Upper mantle seismic anisotropy beneath central Northeast China from shear wave splitting analyses

【作者】 宋雨佳； 顾国辉； 盘晓东； 康建红；

【机构】 吉林省地震局； 中国地震局火山研究所；

【摘要】 <正>1 Research background Central Northeast China is located on the eastern edge of the Central Asian Orogenic Belt and surrounded by the Sino-Korean craton to the south and the Pacific Plate to the east, where the Changbaishan volcano (CBV), the largest Cenozoic active intraplate volcano in China, has been highly detected. The internal complex and variable deformation characteristics beneath central NE China and its causes are still under debate.更多还原