{"id":"7d9aa6e3-7be8-48e0-8304-421505f1c5e3","title":"甲玛铜多金属矿床蚀变与构造地质图（2018-2022）","title_en":"Geological structure and polymetallic alteration of deposit (A-2022)","serial":"","user_limit":"为尊重知识产权、保障数据作者的权益、扩展数据中心的服务、评估数据的应用潜力，请数据使用者在使用数据所产生的研究成果中（包括公开发表的论文、论著、数据产品和未公开发表的研究报告、数据产品等成果），明确注明数据来源和数据作者。对于转载（二次或多次发布）的数据，作者还须注明原始数据来源。","instructions":"命名方式：20220207.JPG\n读取方式：JPG阅读器","description":"1）数据内容：甲玛矿区地质、构造和蚀变信息，是基于甲玛矿区露天采坑揭露的典型地质信息，绘制的图件。2）数据来源及加工：地质数据来源野外一线地质填图，具体填图内容涉及构造解译、蚀变分带以及矿物分带，裂隙产状绘制等多种信息，最终良好地揭示甲玛斑岩成矿系统蚀变与矿化的耦合关系。3）数据质量评述：数据经过室内审校，并重新整理。4）数据应用成果及前景：南坑矿段详细揭示滑覆构造体系中多期次褶皱变形对矽卡岩型蚀变和矿化的控制机制。铅山矿段则重点揭示不同岩石地层单位接触界限矽卡岩的空间分布关系以及褶皱变形和岩体侵位的控制机制。","doi":"10.11888/SolidEar.tpdc.272035","projection":"","language":"zh","share_type":"protected","east":91.76,"west":91.75,"south":29.69,"north":29.7,"scale":null,"crs":null,"filesize":22.8,"share_policy":"c","ts_created":"2022-02-08T07:11:43.518636+08:00","doi_type":"拥有自主知识产权","ts_updated":"2022-02-23T15:58:14.282960+08:00","time_description":"","datas_group":0,"time_description_en":"","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"李明慧","username":"李明慧","email":"liminghui@itpcas.ac.cn","is_cancel_expert":false}],"review_editor":{"id":42421,"last_login":"2022-04-08T15:16:51.670544+08:00","username":"任慧霞","email":"510727846@qq.com","is_active":true,"is_staff":true,"user_name":"任慧霞"},"data_sources":null,"temporal_resolution":"Yearly","spatial_resolution":"1km - 10km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[777],"subtopics":{"metadata":"7d9aa6e3-7be8-48e0-8304-421505f1c5e3","three_pole":null,"third_pole":null},"username":"周敖日格勒","review_time":null,"protected_duration":24,"protected_describe":null,"is_important":false,"hit_count":105}