The Cleanskin impact structure, Northern Territory and Queensland, Australia: A reconnaissance study

T. Kenkmann, P. Haines, I. Sweet, K. Mitchell
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Abstract

We report on the Cleanskin structure (18°10′00″S, 137°56′30″E), situated at the border between the Northern Territory and Queensland, Australia, and present results of preliminary geological fieldwork, microscopic analyses, and remote sensing. The Cleanskin structure is an eroded complex impact structure of ~15 km apparent diameter with a polygonal outline caused by two preexisting regional fault sets. The structure has a central uplift of ~6 km diameter surrounded by a rather shallow ring syncline. Based on stratigraphy, the uplift in the center may not exceed ~1000 m. The documentation of planar deformation features (PDFs), planar fractures (PFs), and feather features (FFs) in quartz grains from sandstone members of the Mesoproterozoic Constance Sandstone confirms the impact origin of the Cleanskin structure, as proposed earlier. The crater was most likely eroded before the Cambrian and later became buried beneath Cretaceous strata. We infer a late Mesoproterozoic to Neoproterozoic age of the impact event. In this chapter, the Cleanskin structure is compared with other midsized crater structures on Earth. Those with sandstone-dominated targets show structural similarities to the Cleanskin structure.
澳大利亚北领地和昆士兰的Cleanskin撞击构造:一项勘察研究
我们报告了位于澳大利亚北领地和昆士兰州交界处的Cleanskin构造(18°10 ' 00″S, 137°56 ' 30″E),并介绍了初步的地质实地调查、微观分析和遥感结果。Cleanskin构造是一个视直径约15 km的侵蚀复杂冲击构造,其多边形轮廓是由两个预先存在的区域断层集形成的。该构造有一个直径约6公里的中央隆起,周围是一个相当浅的环形向斜。根据地层学,中心的隆升可能不超过~1000 m。中元古代康斯坦斯砂岩砂岩段石英颗粒的平面变形特征(PDFs)、平面断裂特征(pffs)和羽毛特征(FFs)的记录证实了前面提出的Cleanskin构造的撞击成因。这个陨石坑很可能在寒武纪之前就被侵蚀了,后来被埋在白垩纪地层之下。我们推断撞击事件的年龄为中元古代晚期至新元古代。在这一章中,我们将把Cleanskin陨石坑结构与地球上其他中型陨石坑结构进行比较。砂岩占主导的靶区与Cleanskin构造具有相似的构造特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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