岩石圈地球物理探测, 深部结构成像与各向异性等研究是青藏高原大陆动力学研究的基础.
近年来, 随着深部地球物理探测技术和反演成像技术的进步, 信息提取与细节分辨能力不断提升 …

In the Longmenshan thrust belt, the Dayi seismic gap, an area with few earthquakes, is
located between the ruptures of the 2008 Wenchuan Earthquake and the 2013 Lushan …

龙门山断裂带沿倾向和走向具有明显的分带性和分段性特征, 通常以4 条主干断裂为界将龙门山
断裂带自西向东分为5 条构造带, 但是对沿走向的分段性特征仍未达成共识 …

Lithospheric geophysical exploration, structural imaging and anisotropy are the basis for the
study of continental dynamics of the Tibetan Plateau. In recent years, with the advancement …

Three continent‐scale shear zones are arguably the most outstanding structural features in
the southeastern Tibetan Plateau, and therefore, their tectonic and landscape evolution …

Between 2008 and 2013, the M s 8.0 Wenchuan earthquake and the M s 7.0 Lushan
earthquake occurred successively in the Longmenshan fault zone. Their aftershocks …

Several seismic gaps have been identified along the Xianshuihe-Xiaojiang fault zone and
the Longmenshan fault zone in the Sichuan-Yunnan region, including the Daofu-Shimian …

The accuracy of earthquake catalogs limits the reliability of earthquake hazard assessment
and the comprehensive understanding of earthquake mechanisms. Current seismic catalogs …

The Longmenshan fault has obvious structural zonation and segmentation characteristics.
Generally, the Longmenshan fault is divided into five structural zones from west to east with …

Abstract The 2008 Wenchuan Mw 7.9 mainshock caused catastrophic destruction to cities
along the northwestern margin of the Sichuan Basin. This earthquake did not activate the …