{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":3,"startPagecode":1},"records":[{"abstractinfo":"<span style=\"color:red\">黄陵</span><span style=\"color:red\">背斜</span>中南部的月亮包金矿床赋存于三斗坪岩体英云闪长岩(794 Ma)中,矿体主要受北北西向次级断裂构造控制,矿床形成经历了成矿前金初步富集、热液成矿作用、金次生富集3个成矿作用过程.流体包裹体岩相学、热力学及拉曼光谱研究表明:成矿热液总体属中-低温、中-低盐度且含有有机质的H2O-NaCl-CO2 (CH4)体系类型.通过研究并综合分析前人资料初步认为:脆-韧性复合剪切带为其控矿构造;岩浆是成矿物质的主要来源;基性岩墙群侵位引起的加热升温作用配合挤压向伸展转换过程中压力突然释放,是引起成矿流体沸腾和成矿的重要因素;丰富的H2O、CO2、 CH4等挥发组分是该区成矿的有利条件.","authors":[{"authorName":"曹锐","id":"dae2f3f6-89ae-4063-84d6-fc6657df16f9","originalAuthorName":"曹锐"},{"authorName":"李德威","id":"25624ad4-764a-48f4-9f52-410e50fc3db5","originalAuthorName":"李德威"},{"authorName":"易顺华","id":"485f7020-1dd4-4b7a-b550-7850a24b2fbf","originalAuthorName":"易顺华"},{"authorName":"曹圣华","id":"740a3ae6-373f-4379-8f78-7214ea77821e","originalAuthorName":"曹圣华"},{"authorName":"李芳","id":"f3c8d55b-9ee7-4559-a63d-9fcfd388b3a5","originalAuthorName":"李芳"}],"doi":"10.3969/j.issn.1001-1277.2009.02.005","fpage":"14","id":"2c660341-9a5b-4fc7-b386-1f4a7e12b89f","issue":"2","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"a80e70d2-4358-4995-bd3b-28be81f89f3e","keyword":"流体包裹体","originalKeyword":"流体包裹体"},{"id":"53fb907d-7b7c-4010-9a3a-543a2e8810a4","keyword":"作用成矿","originalKeyword":"作用成矿"},{"id":"72e59f22-7d6a-4770-ae90-506469a3f899","keyword":"矿床成因","originalKeyword":"矿床成因"},{"id":"8a30fd2a-9a38-4e0e-9acb-8e9075190cbb","keyword":"<span style=\"color:red\">黄陵</span><span style=\"color:red\">背斜</span>","originalKeyword":"黄陵背斜"},{"id":"2d20b962-f519-4303-99d2-6455abd40733","keyword":"月亮包金矿床","originalKeyword":"月亮包金矿床"}],"language":"zh","publisherId":"huangj200902005","title":"<span style=\"color:red\">黄陵</span><span style=\"color:red\">背斜</span>中南部月亮包金矿床流体成矿作用及矿床成因探讨","volume":"30","year":"2009"},{"abstractinfo":"对<span style=\"color:red\">黄陵</span>弱粘煤的物理和化学性能进行了系统的研究,探讨了高炉喷吹<span style=\"color:red\">黄陵</span>弱粘煤的可行性.结果证实,<span style=\"color:red\">黄陵</span>弱粘煤具有许多优点,完全满足高炉喷吹用煤的基本要求;其着火温度低、爆炸性较强、具有一定的粘结性和可磨件较差等缺点,可以通过无烟煤和贫瘦煤的搭配使用得到解决.视搭配煤种的不同,<span style=\"color:red\">黄陵</span>弱粘煤的配比不宜超过30%～50%.","authors":[{"authorName":"毕学工","id":"0db12bfb-d95f-44b5-a677-c89971ef3903","originalAuthorName":"毕学工"},{"authorName":"杨福","id":"344b3df0-5025-41a5-bbbc-b979f462aeea","originalAuthorName":"杨福"},{"authorName":"梁尚国","id":"30118989-24f9-4d80-8f0a-73589175efa7","originalAuthorName":"梁尚国"},{"authorName":"邹明金","id":"0f1ca451-f7eb-4e8e-9561-726e96e5408b","originalAuthorName":"邹明金"},{"authorName