{"id":"686d5823-95ce-4f2a-97ab-e9c75f18f084","title":"四川盆地接收函数地震台站和HK结果数据集（2010-2012）","title_en":"Receiver function, seismic stations and HK results data set in the Sichuan Basin (2010-2012)","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":"112ST_11079_055805.eqr  接收函数用SAC软件直接读取\nSichuansta.txt   台站分布文件用写字板直接打开\nSichuanhk.txt    HK文件用写字板直接打开","description":"数据包括四川盆地14个地震台站的位置信息，远震接收函数波形（高斯系数为5.0）和采用多层H-k叠加方法得到的沉积层和基岩层厚度与Vp/Vs比值。通过挑选研究区中国地震局布设的4个固定台站1年和中国科学院地质与地球物理研究所在2010-2012布设的10个流动地震台站记录到的30-90度震中距和大于5.5级远震事件，采用时间域迭代反褶积方法提取接径向收函数。研究结果表明：四川盆地沉积层厚度主要分布在4.2-7.6 km, 波速比普遍超过1.87, 基岩厚度主要分布在33.4-41.8 km，波速比普遍小于1.74。上传的数据为他人进一步研究四川盆地结构特征提供了有价值数据和信息。","doi":"10.11888/Disas.tpdc.271344","projection":"","language":"zh","share_type":"online","east":106.8,"west":105.4,"south":29.4,"north":31.0,"scale":null,"crs":null,"filesize":15.0,"share_policy":"a","ts_created":"2021-05-25T12:55:28.508901+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-05-31T14:49:08.104443+08:00","time_description":"2010年-2012年","datas_group":3,"time_description_en":"2010-2012","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"张衡","username":"张衡","email":"zhangheng415@itpcas.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":"Yearly","spatial_resolution":"1km - 10km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[522],"subtopics":{"metadata":"686d5823-95ce-4f2a-97ab-e9c75f18f084","three_pole":null,"third_pole":null},"username":"危自根","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":532}