A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …

Shear wave splitting measurements now allow us to examine deformation in the lithosphere
and upper asthenosphere with lateral resolution< 50 km. In an anisotropic medium, one …

提要: 运用地体和地体活动论观点, 提出青藏高原结构划分的新方案; 强调青藏高原的形成经历了
新元古代以来长期活动的过程, 青藏高原是一个“非原地” 诸多地体会聚, 拼合以及经历复合碰撞 …

基于青藏高原东北缘甘肃区域台网41 个宽频带地震台站的远震记录资料, 通过PKS, SKS
和SKKS 震相的剪切波分裂分析, 获取了台站下方介质的各向异性分裂参数 …

岩浆作用与青藏高原演化 Page 1 高校地质学报 Geological Journal of China Universities 2011
年9 月,第17 卷,第3 期,351-367页 September 2011,Vol. 17, No.3, p. 351-367 岩浆作用与青藏 …

Abstract Geochronological (K–Ar or 40Ar/39Ar), major and trace element, Sr–Nd–Pb isotopic
and mineral chemical data are presented for newly discovered Cenozoic volcanic rocks in …

Shear-coupled teleseismic P waves sampling the interior of the Tibetan plateau provide
evidence of systematic variations in crustal structure. The crust thins by up to 20 km from …

Seismic data from central Tibet have been combined to image the subsurface structure and
understand the evolution of the collision of India and Eurasia. The 410-and 660-kilometer …

Shear wave birefringence is a direct diagnostic of seismic anisotropy. It is often used to infer
the northern limit of the underthrusting Indian lithosphere, based on the seismic anisotropy …

Recent research in the Himalayan fold‐thrust belt provides two new sets of observations that
are crucial to understanding the evolution of the Himalayan‐Tibetan orogenic system. First …