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Provenance of the Early Mesoproterozoic Radium Creek Group in the northern Mount Painter Inlier : correlating isotopic signatures to inform tectonic reconstructions

机译:北部画家山内河中元古生界的镭河群的起源:关联同位素特征为构造重建提供依据

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摘要

New in situ zircon LA-ICPMS geochronologic and Hf-isotope data from the Radium Creek Group within the Mount Painter Inlier provide important temporal constraints on the Early Mesoproterozoic palaeogeography of eastern Proterozoic Australia. The entire Radium Creek Group was deposited in a single basin forming phase, and has a maximum depositional age of 1595 ± 3.7 Ma. Detrital zircon from these metasedimentary rocks have U-Pb age populations at ca. 1595 Ma, 1660-1680 Ma, 1710-1780 Ma, ca. 1850 Ma and ca. 2500 Ma. These grains are characterised by isotopically diverse and evolved sources, and have crystallised within predominantly felsic igneous host-rocks. The relative age spectra and isotopic character has more similarity with the Gawler Craton than the Arunta Block, Curnamona Province or the Mount Isa Inlier. These observations suggest that the Mount Painter Province was adjacent to the Gawler Craton in the Early Mesoproterozoic. Our data supports a coherent South Australian Craton at ca. 1595 Ma and a contiguous continental mass that included the North and South Australian cratons. The Mount Painter Inlier occupied a complex plate tectonic setting in the overriding plate of two convergent margins.
机译:来自Mount Painter Inlier内Radium Creek组的新的原位锆石LA-ICPMS地质年代学和Hf同位素数据为澳大利亚东元古代的中元古生代古地理提供了重要的时间约束。整个Radium Creek组沉积在单个盆地形成阶段,最大沉积年龄为1595±3.7 Ma。这些准沉积岩中的碎屑锆石的铀年龄为U-Pb。约1595 Ma,1660-1680 Ma,1710-1780 Ma,约1850年前后2500毫安这些晶粒的特征是同位素来源多样且演化,并在主要为长英质的火成岩中结晶。相对年龄谱和同位素特征与高勒克拉通相比,比库尔纳莫纳省的阿伦塔区块或伊萨山伊里尔山更相似。这些观察结果表明,在中元古代早期,Mount Painter省与Gawler Craton毗邻。我们的数据支持南澳大利亚州克雷顿语的前后一致。 1595 Ma和包括北澳大利亚和南澳大利亚克拉通在内的连续大陆块。 Mount Painter Inlier在两个会聚边缘的上覆板块中占据了复杂的板块构造环境。

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