":"郭玉保","id":"3c183bc4-df97-44e4-8c34-4bce613ac4ce","originalAuthorName":"郭玉保"},{"authorName":"马世强","id":"ad5e7c56-bd66-4b30-80ff-8248ac76d147","originalAuthorName":"马世强"}],"doi":"","fpage":"14","id":"720b464f-4ffc-4087-908f-0e26bfab2b85","issue":"6","journal":{"abbrevTitle":"GT","coverImgSrc":"journal/img/cover/GT.jpg","id":"27","issnPpub":"0449-749X","publisherId":"GT","title":"钢铁"},"keywords":[{"id":"a38daf39-9fae-4acc-9160-492c088330d8","keyword":"弱粘煤","originalKeyword":"弱粘煤"},{"id":"125241db-f5a4-4cc6-be22-ef23f40a0cc6","keyword":"高炉","originalKeyword":"高炉"},{"id":"c65f323e-d667-4685-a0cf-b810ed7252e4","keyword":"喷吹","originalKeyword":"喷吹"},{"id":"4de691ea-1cdb-4634-bb5d-5435c168c40f","keyword":"性能","originalKeyword":"性能"},{"id":"fb1b1c25-453e-4cff-b0c1-b64beecd08d9","keyword":"配比","originalKeyword":"配比"}],"language":"zh","publisherId":"gt200906003","title":"高炉喷吹<span style=\"color:red\">黄陵</span>弱粘煤的原煤特性的研究","volume":"44","year":"2009"},{"abstractinfo":"<span style=\"color:red\">黄陵</span>煤矸石的灰成分以SiO2、Al2O3为主,这些组分正是合成分子筛的原料.将煤矸石经过煅烧活化、酸浸除铁、碱熔预处理后,采用水热合成的方法制备4A分子筛.通过正交试验考察了n(Na2O)∶n(SiO2)、n(H2O)∶n(Na2O)、老化时间、晶化温度、晶化时间5个因素对分子筛钙离子交换性能的影响,实验结果表明:n(Na2O)∶n(SiO2)是对4A沸石钙离子交换量影响最大的因素,其次是晶化温度,最小的为老化时间;且在n(Na2O)∶ n(SiO2)为1.3,n(H2O)∶ n(Na2O)为45,老化时间8h,晶化时间4h,晶化温度85℃下制备所得4A分子筛的钙离子交换量达到296.84 mg CaCO3/g干沸石.自制分子筛的XRD及SEM检测分析表明,最优条件下制备出的4A分子筛晶型完整,轮廓清晰,呈立方体,颗粒大小均匀,在1～2 μm左右.","authors":[{"authorName":"吴涛","id":"6d44c7b8-d421-498e-8222-c2145efb3eb1","originalAuthorName":"吴涛"},{"authorName":"杜美利","id":"885ebbb9-d713-4121-88b0-690afef183df","originalAuthorName":"杜美利"},{"authorName":"司玉成","id":"546f699d-1016-48e7-9130-fb9f82f9c293","originalAuthorName":"司玉成"},{"authorName":"李莹","id":"f3435d26-49b9-4605-a3c2-a45b63d2bb13","originalAuthorName":"李莹"}],"doi":"","fpage":"1348","id":"2b1138c3-b5d2-4bd7-963e-61d400f5d3a3","issue":"5","journal":{"abbrevTitle":"GSYTB","coverImgSrc":"journal/img/cover/GSYTB.jpg","id":"36","issnPpub":"1001-1625","publisherId":"GSYTB","title":"硅酸盐通报   "},"keywords":[{"id":"f494666c-700d-4cf7-bb73-b40f9a9de7ac","keyword":"4A分子筛","originalKeyword":"4A分子筛"},{"id":"aa498d19-f801-4047-8751-d66faad1d334","keyword":"煤矸石","originalKeyword":"煤矸石"},{"id":"604735b7-7e05-42e5-a384-355f0d7d7f8c","keyword":"水热合成","originalKeyword":"水热合成"},{"id":"234e42a7-46be-48b2-9f5b-b7fe5bd08c6c","keyword":"Ca2+交换量","originalKeyword":"Ca2+交换量"}],"language":"zh","publisherId":"gsytb201505031","title":"<span