{"currentpage":1,"firstResult":0,"maxresult":10,"pagecode":5,"pageindex":{"endPagecode":5,"startPagecode":1},"records":[{"abstractinfo":"辽宁省<span style=\"color:red\">白云</span><span style=\"color:red\">金矿</span>区遭受了长期的构造-岩浆热事件影响,形成了复杂的构造形迹.其演化大致可划分为早期塑性流变、中期韧性剪切、后期脆性断裂等阶段.<span style=\"color:red\">金矿</span>属岩浆热液型,其直接的控矿构造为脆性断裂.","authors":[{"authorName":"王富春","id":"09038eda-6a55-4ce3-b7d7-937fffd951d1","originalAuthorName":"王富春"}],"doi":"10.3969/j.issn.1001-1277.2002.05.002","fpage":"4","id":"5ed42a2e-f4a7-4b39-95eb-2d304e7948d7","issue":"5","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"36a1f0ce-038b-4a10-a7da-41a176a8b45b","keyword":"塑性流变","originalKeyword":"塑性流变"},{"id":"38f272cf-4fb4-4b35-bed5-c5ee4b301445","keyword":"韧性剪切","originalKeyword":"韧性剪切"},{"id":"bd4a4c10-2aa5-42b4-8554-f65d7938e8d7","keyword":"脆性断裂","originalKeyword":"脆性断裂"},{"id":"048bc99f-23eb-408f-9843-ccff9151970e","keyword":"<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>","originalKeyword":"白云金矿床"},{"id":"2df9bd0e-72eb-4eb6-8e7a-0924c32a7f57","keyword":"辽宁","originalKeyword":"辽宁"}],"language":"zh","publisherId":"huangj200205002","title":"辽宁<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>的控矿构造特征","volume":"23","year":"2002"},{"abstractinfo":"辽宁凤城<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>赋存于下元古界辽河群盖县组与大石桥组接触部的东西向<span style=\"color:red\">白云</span>推覆构造带中,<span style=\"color:red\">矿床</span>类型为含金硅钾蚀变岩型.文章通过对<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>的地质特征、矿石特征等的系统研究,总结了找矿标志,进而指出了找矿方向.","authors":[{"authorName":"郎福全","id":"26762078-ca54-4496-8764-785ed48d5021","originalAuthorName":"郎福全"},{"authorName":"陈贺","id":"21d0dd0a-6b00-40df-9e2a-8c7a0398f192","originalAuthorName":"陈贺"},{"authorName":"刘恒刚","id":"b8b43592-f511-456b-84ae-9d1057a01955","originalAuthorName":"刘恒刚"}],"doi":"10.3969/j.issn.1001-1277.2007.11.004","fpage":"16","id":"55329a6b-e4cd-4229-984c-6abc21e0154c","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"6d989dfa-ed65-4449-a130-bdf0ccb0f033","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"22b219af-4c73-470d-b6f8-4504a5cc80a4","keyword":"找矿方向","originalKeyword":"找矿方向"},{"id":"6deecab9-ddfb-4b6a-bbc5-b13cb9a23d45","keyword":"<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>","originalKeyword":"白云金矿床"}],"language":"zh","publisherId":"huangj200711004","title":"辽宁凤城<span style=\"color:red\">白云</span><span style=\"color:red\">金矿床</span>地质特征及找矿方向","volume":"28","year":"2007"},{"abstractinfo":"在<span style=\"color:red\">金矿床</span>的各类成因理论研究中,<span style=\"color:red\">金矿床</span>中的生物成矿作用是一个研究程度相对较低的领域,也是研究的前沿领域.