Cambrian ophiolite complexes in the Beishan area, China, southern margin of the Central Asian Orogenic Belt

• Published in: Journal of Asian earth sciences Vol. 153; pp. 193 - 205
• Main Authors: Shi, Yuruo, Zhang, Wei, Kröner, Alfred, Li, Linlin, Jian, Ping
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.03.2018
• Subjects: Beishan; Cambrian; CAOB; China-Mongolian border; Ophiolite; Zircon age; Cambrian; Beishan; Zircon age; China-Mongolian border; Ophiolite; CAOB
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2017.05.021

[Display omitted] •New zircon ages and geochemical data for Cambrian ophiolite in the Beishan area are reported.•The ophiolite complexes were formed within a SSZ setting.•Early Paleozoic southward subduction of the Paleo-Central Asian ocean. We present zircon ages and geochemical data for Cambrian ophiolite complexes exposed in the Beishan area at the southern margin of the Central Asian Orogenic Belt (CAOB). The complexes consist of the Xichangjing-Xiaohuangshan and Hongliuhe-Yushishan ophiolites, which both exhibit complete ophiolite stratigraphy: chert, basalt, sheeted dikes, gabbro, mafic and ultramafic cumulates and serpentinized mantle peridotites. Zircon grains of gabbro samples yielded 206Pb/238U ages of 516±8, 521±4, 528±3 and 535±6Ma that reflect the timing of gabbro emplacement. The geochemical data of the basaltic rocks show enrichment in large-ion lithophile elements and depletion in the high field strength elements relative to normal mid-oceanic ridge basalt (NMORB) in response to aqueous fluids or melts expelled from the subducting slab. The gabbro samples have higher whole-rock initial 87Sr/86Sr ratios and lower positive εNd(t) values than NMORB. These geochemical signatures resulted from processes or conditions that are unique to subduction zones, and the ophiolites are therefore likely to have formed within a supra-subduction zone (SSZ) environment. We suggest that the Cambrian ophiolite complexes in the Beishan area formed within a SSZ setting, reflecting an early Paleozoic subduction of components of the Paleo-Central Asian Ocean and recording an early Paleozoic southward subduction event in the southern CAOB along the northern margin of the Tarim and North China Cratons.