],"doi":"","fpage":"491","id":"27f7bcba-8938-4d99-9b5e-d2f16cda2f46","issue":"9","journal":{"abbrevTitle":"DDYTS","coverImgSrc":"journal/img/cover/DDYTS.jpg","id":"21","issnPpub":"1004-227X","publisherId":"DDYTS","title":"电镀与涂饰   "},"keywords":[{"id":"8af08890-2a91-453d-8742-fdadeba5dae9","keyword":"云母","originalKeyword":"云母"},{"id":"c40787f4-0d73-4055-9efb-e714f76cc959","keyword":"化学镀银","originalKeyword":"化学镀银"},{"id":"1211c999-e95b-4c69-9430-cf06fa914f6f","keyword":"粗化","originalKeyword":"粗化"},{"id":"2473e87c-c9c6-4240-83a5-fa6b1ef99dfe","keyword":"导电填料","originalKeyword":"导电填料"},{"id":"a51b00ea-ca0f-497d-9b9a-d42298e7c740","keyword":"电阻率","originalKeyword":"电阻率"}],"language":"zh","publisherId":"ddyts201509008","title":"化学镀法制备镀银云母","volume":"","year":"2015"},{"abstractinfo":"班公湖-怒江成矿带跨班公湖-怒江缝合带两侧，是近年来发现的一条重要的多金属成矿带。商<span style=\"color:red\">旭</span>金矿床位于班公湖-怒江缝合带中段，主要矿体呈透镜状或脉状产于中-下侏罗统木嘎岗日群浅变质海相复理石建造中，受近东西向断裂构造控制。矿石类型以石英脉型为主，其次为蚀变岩型，近矿围岩蚀变较弱，蚀变类型包括硅化、绢云母化、绿泥石化、碳酸盐化等。矿石中金属矿物主要为自然金、黄铁矿及方铅矿；脉石矿物以石英、方解石以及黏土矿物为主。初步研究表明，该矿床主要受地层及构造因素控制，成因类型为造山型金矿床。在此基础上，初步总结了矿区的主要找矿标志，包括岩性及构造标志、蚀变标志、硫化物标志、化探异常及古采矿遗迹标志等，并认为区域上存在找到商<span style=\"color:red\">旭</span>式金矿床的可能。","authors":[{"authorName":"肖万峰","id":"1d451ac3-887c-4617-a0ca-158b639eee34","originalAuthorName":"肖万峰"},{"authorName":"李光明","id":"a43a9f64-db4e-4ae7-a4db-ad6b5c6fdf01","originalAuthorName":"李光明"},{"authorName":"黄瀚霄","id":"4bd70593-6e2d-4a4a-a476-a8499e8e8141","originalAuthorName":"黄瀚霄"},{"authorName":"马东","id":"62242f64-8b3e-453d-90b4-3cdd52646587","originalAuthorName":"马东"},{"authorName":"张智林","id":"4e3ebf94-f1d0-409d-a4e6-f99d952597d4","originalAuthorName":"张智林"},{"authorName":"曲扎","id":"e0763d49-69d4-429c-ba6a-eba9484badf0","originalAuthorName":"曲扎"}],"doi":"10.11792/hj20131005","fpage":"17","id":"64eb054f-8d90-414b-8571-cdbe479e8b5b","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"e38f1f96-a61b-4a64-b5d5-cf076ed042d1","keyword":"商<span style=\"color:red\">旭</span>金矿床","originalKeyword":"商旭金矿床"},{"id":"222c536e-17cf-4583-ac2e-eb9910f27ce7","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"84cc3253-435b-48e9-8036-2a247c1b10b7","keyword":"控矿因素","originalKeyword":"控矿因素"},{"id":"e472e283-83a4-4b15-bdbe-041026cc787a","keyword":"矿床成因","originalKeyword":"矿床成因"},{"id":"55fa1374-bf4f-4361-8758-6b26fa5c71d1","keyword":"找矿标志","originalKeyword":"找矿标志"},{"id":"b817b4f3-ad9b-4e53-b2d3-2fafe0695a73","keyword":"藏北","originalKeyword":"藏北"}],"language":"zh","publisherId":"huangj201310007","title":"藏北商<span style=\"color:red\">旭</span>金矿床控矿因素及其找矿标志","volume":"","year":"2013"},{"abstractinfo":"鑫<span style=\"color:red\">城</span>金矿属高品位、急倾斜、椭圆形柱状矿体,矿石不稳固,矿岩界限不清.露天转地下开采后应用空场采矿法开采,致使预留的护顶矿柱冒落,采场与露天坑相通,露天边坡大量冒落的废石混入已采下矿石造成严重贫化.