祁连山西段甘肃肃北地区北大河岩群片麻状斜长角闪岩的形成时代

    Geochronology of gneissic plagioclase-amphibolite from Beidahe Group-complex in western segment of Qilian Mountains, China.

    • 摘要: 对祁连造山带西段最古老变质岩系之一的北大河岩群的碎屑锆石SHRIMP U-Pb同位素年代学研究表明,其沉积作用发生于1400~863Ma之间,而不是前人所认为的古元古代。通过高精度的LA-ICP-MS(激光剥蚀等离子体质谱仪)锆石微区原位U-Pb同位素测年,在甘肃省肃北蒙古族自治县党河一带北大河岩群片麻状斜长角闪岩中获得(724.4±3.7)Ma的谐和年龄,为原岩(辉长岩)的形成时代,该年龄相当于Rodinia超大陆裂解的地质记录。此外,还获得1949~1184Ma之间的捕获锆石年龄信息。该项研究对确定祁连造山带存在Rodinia超大陆裂解事件具有重要意义,并可进一步限定北大河岩群的形成时代介于1400~724Ma之间。

       

      Abstract: SHRIMP U-Pb dating of detrital zircons from Beidahe Group-complex, one of the oldest metamorphic series in western segment of Qilian orogenic belt, shows the deposition occurred from 1400Ma to 863Ma rather than Paleoproterozoic previously studied. High resolution LA-ICP-MS in situ dating yields the age of 724.4±3.7 Ma from gneissic amphibolite in Beidahe Group-complex located in Dang River, Subei County, Gansu Province, which indicates the protolith age of gabbro. The age equals to the geological record of Rodinia supercontinent break-down event. Furthermore, the ages of 1949~1184 Ma for captured zircons also are yielded in Beidahe Group-complex. The study is of great significance to the existence of Rodinia supercontinent break-down event in the Qilian orogenic belt, and has further restricted the formation age of Beidahe Group-complex between 1400 and 724Ma.

       

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