Recurrence interval of large earthquake on an active fault zone is an important parameter in assessing seismic hazard. The 2008 Wenchuan earthquake (Mw 7.9) occurred on the central Longmen Shan fault zone and ruptured the Yingxiu-Beichuan fault (YBF) and the Guanxian-Jiangyou fault (GJF). However, there is a considerable discrepancy among recurrence intervals of large earthquake in preseismic a...

The North Qilian Shan, located in the northeastern front of Tibetan Plateau, is an ideal region to study expansion process plateau, which not clearly revealed due lack direct evidence and accurate age control. In Jiudong Basin (foreland basin Shan), a continuous late Cenozoic sedimentary sequence reliable chronostratigraphic framework (post-7 Ma) provide us material this process. study, we firs...

Shan-Chen model is a numerical scheme to simulate multiphase fluid flows using Lattice Boltzmann approach. The original ShanChen model suffers from inability to accurately predict behavior of air bubbles interacting in a non-aqueous fluid. In the present study, we extended the Shan-Chen model to take the effect of the attraction-repulsion barriers among bubbles in to account. The proposed model...

The Paper presents an accounts of wild edible food plants used by shan tribe of Assam. The shan tribe of Assam is Sino-Tibetan race of Mongoloid stock whose ancestors migrated from South -west china. They depend upon forest products for their day to day needs, i.e, food, fodder and shelter etc. Their food include leaves, tubers, bulbs, rhizomes, flowers fruits and seeds of various wild plants s...

Six new species of the genus Junnanotrechus Uéno & Yin, 1993 are described from Yunnan Province, southern China: J. wrasei sp. n. (from the Diancang Shan Mt. R.), J. triporus sp. n. (from the mountains east of Weishan), J. schuelkei sp. n. (from the Ailao Shan Mountain Range), J. elegantulus sp. n. (from the Daxueshan Mount east of Mengsa Town), J. oblongus sp. n. (from the Daxueshan Mount west...

Lathrobium mawenliae sp. n. from the Qinling Shan, Shaanxi, Central China is described and illustrated.

Magnetostratigraphy of sedimentary rock deposited in the Chaka basin (north-easternTibetan Plateau) indicates a lateMiocene onset of basin formation and subsequent development of the adjacent Qinghai Nan Shan. Sedimentation in the basin initiated at 11Ma. In the lower part of the basin ¢ll, a coarsening-upward sequence starting at 9Ma, as well as rapid sedimentation rates, and northward paleocu...

The early Cenozoic topography of the northern Tibetan plateau remains enigmatic because paucity independent paleoelevation constraints. Long-held views northward propagating deformation imply a low Paleogene elevation, but this prediction is speculative. We apply flexural modeling to reconstructed isopach data obtained from Qaidam basin, which requires larger topographic load in Qilian Shan and...

Authors' Oncology a Cancer Ce and Shan Jiaotong U Biotherap Affiliated R Note: Sup Research O

Macropsis validiuscula Dubovsky, 1966, M. vicina (Horvath, 1897) = M. populicola Dubovsky, 1966 = M. albinata Dubovsky, 1966, syn. n. = M. albidula Dubovsky, 1966, syn. n., M. iliensis Mityaev, 1971 and M. elaeagnicola Dubovsky, 1966 are redescribed and illustrated based on material from Tien Shan Mts. (Kyrgyzstan) and Ferghana Valley (Uzbekistan), M. tienschanica Tishetshkin sp. n. from West T...