Collaborative Research: Dating Deformation with Titanite

合作研究：用钛矿测定形变年代

• 批准号: 1927060
• 负责人: Bradley Hacker
• 金额: $ 28.9万
• 依托单位: University of California-Santa Barbara
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-07-15 至 2022-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1927060&HistoricalAwards=false
• 关键词: Collaborative; Research; Dating; Deformation; Titanite

Much of our understanding of the geologic history of the Earth comes from radiometric dating of Earth processes. Currently, Earth scientists have a difficult time placing narrow constraints on the precise time that a fault occurs deep within the crust of the Earth. This project combines two state-of-the-science techniques to directly date the time of faulting along a key fault zone in southeast Alaska, and thereby date when ancient earthquakes occurred. Development of this new analytical technique will enable considerable future research and understanding of how Earth materials deform. In addition, this research project will provide training and research opportunities for a female graduate student and several undergraduate students. Visits to local elementary schools will enable potential future scientists to experience the methods and results of Earth science research, with direct implications for earthquake hazards. This collaborative project consists of two principal objectives: 1) develop the mineral titanite as a tool for dating high-temperature deformation by a combined microstructural and microgeochronology approach, and 2) apply this tool to the evolution of the spectacular Coast Shear Zone and Great Tonalite Sill in the Coast Mountains orogen of southeast Alaska. Research methods will incorporate a field study to understand qualitatively the evolution of a mid- to deep crustal intra-arc shear zone and synkinematic sheeted-sill complex exposed in the Coast shear zone of Alaska and Canada. Titanite analyses will include electron-backscatter diffraction maps of titanite microstructure, and laser-ablation split-stream inductively coupled plasma maps of titanite composition that incorporate U-Pb dates. These data will allow assessment of the physical and chemical processes that affected the crystal, and the identification of crystals whose U-Pb distribution reflects high-temperature deformation. Because titanite is a widespread crustal mineral, this technique should have broad application globally and enhance our understanding of how crust deforms and orogens assemble and change through time.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

我们对地球地质历史的大部分了解来自于地球过程的辐射测年。目前，地球科学家很难对地壳深处发生断层的精确时间施加狭窄的限制。该项目结合了两种最先进的技术，可以直接确定阿拉斯加东南部关键断裂带沿线的断层活动时间，从而确定古代地震发生的时间。这种新分析技术的发展将使未来对地球材料如何变形的大量研究和理解成为可能。此外，该研究项目还将为一名女研究生和几名本科生提供培训和研究机会。参观当地小学将使未来潜在的科学家能够体验地球科学研究的方法和结果，这对地震灾害有直接影响。该合作项目有两个主要目标：1) 开发钛矿矿物作为通过微观结构和微观地质年代学相结合的方法来测定高温变形的工具，2) 将该工具应用于壮观的海岸剪切带和大英闪长岩的演化位于阿拉斯加东南部海岸山脉造山带的山台。研究方法将结合实地研究，定性地了解阿拉斯加和加拿大海岸剪切带中暴露的中深地壳弧内剪切带和同运动板状基台复合体的演化。钛矿分析将包括钛矿微结构的电子背散射衍射图，以及包含 U-Pb 数据的钛矿成分的激光烧蚀分流感应耦合等离子体图。这些数据将有助于评估影响晶体的物理和化学过程，并识别 U-Pb 分布反映高温变形的晶体。由于钛矿是一种广泛分布的地壳矿物，这项技术应该在全球范围内得到广泛的应用，并增强我们对地壳变形和造山带如何随着时间的推移而聚集和变​​化的理解。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力评估进行评估，被认为值得支持。优点和更广泛的影响审查标准。