The Geology of Silali Basin (Kenya) as an Extra-Terrestrial Impact Crater (ETIC)

Loice J Kipkiror, B. K. Rop, E. Ucakuwun
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Abstract

Certain rocks, rock minerals and rock formations have come to be associated with ETICs (Extra-terrestrial Impact Craters). An extra-terrestrial impact crater is a crater that is formed by an extra-terrestrial impact event whereby a heavenly body (a meteor, comet, or asteroid) hits the earth’s surface and creates a crater; before it cools on the earth’s surface as a meteorite or completely gets squashed by the thermodynamics of space transit. The crater created can be dry or filled with water and may be a simple crater or a complex one, also denoted as a basin. The objective of this paper is to describe the geology of the Silali basin as an Extra-Terrestrial Impact Crater (ETIC), highlight the importance of some of its ETIC rocks and explain the formation of the Silali basin resulting from extra-terrestrial impact. Data was collected through field observation, remote sensing, analysis of past geographical and geological studies, interviewing and laboratory analysis. Information has been presented in the form of analyzed satellite images, pictures, tables, and maps. Notably, this is the first study on extra-terrestrial impact cratering (ETIC) in Kenya. Consequently, the Silali basin, as an ETIC, and its environs, is a virgin field for further scientific research.
肯尼亚西拉利盆地作为地外撞击坑的地质特征
某些岩石,岩石矿物和岩层已经与ETICs(地外撞击陨石坑)联系在一起。地外撞击坑是由地外撞击事件形成的陨石坑,由天体(流星、彗星或小行星)撞击地球表面并形成陨石坑;在它像陨石一样在地球表面冷却或被太空运输的热力学完全压扁之前。形成的陨石坑可能是干燥的,也可能充满了水,可能是一个简单的陨石坑,也可能是一个复杂的陨石坑,也被称为盆地。本文的目的是描述希拉里盆地作为一个地外撞击坑(Extra-Terrestrial Impact Crater, ETIC)的地质特征,强调其中一些地外撞击坑岩石的重要性,并解释希拉里盆地是由地外撞击形成的。数据是通过实地观测、遥感、分析过去的地理和地质研究、访谈和实验室分析收集的。信息以分析卫星图像、图片、表格和地图的形式呈现。值得注意的是,这是肯尼亚首次对地外撞击陨石坑(ETIC)进行研究。因此,西拉利盆地及其周边地区是一个有待进一步科学研究的处女地。
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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