{"title":"江西黎川县十字村石英矿地质特征及矿床成因分析","authors":"怀国 汪","doi":"10.36012/etr.v2i7.2204","DOIUrl":null,"url":null,"abstract":"黎川县十字村石英矿属硅酸盐岩石中的热液充填型脉状石英矿床。成矿构造为南北向断裂构造，成矿热液来自于深部正长花岗岩侵入时形成的热液。论文通过对矿床的地质特征、矿床成因的分析，指出了本地区石英矿的类型、规模、开采特性、找矿方向及标志。","PeriodicalId":57110,"journal":{"name":"工程技术研究","volume":"8 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2020-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"江西黎川县十字村石英矿地质特征及矿床成因分析\",\"authors\":\"怀国 汪\",\"doi\":\"10.36012/etr.v2i7.2204\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"黎川县十字村石英矿属硅酸盐岩石中的热液充填型脉状石英矿床。成矿构造为南北向断裂构造，成矿热液来自于深部正长花岗岩侵入时形成的热液。论文通过对矿床的地质特征、矿床成因的分析，指出了本地区石英矿的类型、规模、开采特性、找矿方向及标志。\",\"PeriodicalId\":57110,\"journal\":{\"name\":\"工程技术研究\",\"volume\":\"8 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2020-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"工程技术研究\",\"FirstCategoryId\":\"1087\",\"ListUrlMain\":\"https://doi.org/10.36012/etr.v2i7.2204\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"工程技术研究","FirstCategoryId":"1087","ListUrlMain":"https://doi.org/10.36012/etr.v2i7.2204","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
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