{"id":"3b75f54f-c7e8-42fe-b50e-32092039df35","title":"青藏高原东南缘新生代断裂体系构造地貌","title_en":"Tectonic landscape along active faults in the SE Tibetan 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":"文件命名：影像数据以JPG格式存储，文件的名称为“断裂.jpg”，其中断裂代表断裂名称。\n数据读取方式：该数据可以直接用图片浏览器打开。","description":"基于12.5m DEM以及遥感影像解译可以清晰地识别红河断裂、南汀河断裂以及澜沧耿马断裂沿线发育陡坎、错断的河流、闸门脊、挤压脊等构造地貌，为野外进一步核查提供了基本数据。通过对断裂沿线错断地貌的分析以及对第四纪断层露头的精细构造解析，以确定断裂的运动学特征。水系的偏折以及错断的地质、地貌单元指示红河断裂右旋位错量为几十米至~50 km。南汀河断裂沿线发育一系列大型冲沟的左旋位错、断层槽谷、断层三角面，陡坎等构造地貌。澜沧-耿马断裂沿线以右旋走滑为主。","doi":"10.11888/Geo.tpdc.271629","projection":"","language":"zh","share_type":"online","east":105.0,"west":97.0,"south":20.0,"north":25.0,"scale":null,"crs":null,"filesize":7.11,"share_policy":"a","ts_created":"2021-07-17T17:21:51.277807+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-07-20T09:53:28.355481+08:00","time_description":"1500万年","datas_group":3,"time_description_en":"15 million years","data_format":null,"project":[11],"specials":["b6500306-f60b-4aa1-b0b6-0324d94866df"],"cite":null,"review_status":5,"review_invite":[{"user_name":"颜茂都","username":"颜茂都","email":"maoduyan@itpcas.ac.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":"10m - 100m","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21],"subtopics":{"metadata":"3b75f54f-c7e8-42fe-b50e-32092039df35","three_pole":null,"third_pole":null},"username":"张波","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":894}