SHRIM P Dating of PI agiogranite from Bayingou Ophiol ite in the Northern Tianshan M ountains
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Abstract:
The sensitive high—resolution ion microprobe (SHRIM P)U—Pb zircon dating of plagiogranite from the Bayingou ophiolite in the northern Tianshan M ountains indicates that the magmatic age of the plagiogranite is 324.8± 7.1Ma (2o),which shows the Bayingou ophiolite was formed in the early Carboniferous. This suggests the existence of the late Paleozoic“Red Sea type"ocean basin in the northern Tianshan M ountains and the Baiyingou ophiolite is the rem nant of the oceanic crus.
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xu Xueyi, M A Zhongping, XIA Linqi, W ANG Yanbin, LI Xiangmin, XIA Zuchun, W ANG Lishe.2005. SHRIM P Dating of PI agiogranite from Bayingou Ophiol ite in the Northern Tianshan M ountains[J]. Geological Review,51(5):523-527.