{"id":"16fc997c-eed6-4686-b43e-c35d93011bbc","title":"扎西康矿集区找矿靶区（2018-2022）","title_en":"Prospecting targets of Zhaxikang ore distric","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":"文件命名：扎西康矿集区找矿靶区以图片格式储存，文件名称为“扎西康矿集区找矿靶区.jpg”，其中，“扎西康矿集区找矿靶区”为该数据的内容主题。\n\n数据读取方式：该数据集中的文件可用画图、ACDSee或python等程序打开。","description":"在对扎西康矿床精细结构解剖的基础上，通过系统的构造解析、地球物理探测及解译，结合浅表地球化学特征，运用扎西康矿床地质-地球化学-地球物理综合勘查模型和预测指标体系开展矿产预测工作，圈定扎西康54线附近的深部找矿靶区1处。青木竹深部靶区位于错那洞祥林地区北西部。综合地质、地球化学、地球物理等信息，在青木竹地区深部圈定了一处铍-锡-钨多金属找矿靶区。地球化学特征显示，在青木竹一带具有较高的铅、锌、锑、银衬值累加异常，显示该地区具有铅锌等低温元素异常。同时，地质填图工作在青木竹地表发现了数条北东向断裂破碎带，宽度1-5m不等，充填石英、铁锰碳酸盐及金属硫化物，表明青木竹存在着受断裂控制的脉状铅锌锑多金属矿化体，与扎西康铅锌多金属矿具有相似的成矿特征。根据错那洞穹窿伸展带向北西向延伸正好可以到达青木竹深部。","doi":"10.11888/SolidEar.tpdc.272112","projection":"","language":"zh","share_type":"online","east":91.0,"west":89.0,"south":27.0,"north":31.0,"scale":null,"crs":null,"filesize":1.2,"share_policy":"a","ts_created":"2022-03-05T11:53:51.886530+08:00","doi_type":"拥有自主知识产权","ts_updated":"2022-03-06T05:27:49.016602+08:00","time_description":"","datas_group":3,"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":"--","spatial_resolution":"--","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[808],"subtopics":{"metadata":"16fc997c-eed6-4686-b43e-c35d93011bbc","three_pole":null,"third_pole":null},"username":"张林奎","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":40}