style=\"color:red\">黄陵</span>煤矸石制备4A分子筛的研究","volume":"34","year":"2015"},{"abstractinfo":"基于前人大量研究成果及笔者的工作,对湖北秭归月亮包石英脉型金矿床地质特征进行了分析研究,并结合<span style=\"color:red\">黄陵</span><span style=\"color:red\">背斜</span>成矿带地质背景,探讨了月亮包金矿矿床成因.","authors":[{"authorName":"曹锐","id":"e238ec13-40be-429f-a8b1-ca516125d60b","originalAuthorName":"曹锐"},{"authorName":"湛龙","id":"cb5ba36c-9898-4c6c-918d-1b5eb64b8130","originalAuthorName":"湛龙"},{"authorName":"郭金才","id":"95df1803-0b68-4a0c-b878-4ff98292177e","originalAuthorName":"郭金才"},{"authorName":"马振东","id":"2ce7ddc6-4f4a-466a-bc66-af590ffb72f0","originalAuthorName":"马振东"},{"authorName":"侯光久","id":"ecc375b4-3fce-40f4-84e9-74cf0089dd5e","originalAuthorName":"侯光久"}],"doi":"10.3969/j.issn.1001-1277.2007.02.005","fpage":"16","id":"c8cb3fc4-3d9e-4b78-b17a-27522a3bc36b","issue":"2","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"e406f3b0-a3d1-4f68-974e-06cd9de23408","keyword":"石英脉型金矿","originalKeyword":"石英脉型金矿"},{"id":"074794ac-a3e1-47c6-bf4e-69da8d320239","keyword":"矿床地质特征","originalKeyword":"矿床地质特征"},{"id":"1b28ca0c-36d8-4dc3-9577-a26c89764dab","keyword":"月亮包金矿","originalKeyword":"月亮包金矿"},{"id":"913c68fe-3b8f-400e-bdfa-338fe0108418","keyword":"湖北秭归","originalKeyword":"湖北秭归"}],"language":"zh","publisherId":"huangj200702005","title":"湖北秭归月亮包石英脉型金矿床地质特征研究","volume":"28","year":"2007"},{"abstractinfo":"粉煤灰的火山灰反应是其在采空区充填材料中能够发挥作用的主要因素之一,采用酸溶法测定了矸石电厂粉煤灰-Ca(OH) 2-H2O系统中粉煤灰的化学未溶量及反应率,建立了火山灰反应动力学模型,研究了<span style=\"color:red\">黄陵</span>、蒲白、澄合、芙蓉矸石电厂和灞桥燃煤电厂粉煤灰的火山灰反应活性.结果表明,矸石电厂粉煤灰的火山灰反应在常温下均符合一级动力学模型,<span style=\"color:red\">黄陵</span>和芙蓉的矸石电厂粉煤灰的反应速率常数较大,活性较好,蒲白和澄合次之.","authors":[{"authorName":"陈杰","id":"69d9eb1b-9529-478d-8a28-c0ed9bc7ab8f","originalAuthorName":"陈杰"},{"authorName":"高尚勇","id":"661897c7-2103-44c8-a368-8d00780358fd","originalAuthorName":"高尚勇"},{"authorName":"石荧","id":"b7fe4863-cce9-4f05-bee7-66dc665e5626","originalAuthorName":"石荧"},{"authorName":"黄庆享","id":"24dc198f-5654-48dd-ab16-5ae64d70fb78","originalAuthorName":"黄庆享"},{"authorName":"刘永","id":"d2ea1e58-6b39-4d48-936e-c4d97ba961a9","originalAuthorName":"刘永"}],"doi":"","fpage":"908","id":"4f5704f0-4104-4871-80d3-d7fce403b15f","issue":"3","journal":{"abbrevTitle":"GSYTB","coverImgSrc":"journal/img/cover/GSYTB.jpg","id":"36","issnPpub":"1001-1625","publisherId":"GSYTB","title":"硅酸盐通报   "},"keywords":[{"id":"8661e5be-ac58-4548-a363-1508b6459fb7","keyword":"矸石电厂粉煤灰","originalKeyword":"矸石电厂粉煤灰"},{"id":"8357f3c5-a78e-4512-932b-cd8b6cdf6193","keyword":"反应活性","originalKeyword":"反应活性"},{"id":"b6368afc-71bb-47e3-bccf-550c18c45983","keyword":"酸溶法","originalKeyword":"酸溶法"},{"id":"032723db-cc7d-4d30-8e25-6e3e6b3c9a6c","keyword":"火山灰反应动力学","originalKeyword":"火山灰反应动力学"}],"language":"zh","publisherId":"gsytb201603045","title":"矸石电厂粉煤灰的火山灰反应动力学研究","volume":"35","year":"2016"},{"abstractinfo":"贵州瓮福磷矿老虎洞矿区水文地质条件复杂,制约了矿山开采设计和建设.