{"id":"28df3a53-bf07-404b-b346-080abc7a3c0a","title":"伦坡拉盆地古地磁数据","title_en":"Paleomagnetic data from the lunpola basin","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":"伦坡拉盆地古地磁数据","description":"青藏高原中部的伦坡拉盆地位于羌塘地与拉萨地体之间东西向伸展的班公怒江缝合带南缘。由于伦坡拉盆地新生代沉积序列的年龄限制，特别是其上部由于剥蚀或风化作用造成的露头不连续或不暴露，使其具有典型的湖相油页岩沉积，阻碍了对气候变化记录的研究。通过新生代连续湖相地层的古地磁测量，获得其年龄约为21.2～15Ma。岩相、花粉和化石记录表明，伦坡拉盆地在丁青湖组时期应为相对温暖湿润的气候，表明印度季风发生在~26ma之前。","doi":"10.11888/Geo.tpdc.270282","projection":"","language":"zh","share_type":"online","east":89.7,"west":89.6,"south":31.8,"north":31.9,"scale":null,"crs":null,"filesize":0.07,"share_policy":"a","ts_created":"2019-11-03T20:56:45.351123+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-11-05T10:55:30.192353+08:00","time_description":"2100万年至1500万年","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":["f2a78cde-1c98-4241-94dc-7532eba32b80"],"cite":null,"review_status":5,"review_invite":[],"review_editor":{"id":21056,"last_login":"2022-02-09T12:02:24.544987+08:00","username":"huxiaoli","email":"huxiaoli@lzb.ac.cn","is_active":true,"is_staff":true,"user_name":"胡晓利"},"data_sources":null,"temporal_resolution":"1000 year < x","spatial_resolution":"km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[6],"subtopics":{"metadata":"28df3a53-bf07-404b-b346-080abc7a3c0a","three_pole":null,"third_pole":"XDA20070201"},"username":"XDA20070201","review_time":"2019-11-06T01:26:21.718469+08:00","protected_duration":0,"protected_describe":null,"is_important":false,"hit_count":3938}