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The Subsurface Geology Of Rio Tinto: Material Examined During A Simulated Mars Drilling Mission For The Mars Astrobiology Research And Technologyexperiment (marte)

机译:力拓(Rio Tinto)的地下地质:在一次模拟火星钻探任务中检查的材料,用于火星天体生物学研究和技术实验(marte)

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The 2005 Mars Astrobiology Research and Technology Experiment (MARTE) project conducted a simulated 1-month Mars drilling mission in the Rio Tinto district, Spain. Dry robotic drilling, core sampling, and biological and geological analytical technologies were collectively tested for the first time for potential use on Mars. Drilling and subsurface sampling and analytical technologies are being explored for Mars because the subsurface is the most likely place to find life on Mars. The objectives of this work are to describe drilling, sampling, and analytical procedures; present the geological analysis of core and borehole material; and examine lessons learned from the drilling simulation. Drilling occurred at an undisclosed location, causing the science team to rely only on mission data for geological and biological interpretations. Core and borehole imaging was used for micromorphological analysis of rock, targeting rock for biological analysis, and making decisions regarding the next day's drilling operations. Drilling reached 606 cm depth into poorly consolidated gossan that allowed only 35% of core recovery and contributed to borehole wall failure during drilling. Core material containing any indication of biology was sampled and analyzed in more detail for its confirmation. Despite the poorly consolidated nature of the subsurface gossan, dry drilling was able to retrieve useful core material for geological and biological analysis. Lessons learned from this drilling simulation can guide the development of dry drilling and subsurface geological and biological analytical technologies for future Mars drilling missions.
机译:2005年火星天体生物学研究与技术实验(MARTE)项目在西班牙里约热内卢地区进行了为期1个月的模拟火星钻井任务。首次对干式机器人钻探,岩心取样以及生物和地质分析技术进行了集体测试,以用于火星上。正在火星探索钻探,地下采样和分析技术,因为地下是最有可能在火星上找到生命的地方。这项工作的目的是描述钻井,取样和分析程序。介绍岩心和钻孔材料的地质分析;并研究从钻井模拟中学到的经验教训。钻探发生在一个未公开的地点,导致科学团队仅依靠任务数据来进行地质和生物解释。岩心和井眼成像用于岩石的微观形态分析,将岩石用于生物分析,并就第二天的钻井作业做出决策。钻进深度达606厘米的不牢固的筒状山体,仅占岩心的35%,并且在钻进过程中造成了井壁故障。采样包含任何生物学指示的核心材料,并对其进行更详细的分析以进行确认。尽管地下漏斗的固结性很差,但是干钻能够回收有用的岩心材料,用于地质和生物分析。从钻探模拟中学到的经验教训可以指导干式钻探以及地下火星钻探任务的发展。

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