Collaborative Research: Apatite petrochronology and microtextural analyses: a new tool to directly date subduction processes at the base of the seismogenic zone

合作研究：磷灰石岩石年代学和微观结构分析：直接测定地震带底部俯冲过程的新工具

• 批准号: 2217810
• 负责人: Margaret Odlum
• 金额: $ 37.02万
• 依托单位: University of Nevada Las Vegas
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-09-01 至 2023-10-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2217810&HistoricalAwards=false
• 关键词: Collaborative; Research; Apatite; petrochronology; microtextural

Subduction zones are the locus for the most destructive geological hazards on earth including megathrust earthquakes, volcanic eruptions, and tsunami. The portion of the subduction zone where large earthquakes nucleate and slow earthquakes occur, known as the base of the seismogenic zone, is also an area where intense chemical change and fluid flow occurs. Understanding the timing and processes associated with these rocks deformating and interacting with fluids in this part of the subduction zone is critical for further constraining these earthquakes and global element cycling. However, we currently lack robust tools to do so. This project aims to develop apatite petrochronology, the integration of chronologic, chemical, and textural data from single grains of the common mineral apatite, to directly date chemical and mechanical processes that occurred at the base of the subduction seismogenic zone. The proposed research will provide new tools for researchers studying subduction zones as well as deformation and fluid-rock interactions more broadly. The broader impacts of this work center around providing education and research opportunities that increase inclusivity and accessibility in geoscience through the development of virtual field video game modules that integrate field and lab observations and with petrologic, microstructural, and chronological results from this research. These video games will give students opportunities to gain field skills and link outcrop to microscale observations, while being inclusive and accessible to all students (i.e., no barriers associated with cost or able-bodiedness). This research supports two early career female scientists, a female postdoctoral researcher, and will support an undergraduate and graduate student at UNLV. The base of the subduction seismogenic zone, which occurs at depths of 30-50 kms and temperatures ~200-500°C, is where both large megathrust earthquakes nucleate and enigmatic fault zone behaviors such as episodic tremor and slip occur. This is also an area of intense chemical transformation including devolatilization, fluid flow, and metamorphism. Chemical, mechanical, and fluid processes occurring along the plate interface likely play an important role in influencing the deformation style of the base of the subduction seismogenic zone within the relatively cool greenschist and blueschist metamorphic facies (250°C - 500°C). We currently lack well constrained in situ chronometers in these relatively cold metamorphic rocks, making it challenging to place direct timing constraints on these chemical and mechanical processes in exhumed subduction complexes. Apatite, a common accessory mineral in many subduction zone lithologies, dynamically recrystallizes during deformation, dissolves and reprecipitates during fluid flow, and chemically tracks metamorphic and metasomatic reactions making it a potentially transformative tool for recovering linked microstructure-metamorphism-Temperature-time data. This project tests the hypothesis that apatite U-Pb petrochronology can directly date deformation, metamorphism, and(or) fluid flow in rocks exhumed from the base of the subduction seismogenic zone. Through coupled microstructural (petrographic, EBSD), geochemical (EPMA, LA-ICP-MS), and geochronological (LA-ICP-MS) techniques the researchers will directly date these processes in four exhumed subduction complexes (C. Alps, Catalina Schist, & Crete/Andros, Greece) representing different stages of the subduction evolution across a range of P-T-fluid conditions and lithologies. Their results will systematically constrain the physical and chemical behavior of apatite across different P-T and fluid conditions and facilitate method development of EPMA mapping of apatite, yielding transformative tools for recovering linked microstructure-T-t data. Ultimately, this will provide rheologic, geochronologic, and geochemical constraints on from exhumed subduction related rocks that can be integrated with remote observations (e.g., seismology, geodetic data) to better understand complexities of subduction earthquakes, creeping deformation, slow slip events, and chemical transformations during metamorphism, metasomatism, and fluid flow.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.

俯冲带是地球上最具破坏性的地质灾害的发生地，包括特大地震、火山爆发和海啸。俯冲带中发生大地震和慢地震的部分，也称为孕震带的底部。了解俯冲带这部分岩石变形和与流体相互作用的时间和过程对于进一步限制这些地震至关重要。然而，我们目前缺乏强大的工具来实现这一目标，该项目旨在开发磷灰石岩石年代学，整合常见矿物磷灰石单个颗粒的年代学、化学和结构数据，以直接确定化学和机械过程的年代。拟议的研究将为研究俯冲带以及变形和流体-岩石相互作用的研究人员提供新的工具，这项工作的更广泛影响集中在提供增加的教育和研究机会。通过开发虚拟现场视频游戏模块，将现场和实验室观察以及本研究的岩石学、微观结构和年代结果相结合，提高地球科学的包容性和可访问性。这些视频游戏将为学生提供获得现场技能并将露头与微观观测联系起来的机会。 ，同时对所有学生具有包容性和可及性（即没有与成本或能力相关的障碍）。这项研究支持两名早期职业女性科学家、一名女性博士后研究员，并将支持一名本科生和研究生。 UNLV。俯冲地震带的底部发生在深度为 30-50 公里、温度约为 200-500°C 的地方，是大型逆冲地震成核和神秘断层带行为（例如阵发性震颤和滑动）发生的地方。沿着板界面发生的化学、机械和流体过程也可能在影响中发挥重要作用。相对较冷的绿片岩和蓝片岩变质相（250°C - 500°C）内俯冲地震带底部的变形样式，我们目前在这些相对较冷的变质岩中缺乏良好约束的原位计时器，这使得直接放置具有挑战性。磷灰石是许多俯冲带岩性中常见的副矿物，在挖掘出的俯冲复合体中，这些化学和机械过程的时间限制在动态重结晶过程中。该项目测试了磷灰石 U-Pb 岩石年代学可以直接测定变形的假设，该项目测试了磷灰石 U-Pb 岩石年代学可以直接测定变形的假设。通过耦合的微观结构（岩相、研究人员将利用 EBSD）、地球化学（EPMA、LA-ICP-MS）和地质年代学（LA-ICP-MS）技术直接对四个挖出的俯冲复合体（阿尔卑斯山、卡塔利娜片岩和希腊克里特岛/安德罗斯岛）中的这些过程进行年代测定。 ）代表了一系列 P-T 流体条件和岩性的俯冲演化的不同阶段，他们的结果将系统地约束磷灰石在不同 P-T 和流体条件下的物理和化学行为，并促进方法的发展。开发磷灰石 EPMA 测绘，产生用于恢复相关微观结构-T-t 数据的变革性工具，最终，这将为挖掘出的俯冲相关岩石提供流变学、地质年代学和地球化学约束，这些约束可以与远程观测（例如地震学、大地测量数据）相结合。 ）更好地理解俯冲地震、蠕动变形、慢滑移事件以及变质作用、交代作用和流体流动过程中的化学转变的复杂性。该奖项反映了通过使用基金会的智力价值和更广泛的影响审查标准进行评估，NSF 的法定使命被认为值得支持。