Collaborative Research: Resolving the Nature and Extent Archean Crustal Components in Southwestern Laurentia Using Hf and U-Pb Analysis of Zircon and Baddeleyite

该项目旨在解决北美西南部前寒武纪岩石圈最早演化和深部结构的长期争议。该区域是研究大陆形成过程的全球重要实地实验室。目前的争论集中在需要解决幼年弧增生与较老地壳物质回收和/或与裂谷相关的镁铁质地壳增加的相对重要性。该项目的目标是：1）解决莫哈韦省神秘的太古代和其他前1.8 Ga岩石圈成分的性质，并阐明它们合并成一个组装的1.8-1.6 Ga造山系统的时间和过程; 2）发现更明确的刺穿点（相对于澳大利亚、南极洲等）。可用于超大陆重建的努纳（1.8 Ga）和Rodina（1.0 Ga）;和3）提供了一个全面的基底源区年龄模板，支持广泛的碎屑锆石研究的所有年龄的沉积盆地在西南部。该方法是使用U/Pb放射性测年和Hf同位素特征的锆石从最古老的岩石在西南部。初步研究表明，这些岩石中含有更古老的颗粒，使用这些方法可以破译其历史。该研究团队将分析来自最古老的岩体的继承锆石，这是下地壳熔融的探针，以及来自最古老的变质沉积岩的碎屑锆石，这是侵蚀源区和由此产生的沉积盆地和沉积体系的指示。该项目涉及美国学术界的PI，USGS以及来自学术界和矿业的澳大利亚合作者之间的合作。合并后的数据集将与PI之前几十年的工作以及NSF EarthScope实验中出现的新地球物理图像相结合。这项工作的重要性将是北美大陆这一部分基底结构的结构和演变的新的综合综合，这将有助于地球科学的许多子领域，包括构造学，我们大陆的深时间地质历史，地下地球物理解释的地面实况，以及矿物勘探的应用。该项目还有一个强有力的外联部分，通过培训学生地球科学家，包括少数民族学生，将研究和教育结合起来，并与公园合作，对公众进行非正式的地球科学教育。

This project aims to resolve a long-standing controversy regarding the earliest evolution and deep structure of the Precambrian lithosphere of southwestern North America. This area is a globally important field laboratory for studies of the processes that form continents. Current debate has focused on the need to resolve the relative importance of accretion of juvenile arcs versus recycling of older crustal materials, and/or rift-related addition of mafic crust. The objectives of this project are to: 1) resolve the nature of the cryptic Archean and other pre-1.8 Ga lithospheric components in the Mojave Province and elucidate the timing and processes of their incorporation into an assembling 1.8-1.6 Ga orogenic system; 2) discover more definitive piercing points (relative to Australia, Antarctica, etc.) that can be used for supercontinent reconstructions of Nuna (1.8 Ga) and Rodina (1.0 Ga); and 3) provide a comprehensive basement provenance age template in support of the wide array of detrital zircon studies of sedimentary basins of all ages in the Southwest. The approach is to use U/Pb radiometric dating and Hf isotopic characterization of zircons from the oldest rocks in the Southwest. Pilot studies show that these rocks contain still older grains, whose history will be decipherable using these approaches. The research team will analyze inherited zircons from the oldest plutons, which act as probes what was being melted in the lower crust, and detrital zircons from the oldest metasedimentary rocks, which are an indication of eroding source regions and resulting sedimentary basin and depositional systems.The project involves collaboration between PIs in U.S. academia, the USGS, and Australian collaborators from academia and the mineral industry. The combined datasets will be integrated with several decades of previous work by the PIs and with emerging new geophysical images from the NSF EarthScope experiment. The importance of the work will be a new integrated synthesis of the structure and evolution of the basement architecture of this part of the North American continent that will be useful for many subfields in the geosciences, including tectonics, deep time geologic history of our continent, ground-truth of geophysical interpretations of the subsurface, and applications for minerals exploration. The project also has a strong outreach component that integrates research and education via training of student geoscientists, including minority students, and working with the Parks for informal geoscience education of the public.