{"id":"543a721b-dc71-4719-baa5-f017048c83ca","title":"中国东部晚新生代无棣玄武岩数据集","title_en":"Late Cenozoic Wudi basalt data set in eastern China","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":"所有数据以Excel文件存储。文件名称为“WRMT.xlsx”代表全岩主微量数据。文件名称为“WRIso.xlsx”代表全岩同位素地球化学数据。","description":"本数据包含火山岩的全岩主量元素、微量元素和全岩Sr–Nd-Pb同位素数据。样品采集中国东部无棣地区新生代玄武岩。岩石全岩主量地球化学数据是Rigaku-ZSX-100e型X射线荧光光谱仪（XRF）获得的。全岩微量地球化学数据是通过Perkin Elmer ELAN 6000电感耦合等离子体质谱仪（ICP-MS）获得的。岩石全岩Sr–Nd-Pb同位素是通过样品分离提纯-多接收电感耦合等离子体质谱仪分析获得的。通过获得的数据，可以限定区域内岩浆作用的时代、成因和形成背景。获得的数据可以推测地幔中HIMU储层的位置和性质，评估产生高度不均匀地幔的可能机制。","doi":"10.1029/2020GL087260","projection":"","language":"zh","share_type":"online","east":117.4,"west":117.4,"south":38.06,"north":38.06,"scale":null,"crs":null,"filesize":0.04,"share_policy":"a","ts_created":"2021-05-27T00:34:53.513159+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-06-08T11:12:57.022881+08:00","time_description":"33-872万年来","datas_group":3,"time_description_en":"33-8.72 million years","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"平先权","username":"平先权","email":"xqping@cug.edu.cn","is_cancel_expert":true}],"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":"1000 year < x","spatial_resolution":"<= 0.01º","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[],"subtopics":{"metadata":"543a721b-dc71-4719-baa5-f017048c83ca","three_pole":null,"third_pole":null},"username":"王升鹏","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":371}