对<span style=\"color:red\">金矿床</span>中的生物成矿作用领域的研究现状进行综述,对金的生物地球化学性质进行概括,结合微生物学、<span style=\"color:red\">矿床</span>学、地球化学和成矿模拟实验等方面的研究进展,对卡林型<span style=\"color:red\">金矿床</span>、砂<span style=\"color:red\">金矿床</span>及铁帽型<span style=\"color:red\">金矿床</span>中的生物成矿作用进行了探讨,并对世界最大的<span style=\"color:red\">金矿床</span>即兰德<span style=\"color:red\">金矿床</span>中的生物成矿作用进行了实例分析,以提高对<span style=\"color:red\">金矿床</span>中的生物成矿作用的认识.","authors":[{"authorName":"密文天","id":"8bc9c863-ac07-4da6-a942-7390d1993322","originalAuthorName":"密文天"},{"authorName":"李德亮","id":"669106eb-e8fe-468a-9fc2-5b69c6c91393","originalAuthorName":"李德亮"}],"doi":"10.3969/j.issn.1001-1277.2012.07.004","fpage":"16","id":"61382482-28fb-483b-bd8e-627e42ab5127","issue":"7","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"bb036d64-38d4-4095-946e-d697b94af84e","keyword":"<span style=\"color:red\">金矿床</span>","originalKeyword":"金矿床"},{"id":"bb6a2c07-b1dc-432a-832a-1872bc6c0938","keyword":"生物成矿作用","originalKeyword":"生物成矿作用"},{"id":"a81d5e3d-8640-4e95-b83e-011560636080","keyword":"地球化学","originalKeyword":"地球化学"}],"language":"zh","publisherId":"huangj201207004","title":"<span style=\"color:red\">金矿床</span>的生物成矿作用","volume":"33","year":"2012"},{"abstractinfo":"内蒙古商都项家村<span style=\"color:red\">金矿床</span>位于<span style=\"color:red\">白云</span>鄂博裂谷带东段南缘,<span style=\"color:red\">金矿床</span>的赋矿岩层为晚二叠世黑云母钾长花岗岩. 研究后确定2种矿体类型,分别为蚀变岩型和石英脉型. 区内的控矿构造为乌兰哈达—高勿素深大断裂带,该断裂具多期次和继承性的特征,是重要的导矿构造. 次级构造董家村背斜北翼的层间断裂带为矿质赋存提供了空间,是重要的容矿构造. 项家村<span style=\"color:red\">金矿床</span>的发现为裂谷带南缘找矿指明了方向.","authors":[{"authorName":"密文天","id":"00f8723f-ba1a-4ddb-a3d4-274f135c2b06","originalAuthorName":"密文天"},{"authorName":"辛杰","id":"0ee153cc-41d5-4a2e-b3f5-50fa8d387d3b","originalAuthorName":"辛杰"},{"authorName":"席忠","id":"a866846f-f91e-498e-a000-add087f4bfbe","originalAuthorName":"席忠"},{"authorName":"李长才","id":"fcab8fea-6142-4bce-bac9-00a4164b50de","originalAuthorName":"李长才"},{"authorName":"王文祥","id":"b1369f29-20f2-452e-a600-74cf9161cdd3","originalAuthorName":"王文祥"},{"authorName":"武景龙","id":"8238ee31-da50-4960-9072-386ef4801664","originalAuthorName":"武景龙"}],"doi":"10.11792/hj20151103","fpage":"7","id":"32d06bcc-72a2-4cc6-9e2f-2514039a690a","issue":"11","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"aacd4ca3-f4ff-401b-9079-1265b13c4a1b","keyword":"项家村<span style=\"color:red\">金矿床</span>","originalKeyword":"项家村金矿床"},{"id":"fef81169-0d7b-430f-9c44-0eb82cac5e1d","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"82689415-0057-4e8c-84a6-8f3cc41c04e6","keyword":"<span style=\"color:red\">矿床</span>成因","originalKeyword":"矿床成因"},{"id":"da0ce193-85bb-4e13-83c0-f7c057626234","keyword":"商都","originalKeyword":"商都"},{"id":"f22eaa48-e691-46f6-9f2b-512c6b4129dd","keyword":"内蒙古","originalKeyword":"内蒙古"}],"language":"zh","publisherId":"huangj201511003","title":"内蒙古商都项家村<span style=\"color:red\">金矿床</span>地质特征及<span style=\"color:red\">矿床</span>成因","volume":"36","year":"2015"},{"abstractinfo":"水银洞<span style=\"color:red\">金矿床</span>形成是受峨眉地幔热柱活动的巨大影响,文中从峨眉地幔热柱活动、峨眉山玄武岩浆喷发形成赋<span style=\"color:red\">金矿</span>源层、特殊的岩相古地理环境导致赋金建造形成、峨眉地幔热柱构造动力作用形成<span style=\"color:red\">金矿床</span>成矿的主要驱动力、特殊控矿岩石组合、<span style=\"color:red\">白云</span>质在成矿过程中的作用、吸附成矿作用等方面研究了水银洞<span style=\"color:red\">金矿</span>的成矿地质条件,探讨了水银洞<span style=\"color:red\">金矿</span>的形成机理.