来自Pilbara和Kaapvaal坑的古老撞击层
Gary R Byerly1, Donald R Lowe, Joseph L Wooden
1Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA 70803-4101, USA. gary@geol.lsu.edu
概括
古代地球的影响在南非和西澳大利亚留下了相同的地质证据. 单个子约会揭示了34.7亿年前的全球事件,这表明巨大的波利德撞击造成了广泛的环境变化.
科学领域:
- 地质科学是地球科学.
- 行星科学 行星科学
- 古生态环境重建的重建
背景情况:
- 巴伯顿绿石带 (南非) 和东部皮尔巴拉区 (西澳大利亚) 保存了地球早期的地质记录.
- 证据表明,大 bolide 撞击发生在 32 亿至 35 亿年前,大大改变了行星环境.
研究的目的:
- 准确地确定巴伯顿绿石带和东部皮尔巴拉区最古老的撞击事件的日期.
- 为了确定这些古代撞击事件是否代表单一,全球同步的事件.
主要方法:
- 单一的-约定被用来分析来自两座石中的与撞击有关的沉积物的.
- 用地质绘图和沉积物学分析来描述撞击沉积物和相关的不一致性.
主要成果:
- 对于南非和西澳大利亚的最古老的撞击事件,获得了3470 +/- 2百万年前相同的单一子-年龄.
- 这些冲击沉积物被解释为一个单一的全球性沉降层,与冲击产生的海有关.
- 在西澳大利亚,这种事件与主要的侵蚀性不合规性有关.
结论:
- 在巴伯顿绿石带和东部皮尔巴拉区最古老的已识别的撞击事件是同时存在的,表明一个单一的全球事件.
- 这种古老的撞击事件显著变形了目标岩石,并改变了早期地球表面的环境,可能引发海和广泛的沉积.
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