With the realization that rocks with a schistosity parallel to bedding(S0 parallel S1)have undergone lengthy histories of deformation that predate the obvious first deformation(e.g.Bell et al.,2003; Sayab,2006;Yeh,200...
Whilst the topographic relief of the Tibetan Plateau’s northeast margin reflects recent Himalayan Orogenesis, its position and geometry reflect much older structures that developed during the Indosinian Orogeny c.200...