Discovering Hadean Earth

探索冥古宙地球

• 批准号: 0948724
• 负责人: Timothy Harrison
• 金额: $ 29.9万
• 依托单位: University of California-Los Angeles
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-05-15 至 2015-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0948724&HistoricalAwards=false
• 关键词: Discovering; Hadean; Earth

Intellectual merit. The first 500 million years of Earth history - the Hadean Eon - is a period of 'lost' time as there is virtually no rock record preserved from this interval. However, the PI and colleagues have samples of detrital and xenocrystic zircons from western Australia (Jack Hills) with ages between 4.0 and 4.4 Ga. A massive analysis campaign has identified many thousands of these ancient zircons, and investigations of these grains have been interpreted to suggest the presence of liquid water at the Earth's surface, significant growth of continental crust, a mature sediment recycling system, and perhaps operation of plate boundary-type processes during the Hadean. Such evidence suggests the possibility that the very early planet was much more similar to the present day Earth than previously thought and this stimulates and justifies new measurements. Analytical developments, analysis programs, and experiments are proposed to address the following questions: 1) Could Hadean Jack Hills zircons have been formed by impacts? 2) Do Hadean zircons record the terrestrial counterpart to the ~3.9 Ga lunar cataclysm? 3) What happened to the highly enriched (low Lu/Hf) reservoir seen in 3.9- 4.3 Ga zircons? 4) Do mineral inclusions in 4 Ga zircons retain a pristine Hadean record? 5) Are available barometers applicable to inclusions in Hadean zircons? 6) Do Pu-U variations in Hadean zircons reflect water-mediated fractionation? and 7) Are the collective isotopic, mineralogical, and thermometry data evidence of Hadean continental recycling and plate boundary interactions? Proposed investigations include: 1) Laser ablation ICPMS measurement of initial 176Hf/177Hf in 3.9-3.6 Ga zircons, 2) U-Th-Pb ion microprobe depth profiling of 4 Ga zircons, and 3) characterization of zircons formed in terrestrial impact melts, 4) Hadean Pu-U geochemistry from fission Xe isotopes, 5) Nd isotopic systematics of Jack Hills zircon, 6) NanoSIMS analysis of Si/Al in micron-sized muscovite, 7) K-Ca dating of Hadean muscovite inclusions, and 8) calibration of the Si-in-muscovite barometer forperaluminous granitoids.Broader Impacts. This research will directly benefit the UCLA graduate students supported by this project. Once trained on the ion microprobe, these students in turn provide support to visitors (including numerous graduate students) to the NSF-supported Keck Center for Isotope Geochemistry (see below). Several small projects have been identified that will be used to engender undergraduate research opportunities.Research outcomes are of international interest and could be akin to the results of a planetary exploration mission if the Hadean paradigm is overturned. This project showcases scientific and technical leadership in a field of global interest, aids in capturing the imagination of young people considering a career in science and technology, and provides training opportunities for young scientists. Research results will be communicated to the scientific community via high citation impact scientific journals and to the public through sustained outreach activities (see http://sims.ess.ucla.edu/outreach/outreach.php).

智力上的优点。地球历史的前5亿年--冥古宙--是一段“失落”的时间，因为从这段时间以来几乎没有岩石记录被保存下来。然而，PI和同事们从西澳大利亚（杰克山）获得了年龄在4.0到4.4 Ga之间的碎屑和捕虏晶锆石样本。一项大规模的分析活动已经确定了成千上万的这些古老的锆石，对这些颗粒的研究已经被解释为在地球表面存在液态水，大陆地壳的显着增长，成熟的沉积物循环系统，以及可能在Hadean期间的板块边界型过程的操作。这些证据表明，极早期的行星可能比以前认为的更类似于现在的地球，这激发并证明了新的测量方法。分析的发展，分析程序，并提出了解决以下问题的实验：1）可能Hadean杰克山锆石已形成的影响？2)冥古宙锆石是否记录了地球上与~3.9 Ga月球灾变相对应的东西？3)在3.9- 4.3Ga锆石中发现的高富集（低Lu/Hf）储层发生了什么？4)4Ga锆石中的矿物包裹体是否保留了原始的冥古宙记录？5)现有的气压计是否适用于冥古宙锆石中的包裹体？6)冥古宙锆石的Pu-U变化是否反映了水介导的分馏作用？同位素、矿物学和温度测量数据是否是古冥古代大陆再循环和板块边界相互作用的证据？拟议的调查包括：1）3.9-3.6 Ga锆石中初始176 Hf/177 Hf的激光烧蚀ICPMS测量，2）4 Ga锆石的U-Th-Pb离子微探针深度剖面，以及3）陆地撞击熔体中形成的锆石的表征，4）来自裂变同位素的Hadean Pu-U地球化学，5）Jack Hills锆石的Nd同位素系统学，6）微米级白云母中Si/Al的NanoSIMS分析，7）冥古宙白云母包裹体的K-Ca测年; 8）过铝质花岗岩类白云母中硅气压计的校准。这项研究将直接受益于本项目支持的加州大学洛杉矶分校的研究生。一旦接受离子微探针培训，这些学生反过来为NSF支持的凯克同位素地球化学中心（见下文）的访问者（包括许多研究生）提供支持。已经确定了几个小型项目，将用于创造本科生的研究机会，研究成果具有国际意义，如果推翻冥古宙范式，研究成果可能类似于行星探索使命的结果。该项目展示了在全球感兴趣的领域的科学和技术领导地位，有助于激发考虑从事科学和技术职业的年轻人的想象力，并为年轻科学家提供培训机会。研究成果将通过高引用影响力的科学期刊向科学界传播，并通过持续的外联活动向公众传播（见http：//sims.ess.ucla.edu/outreach/outreach.php）。