• 责任者：Ni Kang (Minxi Geology Team ; Fujian Bureau of Geology and Mineral Resources ; Xiamen 361000 ; China) ; Lei Yongxiao
• 刊名：Northwestern Geology
• 出版年：2013
• 卷期：46(3)
• 关键词：蛇绿岩 ; ophiolite ; 新疆 ; Xinjiang
• 页码：p.64-69
• 图表：2 illus., 1 table, 15 refs.
• 分类号：0801
• issnNo：ISSN1009-6248
• isbnNo：CN61-1149/P

     The Kekesentao ophiolite outcrops in the south of the Erqis suture zone and tectonically mixed in the MidAltai; Kekesentao ophiolite; age; tectonic implicationsDevonian Yundoukala Formation. Main rocks of the ophiolite include serpentinized dunite, olivineAltai; Kekesentao ophiolite; age; tectonic implicationsgabbro and gabbro. In this study, we obtained zircon LAAltai; Kekesentao ophiolite; age; tectonic implicationsICPMS UAltai; Kekesentao ophiolite; age; tectonic implicationsPb age of the gabbros from this ophiolite. Zircons from western and eastern pluton yield concordant age of 332.1 ± 1.5 Ma and 336.5 ± 1.3 Ma respectively, indicating that both of them were coevally emplaced and the ophiolite was formed in early Carboniferous. Combining with the ages obtained in this study and the regional geology, we suggest that the Kekesentao ophiolite was the residue of the oceanic crust between the Kazakstan plate and the AltaiAltai; Kekesentao ophiolite; age; tectonic implieationsMongolia Terrane during their amalgamation at middle to late Carboniferous.