为此,重新确定适应该矿体开采的采矿方法,安全生产,减小贫化,提高效益成为矿山的当务之急.文中针对露天转地下开采问题进行了分析研究,并介绍了推荐方案的主要特征.","authors":[{"authorName":"王志学","id":"645d83dc-caf9-465e-a6ea-3f5e33748498","originalAuthorName":"王志学"},{"authorName":"邢万芳","id":"ad42c8d6-0620-49f4-a54d-ea0fda8846aa","originalAuthorName":"邢万芳"}],"doi":"10.3969/j.issn.1001-1277.2004.10.007","fpage":"22","id":"77f7b463-2689-431e-8b72-bc99a375712c","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"fe74edd8-9a76-4d4f-9a56-4b6fd8f7846c","keyword":"露天转地下开采","originalKeyword":"露天转地下开采"},{"id":"cfcf4bb9-ebe8-42b7-8e5e-64bc751b95ef","keyword":"椭圆形柱状矿体","originalKeyword":"椭圆形柱状矿体"},{"id":"f72f4372-6f05-4a7a-b37a-7d16a854c504","keyword":"损失贫化","originalKeyword":"损失贫化"},{"id":"96ed5a6a-34f9-418e-b013-533ad628ea96","keyword":"分段崩落采矿法","originalKeyword":"分段崩落采矿法"}],"language":"zh","publisherId":"huangj200410007","title":"浅谈鑫<span style=\"color:red\">城</span>金矿露天转地下开采问题","volume":"25","year":"2004"},{"abstractinfo":"文中介绍了鑫<span style=\"color:red\">城</span>金矿地下矿与选矿厂进行改扩建的可行性,为矿山正常生产与不断发展提供了技术保障.","authors":[{"authorName":"王彦慧","id":"147c88df-9add-43ad-be2e-704854a26882","originalAuthorName":"王彦慧"},{"authorName":"张宏达","id":"286cb563-ded6-46ff-9089-3f6b277dafa1","originalAuthorName":"张宏达"},{"authorName":"于宏业","id":"fa304b5d-0e72-40ce-8d0c-3862d92a3fac","originalAuthorName":"于宏业"},{"authorName":"王天野","id":"d9e45976-8168-4570-b0f1-f84511767709","originalAuthorName":"王天野"}],"doi":"10.3969/j.issn.1001-1277.2001.11.006","fpage":"22","id":"489fb775-dd2d-4f28-9a02-444fbe2e6698","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"b53d7eba-a020-40d2-aa1f-a95cc9a7ea66","keyword":"改扩建","originalKeyword":"改扩建"},{"id":"d8df6087-24fd-4ef4-ae37-77441c897a64","keyword":"预可行性","originalKeyword":"预可行性"},{"id":"3fe653c9-1279-46e1-9357-04a574148e02","keyword":"研究","originalKeyword":"研究"}],"language":"zh","publisherId":"huangj200111006","title":"鑫<span style=\"color:red\">城</span>金矿改扩建工程预可行性研究探讨","volume":"22","year":"2001"},{"abstractinfo":"郭<span style=\"color:red\">城</span>断裂带作为郯庐断裂的次级导矿构造,控制着该地区金矿床的分布和产出,并且金矿床还受胶莱盆地边缘层间滑动构造的控制,金矿成矿的地质背景和构造特殊. 从区域成矿背景和矿床特征入手,分析了郭<span style=\"color:red\">城</span>断裂带金矿床的找矿潜力及找矿方向. 分析结果表明,郭<span style=\"color:red\">城</span>断裂带深部存在含矿大岩体,具有很好的金矿成矿条件,找矿潜力巨大,有存在大型金矿床的可能,应该加强该成矿带的找矿工作力度.","authors":[{"authorName":"彭雪峰","id":"1f4ebd1d-12aa-4bdd-9256-76f32c0d5540","originalAuthorName":"彭雪峰"},{"authorName":"姜丽萍","id":"8b8fb11f-f142-44cc-8f23-4b04555b9da7","originalAuthorName":"姜丽萍"},{"authorName":"郝兴春","id":"a2098b2b-1c59-449d-97ec-18da92bc1f2a","originalAuthorName":"郝兴春"},{"authorName":"王龙江","id":"30a91aa0-aad9-4f48-a398-50018b5d4deb","originalAuthorName":"王龙江"},{"authorName":"李明昱","id