Postdoctoral Fellowship: EAR-PF: Investigating spatiotemporal variability of forearc mantle wedge serpentinization and rheology during non-steady state subduction

博士后奖学金：EAR-PF：研究非稳态俯冲过程中弧前地幔楔形蛇纹石化和流变学的时空变化

• 批准号: 2305636
• 负责人: Gabe Epstein
• 金额: $ 18万
• 依托单位: Epstein, Gabe S
• 依托单位国家: 美国
• 项目类别: Fellowship Award
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-09-01 至 2025-08-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2305636&HistoricalAwards=false
• 关键词: Postdoctoral; Fellowship; EAR; PF; Investigating

Dr. Gabe Epstein has been awarded an NSF Earth Sciences Postdoctoral Fellowship to carry out research aimed at constraining the causes, variability, and consequences of forearc mantle wedge hydration under the mentorship of Dr. Adam Holt at the University of Miami. At regions where two tectonic plates converge, subduction is the process by which the “subducting” plate thrusts beneath the “overriding” plate and then descends to great depths within the mantle of the Earth; this process occurs along ~50,000 km of coastline around the world including beneath the states of Washington and Alaska, the Island of Japan, and the west coast of South America. Mantle wedge hydration occurs when water is released from the subducting plate into the section of the Earth’s mantle that lies above the subducting plate (the forearc mantle wedge) and can only proceed if this forearc region of the mantle is cool enough for water-bearing minerals to be stable. Release of water from the subducting plate, and the associated wedge hydration, may contribute to the localization and intensity of arc volcanoes (e.g., the “ring of fire” surrounding the Pacific Ocean) and large magnitude earthquakes. Despite this potential importance of mantle wedge hydration, the temporal variability and consequences of this hydration are poorly resolved, often because the dynamic and time-dependent nature of subduction systems is typically neglected in studies that target these processes. This project will merge novel computational methods with laboratory analysis to investigate how fluid release and wedge hydration in forearcs contributes to subduction dynamics (e.g., the speed and shape of subduction zones), and the impacts such dynamics have on volcanism, seismicity, water storage in the mantle, and Earth’s long-term habitability. Utilizing the research findings, Dr. Epstein will develop a series of accessible, open-source, online learning modules aimed at broadening understanding of geoscience problems pertinent to society, welfare, and equity. The design of the modules will allow for participants (the public and high school to undergraduate students) to interact with large datasets and manipulate software code. Broadly, the learning outcomes will be to demonstrate connectivity between geoscience and other branches of research (natural and social sciences, engineering, art), and to highlight the myriad research endeavors of modern geoscientists (laboratory, computational, and field based). The research and broader impact goals will produce new avenues in interdisciplinary science and will contribute to the NSF goal of advancement of national welfare by enhancing both the scientific community’s and the general public’s understanding of natural disasters and the global, long-term water cycle.Dr. Epstein will merge open-sourced software (Python, Perple_X, and ASPECT) with chemical/rheological insights from the exhumed rock record to develop dynamic models of fluid release and concomitant forearc mantle wedge hydration over a range of subduction conditions to better constrain the extents, spatiotemporal variability, and chemical/geodynamic consequences of mantle hydration. The project goals are: (1) determine the relative timing and extents of wedge hydration during a subduction zone’s lifetime, and the associated spatio-temporal variability in mineralogy and viscosity, through geodynamic modeling; (2) perform microstructural observations of natural wedge serpentinites to characterize deformation mechanisms over a range of P-T conditions; and (3) use trace element ratios and stable isotope analysis to determine the relationship between fluid flow and deformation mechanism. These goals are iterative, with insights from (2) and (3) feeding back into the geodynamic model (1). Laboratory chemical (major and trace element, stable N isotope analysis) and crystallographic/rheologic data (in-situ characterization of deformation mechanisms, EBSD, and Raman spectroscopy) will be performed on samples representing mantle wedge serpentinites or close analogs from New Idria (California, USA; blueschist facies), Cemetery Ridge (Arizona, USA; amphibolite facies), and the Western Alps (Italy/France; greenschist through eclogite). It is expected that earliest phase(s) of the thermal evolution of subduction zones is responsible for stabilization of large volumes of hydrous material in the mantle wedge, and that the rheologic behavior of this material varies depending on the extents and distribution of hydration combined with the temperatures and rates of viscous deformation. Dissemination of the research will include development of a series of accessible, experiential, online learning modules hosted as Jupyter Notebooks (via Binder) and geared towards high school and undergraduate students with the aim of demonstrating the interplay among geoscience, chemistry, physics, and coding. The Universal Design for Learning (UDL) educational framework will be utilized to create an accessible and equitable learning environment throughout creation of the modules.This EAR-PF award was co-funded by the EAR Tectonics Program.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.

