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首页> 外文期刊>Journal of geodynamics >LA ICP MS U-Pb ages of detrital zircons from Russia largest rivers: Implications for major granitoid events in Eurasia and global episodes of supercontinent formation
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LA ICP MS U-Pb ages of detrital zircons from Russia largest rivers: Implications for major granitoid events in Eurasia and global episodes of supercontinent formation

机译:来自俄罗斯最大河流的碎屑锆石的LA ICP MS U-Pb年龄:对欧亚大陆主要花岗岩事件和全球超大陆形成的影响

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The paper presents LA ICP MS U-Pb age data on detrital zircons from sands of major Russian rivers: the Don, Volga, Ob', Yenisey and Amur. The obtained data are discussed in terms of major episodes of granitic magmatism, which are recorded in the continental blocks that form the modern Eurasian continent. Results are compared with published igneous and detrital zircon age data obtained from parental and sedimentary rocks of the river basins under consideration and worldwide. The U-Pb age results allowed us to confirm (ⅰ) the episodic character of continent formation; (ⅱ) the Neoarchean global magmatic event and, possibly, formation of the Kenorland supercontinent; (ⅲ) the global episode of crust formation at 2.0-1.8 Ga, which formed the Columbia supercontinent; (ⅳ) the breakup of Columbia at 1.3-1.2 Ga; (ⅴ) the major period of Phanerozoic crustal growth in Central Asia which is likely to be a result of the Altaid orogeny. On the other hand, our data did not unambiguously confirm previous idea about the global character of the Grenvillian and Pan-African orogenies as a result of the assembly of Rodinia and Gondwana, respectively. The "Rodinia" peak is not observed in the histograms of the Ob', Yenisey and Amur, whereas the "Gondwana" signature is not obvious in the histograms of the Don, Volga and Amur. Of special interest are the 2.7-2.5 Ga and 2.0-1.7 Ga peaks in the Ob' zircon age spectrum in spite of the absence of so far identified Archean and Paleoproterozoic parental rocks in the Ob' catchment area. The obtained age spectra were joined into three groups based on statistics: Baltica (Don and Volga), Siberia (Ob' and Yenisey) and East Asia (Amur). For future reconstructions we suggest to include all the available results on Don and Volga rivers into a North America-Baltica Group corresponding to Laurentia-derived continental blocks, and to consider a Siberia Group (Siberian Craton; Ob', Yenisey, Lena, Indigirka rivers) and an East Asia Group (North and South China cratonic blocks; Amur, Yellow, Yangtze and Mekong rivers).
机译:本文介绍了来自俄罗斯主要河道(唐河,伏尔加河,奥伯河,耶尼西河和阿穆尔河)的碎屑锆石的LA ICP MS U-Pb年龄数据。根据花岗岩岩浆作用的主要事件讨论了获得的数据,这些事件记录在形成现代欧亚大陆的大陆块中。将结果与已发布的火成岩和碎屑锆石年龄数据进行了比较,这些数据是从正在研究的流域的母体和沉积岩中获得的,在全球范围内也是如此。 U-Pb年龄结果使我们能够确认(ⅰ)大陆形成的情节特征; (ⅱ)新archarean全球岩浆事件,可能还有Kenorland超大陆的形成; (ⅲ)在2.0-1.8 Ga形成的全球地壳形成事件,形成了哥伦比亚超大陆; (ⅳ)哥伦比亚在1.3-1.2 Ga处破裂; (ⅴ)中亚地区生代地壳生长的主要时期,很可能是阿尔泰造山运动的结果。另一方面,我们的数据并没有明确地确认先前关于罗迪尼亚和冈瓦纳组装的格伦维利和泛非造山带的全球性的先前观点。在Ob',Yenisey和Amur的直方图中未观察到“ Rodinia”峰,而在Don,Volga和Amur的直方图中,“冈瓦纳”信号并不明显。尽管迄今为止还没有确定的奥伯集水区的太古宙和古元古代亲本岩石,但特别令人关注的是奥伯锆石年龄谱中的2.7-2.5 Ga和2.0-1.7 Ga峰。根据统计数据,将获得的年龄谱分为三类:波罗的海(Don和Volga),西伯利亚(Ob'和Yenisey)和东亚(阿穆尔)。对于未来的重建,我们建议将Don和Volga河流上的所有可用结果纳入对应于Laurentia衍生大陆块的北美洲-巴尔蒂卡组,并考虑西伯利亚组(西伯利亚Craton; Ob',Yenisey,Lena,Indigirka河流)和东亚群(中国北部和南部克拉通块;阿穆尔河,黄河,长江和湄公河)。

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