{"id":"4f35a397-bdca-459e-aaa8-c7214d3c0c7c","title":"青藏高原南北缘新近纪岩浆岩的电气石原位硼同位素数据","title_en":"In situ boron isotopic data of tourmaline from Neogene magmatic rocks in the northern and southern margin of the Qinghai Tibet Plateau","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\"data.xlsx\"代表电气石原位硼同位素数据和主量元素数据。","description":"本文数据集包含青藏高原南北缘新近纪岩浆岩的电气石原位硼同位素数据和主量元素数据。电气石主量元素数据是通过电子探针分析获得的，电气石原位硼同位素数据是通过激光剥蚀-多接收电感耦合等离子体质谱仪分析获得的。电气石来自松潘甘孜地块湖东梁上新世的两个云母-流纹岩和喜马拉雅地块错那洞中新世的两个云母花岗岩，他们的δ11B值分别为-10.47±0.54‰。和-12.48±1.04‰。我们认为这些来自西藏南北缘的强过铝质岩浆岩主要是由于俯冲或上覆大陆沉积岩部分熔融而形成的。","doi":"10.1016/j.sesci.2017.03.003","projection":"","language":"zh","share_type":"online","east":92.0,"west":90.0,"south":28.1,"north":36.0,"scale":null,"crs":null,"filesize":0.4,"share_policy":"a","ts_created":"2021-05-24T11:47:46.179560+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-05-24T15:38:13.073164+08:00","time_description":"3-17 Ma","datas_group":3,"time_description_en":"3-17 Ma","data_format":null,"project":[11],"specials":[],"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":"1000 year < x","spatial_resolution":"1km - 10km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[522],"subtopics":{"metadata":"4f35a397-bdca-459e-aaa8-c7214d3c0c7c","three_pole":null,"third_pole":null},"username":"王军","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":451}