":"8f9ed102-f30c-4269-ac17-7b24aad6ad5d","originalAuthorName":"李明昱"}],"doi":"10.11792/hj20151104","fpage":"13","id":"8692ae86-9f4b-43e8-a348-90458a6115e2","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"12241c16-9d10-498b-8e64-75e50d4ec734","keyword":"金矿床","originalKeyword":"金矿床"},{"id":"5fe87290-3e9d-4c4a-bd67-6d3521e3bd08","keyword":"找矿潜力","originalKeyword":"找矿潜力"},{"id":"aa4448af-c278-4545-9715-e7010ee02120","keyword":"郭<span style=\"color:red\">城</span>断裂带","originalKeyword":"郭城断裂带"},{"id":"f37a6dc8-6d08-45fc-b511-f1ebf172a8cc","keyword":"胶东","originalKeyword":"胶东"}],"language":"zh","publisherId":"huangj201511004","title":"胶东郭<span style=\"color:red\">城</span>断裂带金矿找矿潜力分析","volume":"36","year":"2015"},{"abstractinfo":"对江西<span style=\"color:red\">洪</span>州窑从东汉晚期至晚唐五代8期400个瓷胎样品进行了中子活化分析, 分析结果显示碱金属元素Na和Rb、碱土金属元素Ba及Fe等作为胎的助熔剂元素随年代的变化趋势相似, 都呈现出两头高中间低的U字形变化规律, 其中Fe作为呈色元素, 其含量的高低与瓷胎颜色的深浅是一致的.分析结果还揭示<span style=\"color:red\">洪</span>州窑的发展与衰落以及窑址的不断变迁可能都与制瓷原料的发现与消耗有关.对分析数据进行主成分分析, 可以将不同时期烧制的瓷胎样品大致分为5组: (1)东汉晚期东吴时期; (2)两晋和南朝时期; (3)隋代; (4)初唐和盛唐时期; (5)晚唐五代时期.","authors":[{"authorName":"冯向前","id":"bb73e52d-559b-4aa0-9509-23f003727157","originalAuthorName":"冯向前"},{"authorName":"冯松林","id":"13c25759-1db8-425f-b21e-84ae056cff1f","originalAuthorName":"冯松林"},{"authorName":"张文江","id":"8d96cc12-6a67-4944-817b-215bb3dec0c3","originalAuthorName":"张文江"},{"authorName":"樊昌生","id":"e5d11a72-233a-41c4-a38d-1904e5cfad2a","originalAuthorName":"樊昌生"},{"authorName":"权奎山","id":"1f96e504-74c9-4ce8-88b5-559409c26f07","originalAuthorName":"权奎山"}],"doi":"10.3969/j.issn.1007-4627.2005.01.043","fpage":"142","id":"70359f2b-8369-4007-987f-7444de816237","issue":"1","journal":{"abbrevTitle":"YZHWLPL","coverImgSrc":"journal/img/cover/YZHWLPL.jpg","id":"78","issnPpub":"1007-4627","publisherId":"YZHWLPL","title":"原子核物理评论   "},"keywords":[{"id":"5d15414d-1511-4f0b-9870-b7212e945429","keyword":"核分析技术","originalKeyword":"核分析技术"},{"id":"b1f77f43-f953-4410-ad65-387980a986c6","keyword":"<span style=\"color:red\">洪</span>州窑古瓷","originalKeyword":"洪州窑古瓷"},{"id":"3118b21f-e76c-44d6-895c-ff785bb4462d","keyword":"元素特征","originalKeyword":"元素特征"}],"language":"zh","publisherId":"yzhwlpl200501043","title":"历代<span style=\"color:red\">洪</span>州窑古瓷的元素组成特征的中子活化分析研究","volume":"22","year":"2005"},{"abstractinfo":"在热重分析仪上研究沛<span style=\"color:red\">城</span>煤矿天然焦-CO2气化反应特性:比较了不同温度下天然焦与原煤的气化特性,考察了气化反应温度、气化介质CO2流量和操作压力对天然焦-CO2气化反应特性的影响.