Gabe Epstein博士已被授予NSF地球科学博士后奖学金，在迈阿密大学Adam Holt博士的指导下开展旨在限制弧前地幔楔水合作用的原因、可变性和后果的研究。在两个构造板块交汇的地区，俯冲是“俯冲”板块冲到“上覆”板块之下，然后下降到地幔深处的过程;这个过程发生在世界各地沿着~ 50，000公里的海岸线，包括华盛顿和阿拉斯加州、日本岛和南美洲西海岸。当水从俯冲板块释放到位于俯冲板块上方的地幔部分（弧前地幔楔）时，地幔楔水合作用发生，并且只有当地幔的弧前区域足够冷以使含水矿物稳定时才能进行。从俯冲板块释放的水，以及相关的楔状水化作用，可能有助于弧火山的定位和强度（例如，太平洋周围的“火环”）和大规模地震。尽管地幔楔水合作用具有潜在的重要性，但这种水合作用的时间变异性和后果并没有得到很好的解决，这通常是因为俯冲系统的动态和时间依赖性在针对这些过程的研究中通常被忽视。该项目将把新的计算方法与实验室分析相结合，以研究前弧中的流体释放和楔状水化如何有助于俯冲动力学（例如，俯冲带的速度和形状），以及这种动力学对火山活动、地震活动、地幔中的水储存和地球的长期可居住性的影响。爱泼斯坦博士将开发一系列可访问的，开源的在线学习模块，旨在扩大对与社会，福利和公平有关的地球科学问题的理解。模块的设计将允许参与者（公众和高中到本科生）与大型数据集进行交互并操作软件代码。从广义上讲，学习成果将展示地球科学与其他研究分支（自然和社会科学，工程，艺术）之间的联系，并突出现代地球科学家（实验室，计算和实地）的无数研究努力。研究和更广泛的影响目标将在跨学科科学中开辟新的途径，并将通过提高科学界和公众对自然灾害和全球长期水循环的理解，为国家福利的发展做出贡献。（Python，Perple_X和ASPECT），从挖掘的岩石记录中获得化学/流变学见解，以开发在一系列俯冲条件下流体释放和伴随的弧前地幔楔水合作用的动态模型，以更好地限制范围，时空变化和地幔水化的化学/地球动力学后果。该项目的目标是：（1）通过地球动力学模拟，确定俯冲带生命周期中楔状体水化作用的相对时间和程度，以及矿物学和粘度的相关时空变化;（2）对天然楔状蛇纹岩进行显微结构观察，以表征P-T条件范围内的变形机制;（3）利用微量元素比值和稳定同位素分析确定流体流动与变形机制的关系。 这些目标是迭代的，从（2）和（3）反馈到地球动力学模型（1）的见解。实验室化学将对代表来自新伊德里亚（美国加州;蓝片岩相）、公墓岭（美国亚利桑那州;角闪岩相）和西阿尔卑斯山（意大利/法国;绿片岩至榴辉岩）的地幔楔蛇纹岩或类似物的样品进行分析（主量和微量元素、稳定氮同位素分析）和晶体学/流变学数据（变形机制的原位表征、EBSD和拉曼光谱）。预计俯冲带热演化的最早阶段是地幔楔中大量含水物质稳定的原因，这种物质的流变行为取决于水化的程度和分布以及粘性变形的温度和速率。该研究的传播将包括开发一系列可访问的，体验式的在线学习模块，这些模块作为笔记本电脑（通过Binder）托管，面向高中和本科生，旨在展示地球科学，化学，物理和编码之间的相互作用。通用学习设计（UDL）教育框架将被用于在整个模块的创建过程中创造一个可访问和公平的学习环境。EAR-PF奖由美国国家科学基金会（NSF）建筑学计划共同资助。该奖项反映了NSF的法定使命，并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，被认为值得支持。