{"id":"fb623903-2406-470c-8b53-56be4c15f16c","title":"尼泊尔白垩纪以来地层古气候数据","title_en":"Paleoclimatic results of Cretaceous strata in Nepal","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":"尼泊尔白垩纪以来地层古气候数据.xlsx","description":"喜马拉雅山南麓的海-陆相沉积物记录了大陆碰撞最前缘的构造变形和环境演化。为了更好地了解喜马拉雅山南缘的变形机制与环境演化，我们选取了尼泊尔西部晚白垩世至中始新世地层的三个出露良好的天然剖面并进行岩石磁学研究。目前，对120米厚的Palpa剖面的样品开展了磁化率（χlf）、非磁滞剩磁（ARM）与饱和等温剩磁（SIRM）的测量。同时，获得了细颗粒沉积物的等温剩磁（IRM）和磁滞回线，并得出饱和磁化强度（Ms）与饱和剩磁强度（Mrs）等重要磁性参数。","doi":"10.11888/Paleoenv.tpdc.270913","projection":null,"language":"zh","share_type":"protected","east":84.0,"west":83.0,"south":27.0,"north":28.0,"scale":null,"crs":null,"filesize":0.019,"share_policy":"a","ts_created":"2020-09-17T05:28:04.186961+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-04-19T19:11:41.737517+08:00","time_description":"白垩纪","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":["f2a78cde-1c98-4241-94dc-7532eba32b80"],"cite":null,"review_status":5,"review_invite":[{"user_name":"李育","username":"李育","email":"liyu@lzu.edu.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":"100m - 1km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[6],"subtopics":{"metadata":"fb623903-2406-470c-8b53-56be4c15f16c","three_pole":null,"third_pole":"XDA20070201"},"username":"XDA20070201","review_time":null,"protected_duration":24,"protected_describe":null,"is_important":false,"hit_count":1814}