Precambrian crustal growth in the Canadian shield: investigating a billion year of tectono-magmatic evolution in the Winnipeg River subprovince, Ontario, Canada

板块构造（即，板块运动和相互作用）发生在整个地球的历史，但驱动力和相关的过程中演变的太古代和元古宙，并导致全球构造，岩浆和环境的变化。最终，这些变化会对碱的性质、丰度和空间分布产生影响（例如，Ni、Cu、Zn）、贵金属（例如，Au）和战略（例如，Li-REE-Nb-Ta金属矿床。前寒武纪时代的每个大陆地壳碎片都代表了一块拼图，然而，将它们整合到一个统一的、全球规模的板块构造演化模型中是具有挑战性的。该研究计划的长期目标是使用多学科方法对加拿大地盾提出全面的地球动力学解释，并将其与南非，澳大利亚，西非和南美洲其他有充分记录的前寒武纪地盾进行测试。加拿大地盾是一个理想的研究区域，其中包括一些最大的太古代地壳碎片（例如，上级省），其边界是广泛的古元古代造山带（例如，Trans-Hudson），并显示了跨越地球历史一半的几乎连续的地壳生长和循环（即，从4.0 Ga到1.8 Ga）。重点研究前寒武纪陆壳的构造、变质、地球化学演化及其对资源前景的意义。在未来五年内，短期目标是解开安大略西北部苏族瞭望台和肯诺拉之间的温尼伯河次省10亿年的太古代地壳历史。温尼伯河次省的年龄、岩石类型、构造样式和变质等级的多样性使其成为解读西部苏必利尔上级省更广泛的地球动力学演化的合适研究区域。这项研究计划将：（1）利用构造、年代学、岩石地球化学和变质制约因素，对温尼伯河亚省的地壳生长和再循环有了新的认识;（2）认识温尼伯河亚省的古-中-新太古代演化之间可能的长期地球动力学变化;（3）提出一个修正的上级省西部构造-地层模型，并检验其对太古代地球动力学过程的意义，这将是实现这项研究计划长期目标的第一步;（4）对上级省的一个片麻岩-花岗岩类“粉红岩”带进行综合和多学科的研究，对战略金属矿点的起源和分布进行综合调查，这可能有助于未来的勘探项目，并最终提高安大略西北部的矿产资源潜力。

Plate tectonics (i.e., plate movement and interaction) occurred throughout all Earth's history, but driving forces and associated processes evolved during the Archean and Proterozoic eons, and resulted in global tectonic, magmatic, and environmental changes. Ultimately, these changes have implications on the nature, abundance and spatial distribution of base (e.g., Ni, Cu, Zn), precious (e.g., Au) and strategic (e.g., Li-REE-Nb-Ta) metal deposits in Precambrian shields. Each continental crust fragment of Precambrian age represents a piece of the puzzle, however their integration in a unified, global-scale, plate tectonics evolutionary model is challenging. The long term objective of this research program is to use multi-disciplinary approaches to propose a comprehensive geodynamic interpretation of the Canadian shield, and test it against other well documented Precambrian cratons in South Africa, Australia, West Africa and South America. The Canadian shield is an ideal study area that includes some of the largest Archean crustal fragments (e.g., Superior Province) that are bounded by extensive Paleoproterozoic orogenic belts (e.g., Trans-Hudson), and displays a nearly continuous crustal growth and recycling spanning half of the Earth's history (i.e., from 4.0 Ga to 1.8 Ga). In this program, the emphasis will be on the structural, metamorphic and geochemical evolution of the Precambrian continental crust, and its implications to prospect for natural resources. In the next five years, the short term objective is to unravel a billion year of Archean crustal history in the Winnipeg River subprovince, between Sioux Lookout and Kenora, north-western Ontario. The variety of ages, rocks types, structural patterns and metamorphic grades in the Winnipeg River subprovince makes it an appropriate study area to decipher the broader geodynamic evolution of the western Superior Province. This research program will: (1) develop a new understanding of crustal growth and recycling in the Winnipeg River subprovince, using structural, geochronological, lithogeochemical, and metamorphic constraints; (2) recognize possible secular geodynamic changes between the Paleo- Meso- and Neoarchean evolution of the Winnipeg River subprovince; (3) propose a revised tectono-stratigraphic model of the western Superior Province, and test its implications for Archean geodynamic processes, which will be a first step toward the long term objective of this research program; (4) deliver a comprehensive and multi-disciplinary study of a gneiss-granitoid "pinkstone" belt in the Superior Province, with integrated investigations on the origin and distribution of strategic metal occurrences, which may assist future exploration projects and ultimately enhance the mineral resources potential of north-western Ontario.