着眼于矿区地形地貌特征,研究地貌发育与地质构造、岩溶作用之间的关系,探讨地貌发育过程和机制.研究表明,矿区位于岩根河谷地北部,地貌类型为<span style=\"color:red\">背斜</span>槽谷,是一种独特的构造岩溶地貌,构造和岩溶作用对矿区槽谷地貌的形成演化具有重要作用,白岩<span style=\"color:red\">背斜</span>为槽谷的形成提供了构造基础,地壳持续隆升是槽谷进一步发展的必要条件,碳酸盐岩地层的岩溶作用对槽谷的发展具有积极促进作用,在经历褶皱成山、剥蚀夷平和侵蚀成谷三个阶段后,矿区<span style=\"color:red\">背斜</span>槽谷地貌发育成型.","authors":[{"authorName":"雷显权","id":"41f88834-665c-4cac-994c-396c89da804c","originalAuthorName":"雷显权"}],"doi":"10.3969/j.issn.2095-1744.2017.01.013","fpage":"60","id":"92d2477f-a203-4ba6-baa1-fb7ee781cde3","issue":"1","journal":{"abbrevTitle":"YSJSGC","coverImgSrc":"journal/img/cover/YSJSGC.jpg","id":"76","issnPpub":"2095-1744","publisherId":"YSJSGC","title":"有色金属工程"},"keywords":[{"id":"9287e350-5b45-49c4-a545-d220b46aeb44","keyword":"老虎洞磷矿","originalKeyword":"老虎洞磷矿"},{"id":"03c2ac97-762a-4601-9a9b-d742816d45d7","keyword":"地貌特征","originalKeyword":"地貌特征"},{"id":"e63bb890-2ed1-4b7b-ab67-d2f4d7459d10","keyword":"<span style=\"color:red\">背斜</span>槽谷","originalKeyword":"背斜槽谷"},{"id":"769ad769-1ce3-4d88-b00a-e43f9087172a","keyword":"构造作用","originalKeyword":"构造作用"},{"id":"1b09eef4-d3cd-40b8-a1e8-0b7b967a26a3","keyword":"岩溶作用","originalKeyword":"岩溶作用"}],"language":"zh","publisherId":"ysjs201701013","title":"贵州老虎洞磷矿区地貌特征及与构造和岩溶作用的关系","volume":"7","year":"2017"},{"abstractinfo":"枣子沟金矿床位于新堡—力士山复<span style=\"color:red\">背斜</span>南翼之合作—岷县区域断裂带上,构造和岩浆热液控矿明显.综合矿床地质特征,从时空、构造、稀土元素等方面对中性岩脉与成矿的关系进行了分析.结果表明,无论在时空分布,还是热动力条件和成矿物质方面,均显示出中性岩脉与成矿具有密切的成因联系.","authors":[{"authorName":"代文军","id":"6aff9254-bde7-43a0-8b30-965fdd844b05","originalAuthorName":"代文军"},{"authorName":"陈耀宇","id":"65e80cd3-2dca-4042-8099-849b65db5c20","originalAuthorName":"陈耀宇"}],"doi":"10.3969/j.issn.1001-1277.2012.01.005","fpage":"19","id":"1a8f404d-aa1d-468b-a3fa-db66eccbb941","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"3b92c0ef-31ef-42ec-84cd-679f82f3edf1","keyword":"中性岩脉","originalKeyword":"中性岩脉"},{"id":"4eef0a06-622f-4631-85a5-52eeeea228b2","keyword":"成矿","originalKeyword":"成矿"},{"id":"706ad389-355e-4c62-82e5-b9055443cd50","keyword":"枣子沟金矿区","originalKeyword":"枣子沟金矿区"},{"id":"52abfd25-b8e9-4ef1-9809-302967a1a79e","keyword":"甘肃","originalKeyword":"甘肃"}],"language":"zh","publisherId":"huangj201201005","title":"甘肃枣子沟金矿区中性岩脉与成矿关系","volume":"33","year":"2012"},{"abstractinfo":"寨上金矿床以F5断裂为界，可分为南、北2个矿带，在地质、地球化学特征方面存在差异。