Continental reconstruction and metallogeny of the Circum-Junggar areas and termination of the southe

• 作 者: Wenjiao Xiao Min Sun M.Santosh
• 机 构: Xinjiang Research Centre for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese A
• 出 处: Geoscience Frontiers
• 发表日期: 2015年02期
• 关键词: structural evolution Orogenic Belt Central Asia North China

Continental reconstructions in Central Asia are represented by orogenesis along some large orogenic belts in the Altaid collage(Fig.1)or Central Asian Orogenic Belt(CAOB),which separate the East European and Siberian cratons to the north from the Tarim and North China cratons to the south(Sengor et al.,1993;Jahn et al.,2004;Windley et al.,2007;Qu et al.,2008;

Continental reconstructions in Central Asia are represented by orogenesis along some large orogenic belts in the Altaid collage (Fig.1) or Central Asian Orogenic Belt (CAOB), which separate the East European and Siberian cratons to the north from the Tarim and North China cratons to the south (Sengor et al., 1993; Jahn et al., 2004; Windley et al., 2007; Qu et al., 2008;