首页> 外文期刊>Gondwana research: international geoscience journal >Provenance and tectonic setting of the Carboniferous sedimentary rocks of the East Junggar Basin, China: Evidence from geochemistry and U-Pb zircon geochronology
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Provenance and tectonic setting of the Carboniferous sedimentary rocks of the East Junggar Basin, China: Evidence from geochemistry and U-Pb zircon geochronology

机译:东准gar尔盆地石炭纪沉积岩的物源和构造背景:来自地球化学和U-Pb锆石年代学的证据

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The modern Junggar Basin was located in the Central Asian Orogenic Belt (CAOB) during the Devonian and Carboniferous. Few data concerning the weathering, provenance and tectonic setting of the Carboniferous sedimentary rocks in the Junggar Basin have been published. The recent discovery of an oil-gas field in the East Junggar Basin provides the impetus for this study. Twenty-eight sediment samples were recovered from eight boreholes, and all were analysed for major and trace element geochemistry. Two samples of sedimentary rocks were selected for zircon U-Pb dating. Low chemical index of alteration (CIA) values (44-71) and relatively high index of compositional variability (ICV) values (0.72-1.83) suggested weak chemical weathering and an immature source for these samples. The relatively low Th/U (2.16-10.55) and Rb/Sr (0.03-5.44) ratios of the drill core samples reflect a simple recycling history. Two samples indicated upper Carboniferous ages (314.6. Ma) and a lower-middle Devonian age (397.9. Ma). Geochemistry and detrital zircon geochronology from the East Junggar Basin reveal a distinct difference in the composition and source rock ages of clastic rocks from the lower and the upper Carboniferous. Major and trace element compositions of the lower Carboniferous sedimentary rocks (LCRs) were derived from typical mafic rocks and an intermediate ocean island arc of early to middle Devonian age, whereas the upper Carboniferous sedimentary rocks (UCRs) were derived from a continental island arc or active continental margin setting with a dominantly felsic to intermediate late Carboniferous age. The current data provide little support for tectonic models that show a passive continental margin of a Precambrian crystalline basement; our study suggests that a volcanic arc accretion or archipelago (early Carboniferous to early-middle Devonian) model for the East Junggar Basin is more viable.
机译:现代的准gar尔盆地在泥盆纪和石炭纪时期位于中亚造山带(CAOB)中。很少有关于准the尔盆地石炭系沉积岩的风化,物源和构造背景的数据。最近在东准gar尔盆地发现的一个油气田为该研究提供了动力。从八个钻孔中采集了28个沉积物样品,并对所有样品进行了主要和微量元素地球化学分析。选择了两个沉积岩样品进行锆石U-Pb测年。低的化学变化指数(CIA)值(44-71)和相对高的组成变异性指数(ICV)值(0.72-1.83)表明这些样品的化学风化较弱且来源不成熟。钻芯样品的Th / U(2.16-10.55)和Rb / Sr(0.03-5.44)比率相对较低,反映了简单的回收历史。两个样品表明石炭纪年龄较高(314.6。Ma),泥盆纪中下部年龄(397.9。Ma)。东准gar尔盆地的地球化学和碎屑锆石地球年代学揭示了石炭纪下部和上部的碎屑岩的成分和烃源岩年龄存在明显差异。下石炭纪沉积岩(LCRs)的主要和微量元素成分来自典型的镁铁质岩石和早至中泥盆世时代的中岛环岛弧,而上石炭纪沉积岩(UCRs)则来自大陆岛弧或活跃的大陆边缘环境,主要为长石质至中石炭纪晚期。目前的数据几乎没有为构造模型提供支持,这些模型显示了前寒武纪晶体基底的被动大陆边缘。我们的研究表明,东准gar尔盆地的火山弧增生或群岛(早石炭纪至中早泥盆世)模型更为可行。

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