这为研究水银洞<span style=\"color:red\">金矿床</span>成因及进一步探讨黔西南<span style=\"color:red\">金矿</span>成矿提供了理论依据.","authors":[{"authorName":"聂爱国","id":"bbbf6a58-77c3-4670-ab08-5ff653afe2ff","originalAuthorName":"聂爱国"},{"authorName":"张竹如","id":"2de74147-0df6-4d3b-85c6-3c244c1530f3","originalAuthorName":"张竹如"}],"doi":"10.3969/j.issn.1001-1277.2006.06.002","fpage":"5","id":"8038a420-0e7b-48e0-bfab-9faa62dc594e","issue":"6","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"32733360-c875-4989-9c3c-1e8893333acc","keyword":"成矿地质条件","originalKeyword":"成矿地质条件"},{"id":"b0608305-b486-4a05-8e3d-4c549207425d","keyword":"形成机理","originalKeyword":"形成机理"},{"id":"ee19c525-18e7-4549-94ec-cda0f043f770","keyword":"水银洞<span style=\"color:red\">金矿床</span>","originalKeyword":"水银洞金矿床"},{"id":"6c729ae5-1690-446f-a5d0-8262c79ba15d","keyword":"黔西南","originalKeyword":"黔西南"}],"language":"zh","publisherId":"huangj200606002","title":"黔西南水银洞<span style=\"color:red\">金矿床</span>成矿地质条件研究","volume":"27","year":"2006"},{"abstractinfo":"韧性剪切带型<span style=\"color:red\">金矿床</span>作为重要<span style=\"color:red\">金矿床</span>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<span style=\"color:red\">金矿床</span>和广东河台<span style=\"color:red\">金矿床</span>2个典型韧性剪切带型<span style=\"color:red\">金矿床</span>为例，对韧性剪切带型<span style=\"color:red\">金矿床</span>地质特征进行概括和总结。韧性剪切带型<span style=\"color:red\">金矿床</span>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<span style=\"color:red\">金矿床</span>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<span style=\"color:red\">金矿床</span>","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<span style=\"color:red\">金矿床</span>","originalKeyword":"排山楼金矿床"},{"id":"a6a67657-f9aa-4511-9387-1123023a9940","keyword":"河台<span style=\"color:red\">金矿床</span>","originalKeyword":"河台金矿床"}],"language":"zh","publisherId":"huangj201310006","title":"韧性剪切带型<span style=\"color:red\">金矿床</span>地质特征研究--以辽宁排山楼<span style=\"color:red\">金矿床</span>与广东河台<span style=\"color:red\">金矿床</span>为例","volume":"","year":"2013"},{"abstractinfo":"通过对也门共和国境内<span style=\"color:red\">金矿床</span>的成矿地质背景和<span style=\"color:red\">矿床</span>地质特征的总结,对也门境内可能存在的<span style=\"color:red\">矿床</span>类型及其成矿潜力进行了初步分析.认为也门境内有成矿潜力的主要<span style=\"color:red\">金矿床</span>类型应为与韧性剪切带有关的前寒纪绿岩型<span style=\"color:red\">金矿床</span>、产于沉积岩中的细脉浸染型<span style=\"color:red\">金矿床</span>、产于火山岩中的热泉型<span style=\"color:red\">金矿床</span>、与中酸性岩浆侵入体有关的中温中深脉状<span style=\"color:red\">金矿床</span>以及表生<span style=\"color:red\">金矿床</span>.