Decoupled anisotropy in the lower crust and upper mantle extracted by the Wave Gradiometry method resolves the differential deformation mechanisms beneath the northeastern Tibetan Plateau
Y. Dai, Chuntao Liang, Feihuang Cao, Ling Chen, Zhen Liu, Xingli Fan, Chaoliang Wang
Topics & Concepts
GeologyCrustSeismologyAnisotropyPlateau (mathematics)GeophysicsDeformation (meteorology)Mantle (geology)Mathematical analysisMathematicsOceanographyPhysicsQuantum mechanicsHigh-pressure geophysics and materialsearthquake and tectonic studiesGeological and Geochemical Analysis