{"id":"d8f9d311-0508-494d-900d-94a2114bec41","title":"临汾裂谷接收函数地震台站和地壳S波速度数据集（2017）","title_en":"Receiver function, seismic station and crustal S-wave velocity in the Linfen rift (2017)","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":"S1_2017308_090019.eqr 接收函数用SAC软件直接读取\nLinfensta.txt 台站分布文件用写字板直接打开","description":"数据包括临汾裂谷及其周边区域23个地震台站的位置信息和台站的远震接收函数波形。通过挑选中国科学院测量与地球物理研究所在2017年11月布设的观测时长为1个月的23个高频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CPS程序的时间域迭代反褶积方法提取接径向收函数。研究结果表明： 临汾裂谷区中下地壳存在不同尺度的低速体，发震层深度由南往北逐渐从~25km增加到~34 km，大致对应着壳内低速体的底界面；重定位地震大都位于高低速体过渡带区域，其中一个的震源深度达到32km，临汾Ｍ7.75级地震位于高速体内，洪洞M8.0级地震位于高速体底部。上传的数据为他人进一步研究临汾裂谷及其邻区结构特征提供了有价值数据和信息。","doi":"10.11888/Disas.tpdc.271330","projection":"","language":"zh","share_type":"online","east":111.94,"west":110.66,"south":35.32,"north":36.81,"scale":null,"crs":null,"filesize":3.0,"share_policy":"a","ts_created":"2021-05-25T12:22:23.366932+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-06-09T08:27:12.312319+08:00","time_description":"2017年11月","datas_group":3,"time_description_en":"November 2017","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":"d8f9d311-0508-494d-900d-94a2114bec41","three_pole":null,"third_pole":null},"username":"危自根","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":455}