地质研究程度和勘探程度较低是目前也门<span style=\"color:red\">金矿</span>发现较少的主要原因.","authors":[{"authorName":"阿卜杜·克里木","id":"51a158bd-5c50-40af-a919-7033a56781fc","originalAuthorName":"阿卜杜·克里木"},{"authorName":"李绪俊","id":"e160c169-1eea-4812-b2ed-d76a88634ff6","originalAuthorName":"李绪俊"}],"doi":"10.3969/j.issn.1001-1277.2003.03.004","fpage":"15","id":"e76c0088-6098-4e9e-88c4-ee09ebf7322f","issue":"3","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"82a35ae7-4ce7-40d5-b1fe-22215de27e34","keyword":"也门<span style=\"color:red\">金矿</span>","originalKeyword":"也门金矿"},{"id":"1bbdd8bc-d8c2-4000-9df6-4b2705c0b444","keyword":"成矿潜力","originalKeyword":"成矿潜力"},{"id":"b8cd8de2-d523-442c-bd7d-4256d5f19626","keyword":"勘探程度","originalKeyword":"勘探程度"}],"language":"zh","publisherId":"huangj200303004","title":"也门<span style=\"color:red\">金矿床</span>地质类型及成矿潜力","volume":"24","year":"2003"},{"abstractinfo":"黄埠岭<span style=\"color:red\">金矿床</span>是招莱<span style=\"color:red\">金矿</span>带内典型的脉型<span style=\"color:red\">金矿床</span>之一.研究表明,该<span style=\"color:red\">矿床</span>矿石中金主要是以显微可见的金银系列矿物,呈裂隙金、包裹金和粒间金产于黄铁矿、石英、黄铜矿、方铅矿、闪锌矿、钾长石和硫盐矿物等之中.<span style=\"color:red\">金矿</span>物主要富集在早期<span style=\"color:red\">金矿</span>化的二、三成矿阶段和晚期硫盐矿物富集阶段.这一特征与区域招莱<span style=\"color:red\">金矿</span>带内其他<span style=\"color:red\">金矿床</span>相比较,该<span style=\"color:red\">矿床</span>具有晚期金与硫盐矿物共生富集特征,证明该<span style=\"color:red\">矿床</span>存在两期<span style=\"color:red\">金矿</span>化.","authors":[{"authorName":"张五荣","id":"fa6e81e8-cb02-4c52-84b3-ad1bd9e67ed5","originalAuthorName":"张五荣"},{"authorName":"张渊","id":"1e97c346-a43c-44c6-9b09-50a5fbeb3afa","originalAuthorName":"张渊"},{"authorName":"张佳楠","id":"1736e1f7-2a71-43c3-bd28-afe0f6cba10f","originalAuthorName":"张佳楠"},{"authorName":"张洪喜","id":"bea43e26-b362-4ce8-ad07-19b707daaf09","originalAuthorName":"张洪喜"},{"authorName":"杨开春","id":"f965f30a-7a01-4359-b97b-2f39a695d3d9","originalAuthorName":"杨开春"}],"doi":"10.3969/j.issn.1001-1277.2010.09.006","fpage":"26","id":"941eee2f-63c3-405e-a0d6-f23d479f038e","issue":"9","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"03958e93-7117-4df2-91e1-70a82ad89caf","keyword":"<span style=\"color:red\">金矿</span>物","originalKeyword":"金矿物"},{"id":"1bad80e8-0b5c-4e49-91cd-cd5552f2b5f6","keyword":"载<span style=\"color:red\">金矿</span>物","originalKeyword":"载金矿物"},{"id":"b0c099e5-0267-4f7c-a28f-0a4ec362c91a","keyword":"黄埠岭<span style=\"color:red\">金矿床</span>","originalKeyword":"黄埠岭金矿床"},{"id":"c5b2c7e0-c6e4-4659-a0b8-2bb70740da48","keyword":"山东","originalKeyword":"山东"}],"language":"zh","publisherId":"huangj201009006","title":"山东黄埠岭<span style=\"color:red\">金矿床</span><span style=\"color:red\">金矿</span>物及载<span style=\"color:red\">金矿</span>物特征","volume":"31","year":"2010"},{"abstractinfo":"酒店<span style=\"color:red\">金矿床</span>定位于礼县—<span style=\"color:red\">白云</span>—山阳深断裂西段膨大、分支锐角夹持区,受印支期中川花岗岩体北外接触带中NW向断裂构造控制.