Dix-Type Multi-Component Scholte Wave Dispersion Inversion without Initial Model  

作　　者：Linjing Zhao Xiangchun Wang Xiaobo Liu 

机构地区：[1]School of Geophysics and Information Technology,China University of Geosciences,Beijing 100083,China [2]Key Laboratory of Intraplate Volcanoes and Earthquakes,Ministry of Education,China University of Geosciences,Beijing 100083,China [3]School of Ocean Sciences,China University of Geosciences,Beijing 100083,China [4]Key Laboratory of Polar Geology and Marine Mineral Resources,Ministry of Education,China University of Geosciences,Beijing 100083,China

出　　处：《Journal of Earth Science》2024年第4期1393-1396,共4页地球科学学刊（英文版）

基　　金：supported by Major Research Project on Scientific Instrument Development,National Natural Science Foundation of China(No.42327901);the research project of the China National Petroleum Corporation(No.2021ZG02);the National Natural Science Foundation of China(Nos.42004091,62127815,42150201);Beijing Natural Science Foundation(No.8222030);sponsored by the Chinese“111”Project(No.B20011).

摘　　要：0 INTRODUCTION Scholte wave dispersion curves contain rich information regarding seafloor media and have therefore attracted increasing attention(Wang et al.,2022;Dong et al.,2021;Du et al.,2020).Ocean bottom seismometer(OBS)data are widely used in the study of seafloor medium information(Wang et al.,2024),and contain rich surface wave information.

关 键 词：SEAFLOOR WAVE INVERSION 

分 类 号：P631.46[天文地球—地质矿产勘探] P736[天文地球—地质学]