北矿带位于<span style=\"color:red\">背斜</span>北翼下二叠统十里墩组地层中，南矿带产于<span style=\"color:red\">背斜</span>核部中泥盆统安家岔组、上泥盆统大草滩组地层中。流体包裹体研究显示，矿床总体具有中低温、低盐度、低密度、低压力和较浅的成矿深度，南矿带相对于北矿带成矿温度、流体盐度、密度要高，成矿压力以及成矿深度要大。南北矿带可能为一个统一的热液成矿系统，浅部表现为类似于北矿带的微细浸染型金矿化，深部表现为类似于南矿带的脉状富金多金属矿化。","authors":[{"authorName":"喻万强","id":"2a9c0c1d-395e-4833-ab84-ef6fdca8792e","originalAuthorName":"喻万强"},{"authorName":"阎凤增","id":"ad62d408-55d3-4b94-b492-521cf37ab587","originalAuthorName":"阎凤增"},{"authorName":"杨立强","id":"2bd63867-9f18-46fc-a2b8-a87ad67fdc20","originalAuthorName":"杨立强"},{"authorName":"葛良胜","id":"751f7b81-e7d1-4d10-82e4-947bbb69110e","originalAuthorName":"葛良胜"},{"authorName":"张翔","id":"cabee398-66f2-4fee-bfab-950efd1e9ab5","originalAuthorName":"张翔"}],"doi":"10.11792/hj20130603","fpage":"8","id":"0e65a47f-c4fe-4873-b0f4-73bf0bcf9dd5","issue":"6","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"b3991f96-8929-40ac-b338-8c4dff9f5d54","keyword":"寨上金矿床","originalKeyword":"寨上金矿床"},{"id":"ee592e01-cb6f-40d9-b182-c82c9c48ddb3","keyword":"南","originalKeyword":"南"},{"id":"c3663acc-d339-47f0-8036-f6f6a0cfbde2","keyword":"北矿带","originalKeyword":"北矿带"},{"id":"298e0d10-b027-4a7c-ac8d-4a3e18f4f2ed","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"0e180fc5-2f5a-4a56-b7f8-b9d0e3494e1a","keyword":"地球化学","originalKeyword":"地球化学"},{"id":"106355e5-3f3a-4818-b38a-f01dd7d23245","keyword":"流体包裹体","originalKeyword":"流体包裹体"}],"language":"zh","publisherId":"huangj201306004","title":"甘肃寨上大型金矿床南、北矿带地质地球化学特征对比研究","volume":"","year":"2013"},{"abstractinfo":"通过铸体薄片、扫描电镜和压汞分析，以及依据油藏所处的构造形态、储层成因类型、油藏成藏要素等对油藏进行解剖分析，探讨鄂尔多斯盆地吴起地区长2油层组侵蚀残余地层油藏的控制因素。吴起地区长2油层组储层砂体孔隙类型主要为剩余原生粒间孔和次生溶孔，孔隙结构分选中等；发育上倾尖灭型、透镜体型、小幅<span style=\"color:red\">背斜</span>构造型和复合成因型4种油藏类型。鄂尔多斯盆地延长组侵蚀残余地层油藏成藏受古地貌、岩性和构造等多重因素的控制，油藏主要分布于古河道两侧的斜坡带上。地层完整的长2油层组内，小幅<span style=\"color:red\">背斜</span>构造与分流河道砂体叠置，形成规模较大的构造-岩性复合成因油藏，是吴起地区长2油层组主要的油藏类型。","authors":[{"authorName":"杜凌春","id":"098982e4-d0d4-4981-b1a2-c2e2b07b8f11","originalAuthorName":"杜凌春"},{"authorName":"李凤杰","id":"a25a714e-87cd-42ae-ac97-bac1edf349ea","originalAuthorName":"李凤杰"},{"authorName":"屈雪林","id":"5b35a559-ab3e-4787-a597-6fd9125efee3","originalAuthorName":"屈雪林"},{"authorName":"张雁","id":"0b7a1d5d-6f2a-4d30-b432-0f6a8adc3efe","originalAuthorName":"张雁"},{"authorName":"侯景涛","id":"3033f92f-cb9f-4cda-836d-27e6bd0abd3c","originalAuthorName":"侯景涛"},{"authorName":"苏幽雅","id":"def9e91a-ad77-4e65-9f13-a97726733a1a","originalAuthorName":"苏幽雅"}],"doi":"10.3969/j.issn.1671-9727.2015.06.10","fpage":"719","id":"5b5324b9-5709-4800-98ed-8d55492dd831","issue":"10","journal":{"abbrevTitle":"ZGCLJZ","coverImgSrc":"journal/img/cover/中国材料进展.jpg","id":"80","issnPpub":"1674-3962","publisherId":"ZGCLJZ","title":"中国材料进展"},"keywords":[{"id":"57ec7acc-537b-420a-87c2-2a5d775a9423","keyword":"残余地层","originalKeyword":"残余地层"},{"id":"1bd9e871-276a-4d6d-a932-06542b747b4d","keyword":"油藏控制因素","originalKeyword":"油藏控制因素"},{"id":"d72b615c-2628-4469-ba33-1afb784b1218","keyword":"长 2 油层组","originalKeyword":"长 2 油层组"},{"id":"6f01502d-64f5-42bd-bd56-3012d5625812","keyword":"吴起地区","originalKeyword":"吴起地区"},{"id":"7c69f38a-dbfb-4068-a5f6-95265746681a","keyword":"鄂尔多斯盆地","originalKeyword":"鄂尔多斯盆地"}],"language":"zh","publisherId":"zgcljz201510010","title":"吴起地区长2油层组侵蚀残余地层油藏控制因素","volume":"","year":"2015"},{"abstractinfo":"通过系统的路线调查和详细的矿区地质填图,认为寨上金矿区构造格架是由区域性断裂(F1、F10)、主干断裂(F1、F5、轴面断裂、F8、F9)、容矿断裂(矿脉)三者围绕扎麻树<span style=\"color:red\">背斜</span>核部形成一个规模逐渐降低的断裂构造成矿系统.成矿前为左旋压扭性应力场,<span style=\"color:red\">背斜</span>发生二次变形,同时配套形成主干断裂和左行斜列分布的容矿断裂;成矿期为右旋张扭性应力场,形成右行斜列矿体和单个矿体向西侧伏.依据构造控矿特征对矿区和外围下一步的找矿提出了明确的方向.","authors":[{"authorName":"喻万强","id":"faaac981-9eeb-4f2c-bf8e-acd35101b5c1","originalAuthorName":"喻万强"},{"authorName":"刘纲","id":"6542c857-47a3-4d5b-a401-59b7bf37bf77","originalAuthorName":"刘纲"},{"authorName":"王建国","id":"df0a939d-699d-4e89-a906-8412588ffc7c","originalAuthorName":"王建国"},{"authorName":"王晓军","id":"5efbdc4a-e814-4cc9-8d4d-eb2a5cf6cb08","originalAuthorName":"王晓军"},{"authorName":"王治华","id":"c952e38e-4048-4946-8121-030167c4aaa6","originalAuthorName":"王治华"},{"authorName":"牛翠祎\n","id":"a808565d-f2e4-49fd-afc0-7a1914826327","originalAuthorName":"牛翠祎\n"}],"doi":"10.3969/j.issn.1001-1277.2010.09.004","fpage":"15","id":"9193962f-e098-48ba-a757-28d540fceab4","issue":"9","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"2a329a6b-bb06-4913-bd86-0e4cf2d1fb5c","keyword":"寨上金矿床","originalKeyword":"寨上金矿床"},{"id":"3c9c2100-c151-4fda-b713-ab390a87d2ea","keyword":"控矿规律","originalKeyword":"控矿规律"},{"id":"bf4dd3b0-5db8-4103-b362-559316c634fa","keyword":"控矿模式","originalKeyword":"控矿模式"},{"id":"f7f22dcd-a9e9-46b1-91d9-5c73132d4176","keyword":"找矿预测","originalKeyword":"找矿预测"}],"language":"zh","publisherId":"huangj201009004","title":"甘肃岷县寨上金矿床构造控矿特征及找矿预测","volume":"31","year":"2010"}],"totalpage":3,"totalrecord":21}