{"id":"ff082d6f-4fec-4ddf-ace1-50be646b1229","title":"喜马拉雅穹隆带错那洞穹隆电气石花岗岩电子探针分析","title_en":"Electron microprobe analysis of tourmaline granite in cuonadong dome of Himalayan dome belt","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":"文件名称：CuoNaDong EPMA TUR 2019, CuoNaDong为北喜马拉雅穷错那洞地区，EPMA为电子探针分析方法，TUR为分析 电气石， 2019为分析时间,","description":"北喜马拉雅穹隆带错那洞穹隆就位大量含电气石淡色花岗岩，对于电气石淡色花岗岩中电气石主量元素分析，采用对单颗粒核部到边部的主量元素丰度探测，探测方法为电子探针。\n数据来源与加工：电子探针EPMA测试，测试实验室：北京大学 造山带与地壳演化教育部重点实验室 电子探针实验室；探针薄片中电气石矿物元素丰度测试；\n数据质量：元素丰度误差<0.1%.\n数据应用于前景：分析淡色花岗岩源区及其差异，以及探讨流体作用的改造。","doi":"10.11888/Geo.tpdc.271451","projection":"","language":"zh","share_type":"protected","east":92.0,"west":81.1,"south":28.12,"north":30.4,"scale":null,"crs":null,"filesize":2.0,"share_policy":"a","ts_created":"2021-05-31T11:01:39.956632+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-05-31T11:47:31.134157+08:00","time_description":"20 Ma","datas_group":0,"time_description_en":"","data_format":null,"project":[11],"specials":["b6500306-f60b-4aa1-b0b6-0324d94866df"],"cite":null,"review_status":5,"review_invite":[{"user_name":"王浩","username":"王浩_iggcas","email":"wanghao@mail.iggcas.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":"<= 1 m","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21],"subtopics":{"metadata":"ff082d6f-4fec-4ddf-ace1-50be646b1229","three_pole":null,"third_pole":null},"username":"张波","review_time":null,"protected_duration":12,"protected_describe":null,"is_important":false,"hit_count":485}