通过对<span style=\"color:red\">矿床</span>地质特征的分析,总结了控矿因素,对现有矿体在走向、倾向上的控制程度及<span style=\"color:red\">矿床</span>外围金异常进行了研究,指出了下一步的找矿方向.","authors":[{"authorName":"鲁挑建","id":"84927236-608a-455f-8f76-f6588ba2f6a2","originalAuthorName":"鲁挑建"},{"authorName":"姜启明","id":"2735d065-fa38-4351-8419-5e10bc8c49f2","originalAuthorName":"姜启明"}],"doi":"","fpage":"19","id":"441a9ef0-3392-4891-94c8-9f057e97f589","issue":"9","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"97486d17-526b-4660-8e1a-c6ed124bd596","keyword":"酒店<span style=\"color:red\">金矿床</span>","originalKeyword":"酒店金矿床"},{"id":"af5fb7e4-3c6d-4a0f-8c55-c1d8685f226c","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"43808139-6c02-4dd6-8cdf-a2938ba3ac42","keyword":"控矿因素","originalKeyword":"控矿因素"},{"id":"c1be6145-1274-4b20-b61e-9f8d4630f2e2","keyword":"找矿方向","originalKeyword":"找矿方向"}],"language":"zh","publisherId":"huangj201209005","title":"甘肃酒店<span style=\"color:red\">金矿床</span>地质特征、控矿因素及找矿方向","volume":"33","year":"2012"},{"abstractinfo":"胶东地区存在两种不同地质特征的脉型<span style=\"color:red\">金矿</span>--中深成热液脉型<span style=\"color:red\">金矿</span>与浅成热液脉型<span style=\"color:red\">金矿</span>.本文用<span style=\"color:red\">矿床</span>模型思维,描述北泊<span style=\"color:red\">金矿床</span>的矿脉与矿体地质、矿石特征、矿石地球化学特征、近矿围岩蚀变、<span style=\"color:red\">金矿</span>与脉岩、成矿深度和成矿时代等<span style=\"color:red\">矿床</span>本质特征,说明北泊<span style=\"color:red\">金矿</span>为浅成热液脉型<span style=\"color:red\">金矿床</span>.","authors":[{"authorName":"仇广乐","id":"17a8e200-5fa6-4f22-8b06-0bd07e0b19f3","originalAuthorName":"仇广乐"},{"authorName":"刘连登","id":"a6d4f066-e097-4aaf-9d9a-3948a4e18f23","originalAuthorName":"刘连登"},{"authorName":"陈国华","id":"4a3d9692-9af2-451b-8f82-a696adb2271d","originalAuthorName":"陈国华"},{"authorName":"崔克勇","id":"75ae6ce4-9d6d-44f5-beaf-4d39106e2112","originalAuthorName":"崔克勇"},{"authorName":"迟华松","id":"0566ad43-4066-4113-b470-d8c74fba3333","originalAuthorName":"迟华松"},{"authorName":"张福礼","id":"63c0f2b1-0a9b-41fb-a651-f3ed5372a6b2","originalAuthorName":"张福礼"}],"doi":"10.3969/j.issn.1001-1277.2001.06.002","fpage":"6","id":"1907f4a2-0471-44b1-a2ae-daa81ede361e","issue":"6","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"8b84250a-9ef5-4529-9d0f-5fcd2349aa3a","keyword":"浅成热液脉型<span style=\"color:red\">金矿</span>","originalKeyword":"浅成热液脉型金矿"},{"id":"7f0ccc4a-97d4-4db2-881a-518a9214191c","keyword":"中深成热液脉型<span style=\"color:red\">金矿</span>","originalKeyword":"中深成热液脉型金矿"},{"id":"b7b8616d-c64d-48b6-88e9-c5e2f58add77","keyword":"<span style=\"color:red\">矿床</span>本质特征","originalKeyword":"矿床本质特征"},{"id":"26e2f24b-ecb5-4fae-8544-adb3f613d822","keyword":"胶东","originalKeyword":"胶东"}],"language":"zh","publisherId":"huangj200106002","title":"山东莱西北泊<span style=\"color:red\">金矿床</span>本质特征","volume":"22","year":"2001"}],"totalpage":194,"totalrecord":1938}