Geochemistry and Geochronology of the High-Mg Gabbro Dykes from Quanji Massif: Implications for the

• 作 者: LIAO Fanxi CHEN Nengsong M.Santosh SUN Min WANG Qinyan XU Yixian
• 机 构: International Research Centre for Geology and Resources along the Silk Roads, China University of Ge
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2016年S1期
• 关键词: continental blocks magma subduction depleted southeastern mantle texture margin

The Tarim Craton is one of the major continental blocks in China.Mafic dykes,ultra-mafic–mafic–carbonatite complex and ultra-mafic–mafic pluton of 0.82–0.75 Ga widely occur in Kuluktage,Aksu and Tieklik area along

The Tarim Craton is one of the major continental blocks in China. Mfty dykes, ultra-mafic-mafic-carbonatite complex and ultra-mafic-mafic pluton of 0.82-0.75 Ga widely occur in Kuluktage, Aksu and Tieklik area along