结果表明:沛<span style=\"color:red\">城</span>煤矿天然焦与原煤的气化特性比较接近,略高于原煤;气化温度对气化反应影响显著;气化温度1000℃、试样质量10 mg左右、常压气化条件下,气化反应气体流量达到60 mL/min时,才基本消除外扩散的影响;随着气化压力的增加,气化反应速率增加,天然焦试样碳转化率增加,同一反应时刻,随压力的增加,试样碳转化率的增加并不呈线性,在较高压力下,压力对二氧化碳与沛<span style=\"color:red\">城</span>煤矿天然焦的还原反应的影响较弱.","authors":[{"authorName":"庞克亮","id":"844d4075-1f1c-47a1-847b-bea287edeaad","originalAuthorName":"庞克亮"},{"authorName":"向文国","id":"06152a2b-85be-4a44-9fe9-f7438dd70b18","originalAuthorName":"向文国"},{"authorName":"赵长遂","id":"4857cf68-9bca-45fb-a8a0-7f186186869c","originalAuthorName":"赵长遂"},{"authorName":"李振中","id":"faacf835-adea-471c-b13a-168f1508aae4","originalAuthorName":"李振中"}],"doi":"","fpage":"165","id":"513f6a08-1630-468b-9dfe-4460786db228","issue":"1","journal":{"abbrevTitle":"GCRWLXB","coverImgSrc":"journal/img/cover/GCRWLXB.jpg","id":"32","issnPpub":"0253-231X","publisherId":"GCRWLXB","title":"工程热物理学报   "},"keywords":[{"id":"03139d53-d15a-41d2-bbf1-b3feb4341c4c","keyword":"天然焦","originalKeyword":"天然焦"},{"id":"228b723c-b58c-4a3b-bd94-c47fb2985a2f","keyword":"气化","originalKeyword":"气化"},{"id":"25ec0e44-d031-4d1a-9fb0-90aa71296a3d","keyword":"XRD","originalKeyword":"XRD"},{"id":"2c4fc3ca-ac3e-4e93-85cf-6ef1f11d01d0","keyword":"热重法","originalKeyword":"热重法"},{"id":"de400b8b-5e73-4495-87b6-eb07e40e3ced","keyword":"催化剂","originalKeyword":"催化剂"}],"language":"zh","publisherId":"gcrwlxb201001046","title":"沛<span style=\"color:red\">城</span>煤矿天然焦-CO2气化特性研究","volume":"31","year":"2010"},{"abstractinfo":"文中通过寻找适合鑫<span style=\"color:red\">城</span>金矿矿岩稳固程度及开采技术条件的最佳采矿方法,对该矿应用非胶结充填采矿方法作一探讨,并对在230～330m之间矿体应用该方法取得的成绩予以总结.","authors":[{"authorName":"张宏达","id":"436ba7e5-86fe-440c-9c4b-fb32d1a79fe0","originalAuthorName":"张宏达"}],"doi":"10.3969/j.issn.1001-1277.2001.01.006","fpage":"25","id":"f8d70563-ffd7-4858-b3cf-b550bf37800d","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"0a84286a-5bde-41ba-8f62-ea4ae599c708","keyword":"胶结充填","originalKeyword":"胶结充填"},{"id":"47a70c78-d119-475d-bced-e70017febda7","keyword":"浅孔留矿采矿法","originalKeyword":"浅孔留矿采矿法"},{"id":"4303ed7e-ea5f-4858-b204-da2e536abec4","keyword":"分段崩落采矿法","originalKeyword":"分段崩落采矿法"},{"id":"b77dea6f-032b-43c3-85fe-f84b8b663fc9","keyword":"探讨与实践","originalKeyword":"探讨与实践"}],"language":"zh","publisherId":"huangj200101006","title":"鑫<span style=\"color:red\">城</span>金矿230～330m之间矿体的采矿方法探讨与实践","volume":"22","year":"2001"},{"abstractinfo":"牧牛山二长花岗岩体是胶东郭<span style=\"color:red\">城</span>地区出露面积最为广泛的岩体,为区内重要的赋矿围岩之一.采用锆石LA-ICPMS U-Pb定年方法,获得岩体结晶成岩年龄为(2 105 ±26)Ma,并经历了约1.85 Ga时期的变质改造事件.岩体侵位与区内金成矿作用时间差距甚远,因此直接提供金或成矿流体的可能性不大.","authors":[{"authorName":"冯波","id":"028fdf62-aa5a-4869-bd32-bd4593db2037","originalAuthorName":"冯波"},{"authorName":"李红梅","id":"b3ba3328-9ae7-4553-8915-5adcdd3b735a","originalAuthorName":"李红梅"},{"authorName":"魏兴亮","id":"110edf70-d81c-41ff-bac1-b9e6f87efa01","originalAuthorName":"魏兴亮"},{"authorName":"陶鑫","id":"e9b14edd-3807-46ed-9184-45a630045f2a","originalAuthorName":"陶鑫"},{"authorName":"张文胜","id":"6533ea53-9732-4cde-919f-c8e575843fa2","originalAuthorName":"张文胜"}],"doi":"10.11792/hj20130406","fpage":"24","id":"dea60eb7-5859-49d2-a6f5-156ba6ee2f21","issue":"4","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"3e60d33d-86b5-45cc-ad3d-8483fc5c4177","keyword":"锆石","originalKeyword":"锆石"},{"id":"d8d5e074-3d5d-4bfa-9072-31fcadeb4687","keyword":"LA-ICPMS","originalKeyword":"LA-ICPMS"},{"id":"471277b8-2604-4d79-af23-616ca652beb3","keyword":"牧牛山岩体","originalKeyword":"牧牛山岩体"},{"id":"2788aebd-77e8-4631-b180-819e7039f4e1","keyword":"郭<span style=\"color:red\">城</span>地区","originalKeyword":"郭城地区"},{"id":"b01e5a64-30e8-4667-889e-cf6dac5843aa","keyword":"胶东","originalKeyword":"胶东"}],"language":"zh","publisherId":"huangj201304006","title":"胶东郭<span style=\"color:red\">城</span>地区牧牛山岩体年代学研究及其地质意义","volume":"34","year":"2013"},{"abstractinfo":"江南造山带新元古变基性岩为区域构造事件和演化模型的建立提供地质依据.对江南造山带东段皖南鹤<span style=\"color:red\">城</span>地区变玄武质岩的地球化学及岩石成因进行研究.鹤<span style=\"color:red\">城</span>变玄武岩呈北东—南西向沿瑶里—鹤<span style=\"color:red\">城</span>—江潭—带分布.元素地球化学的研究表明:休宁鹤<span style=\"color:red\">城</span>变玄武岩同科马提质玄武岩及岛弧玄武岩相类似;富集Rb、Ba、Th、U等强不相容元素,亏损高场强元素Nb和Ta,指示其成因可能与富集地幔的部分熔融有关,同时有地壳物质的混染,其可能属于皖南伏川蛇绿岩西延组成部分,与伏川蛇绿岩组成一个弧后杂岩带,形成于与俯冲有关的弧后小洋盆环境.结合区域资料,表明新元古代板块俯冲、岛弧岩浆活动以及拼合是江南造山带形成的比较合理的构造演化过程.","authors":[{"authorName":"汪龙","id":"57829a41-0fda-4193-942c-a864b24ed26e","originalAuthorName":"汪龙"},{"authorName":"刘春明","id":"380a9376-24d2-4d0b-b7c2-9311c80236ce","originalAuthorName":"刘春明"},{"authorName":"胡召齐","id":"ca4168ff-6b82-41de-be38-cff2600653c9","originalAuthorName":"胡召齐"},{"authorName":"江来利","id":"0e931e11-aafd-4ac5-bdd7-9685ee83dff1","originalAuthorName":"江来利"},{"authorName":"黄德志","id":"f3995eda-666f-40b5-bcd6-32314c8c87c5","originalAuthorName":"黄德志"}],"doi":"","fpage":"863","id":"2cf23d7f-d60b-48d1-8c30-f7e21d77d52e","issue":"4","journal":{"abbrevTitle":"ZGYSJSXB","coverImgSrc":"journal/img/cover/ZGYSJSXB.jpg","id":"88","issnPpub":"1004-0609","publisherId":"ZGYSJSXB","title":"中国有色金属学报"},"keywords":[{"id":"823b3b9d-6c1a-4e0f-a733-7b083be4bd02","keyword":"江南造山带东段","originalKeyword":"江南造山带东段"},{"id":"d0fa7970-3a40-48bf-9da9-f3ffb1d91fb0","keyword":"鹤<span style=\"color:red\">城</span>","originalKeyword":"鹤城"},{"id":"f73efb2e-f301-4bb9-a46f-96b6e46349f9","keyword":"变玄武岩","originalKeyword":"变玄武岩"},{"id":"ebcab0c0-7506-4e82-b70a-4aa1a071eabd","keyword":"科马提质玄武岩","originalKeyword":"科马提质玄武岩"},{"id":"501f2e8a-6d49-4826-9527-2dfdf9351f59","keyword":"岛弧玄武岩","originalKeyword":"岛弧玄武岩"}],"language":"zh","publisherId":"zgysjsxb201604019","title":"皖南鹤<span style=\"color:red\">城</span>科马提质变玄武岩地球化学特征及大地构造意义","volume":"26","year":"2016"}],"totalpage":5,"totalrecord":44}