Collaborative Research: Theoretical and Experimental Investigation of Grain Damage and the Formation of Plate Boundaries

合作研究：颗粒损伤和板块边界形成的理论和实验研究

基本信息

批准号：
1853184
负责人：
David Bercovici
金额：
$ 27.3万
依托单位：
Yale University
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
2019
资助国家：
美国
起止时间：
2019-06-01 至 2021-06-30
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1853184&HistoricalAwards=false
关键词：
Collaborative Research Theoretical Experimental Investigation

项目摘要

Plate tectonics describes the motion of Earth's upper-most rocky layers and governs almost all geological activity on Earth, such as earthquakes and volcanoes. Plate tectonics is only known to occur on Earth, but not on Venus and Mars, and whether Earth always had plate tectonics in its 4.5 billion-year history is unknown. The emergence of plate tectonics on Earth depends on how rocks in the cold uppermost layers of the mantle - the lithosphere - deform. As rocks deform they can weaken through the process of damage, which concentrates deformation, resulting in more damage, and so on. This positive feedback focuses lithospheric deformation into weak narrow plate boundaries, which are the locus of most seismic and volcanic activity. This project will develop and apply the physics of how mineral grains in rocks are damaged (termed "grain-damage") through combined theoretical and laboratory approaches. When mineral grains are deformed they accumulate defects, which eventually leads to grains breaking down into smaller grains, and this in turn makes the rocks weaker. This process is evident in rocks called mylonites that are often found at plate tectonic boundaries. This project will use grain damage physics to understand how and when plate tectonics arose on early Earth. The project will also study how damage in grains influences cycles of earthquakes at plate boundaries, specifically how rocks weaken, recover and transmit stress to other rocks and eventually trigger more earthquakes. Plate boundary processes have a significant human impact, including evolution of plate boundary fault systems and earthquake recurrence. The project promotes diversity through the support and professional development of two early career female scientists, specifically with interdisciplinary training in theoretical and experimental methods. The project will also involve organization of a symposium on the evolution of plate boundaries for students and young scientists, and will contribute new scientific materials to education and outreach activities at an established scientific visualization facility. This project will advance the study of lithospheric grain-scale physics and deformation mechanisms, and their application to the generation and operation of plate tectonics. The PI's will extend the grain damage theory for lithospheric weakening and plate boundary formation to include mineralogical phase mixing and dislocation dynamics in polymineralic materials, with calibration and testing by rock deformation experiments. These new developments are necessary to address two major scientific questions:1. Emergence of plate tectonics: How did tectonic plate boundaries form in the ancient Archean Earth? Did thermal and petrological evolution in the early Earth, namely cooling, decreasing crustal production, and changes in lithospheric composition, affect localization of deformation in the lithosphere and the emergence of plate tectonics? Specifically, the PI's hypothesize that temperature and melting affect mineral composition, which can then influence rock weakening through the positive feedback of grain damage and mixing between petrological phases.2. Post-seismic creep and lithospheric shear zones: How does transient ductile behavior in the lithosphere, with associated changes in microstructure like grain-size and dislocation density, influence the accumulation, transmission and release of stress following an earthquake? How does this response affect earthquake recurrence cycles and triggering? Does inherited lithospheric weakness, and thus age of a plate boundary, influence post-seismic recovery and earthquake cycles?To address these questions, the investigators will connect new developments in grain-scale physics to plate-scale geodynamic models using experimentally determined rheological laws. These multi-scale models will provide the platform for coupling plate-boundary formation to thermo-chemical evolution of the upper mantle, and to seismogenic behavior in the crust. The ultimate scientific goal of this project is to understand emergence of plate tectonics on early Earth, and how plate boundary evolution and behavior influences post-seismic response and earthquake cycles. These issues span the time scales of the evolution of Earth's surface in deep time, the development of the neotectonic environment, and the behavior of seismically active zones. The proposed work will use theory and experiments to better understand Earth's tectonic processes on the geological and human time scales.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.

板块构造描述了地球最上层岩石层的运动，并控制着地球上几乎所有的地质活动，例如地震和火山。据了解，板块构造只发生在地球上，金星和火星上却没有，而且地球在其 45 亿年的历史中是否一直存在板块构造尚不得而知。地球上板块构造的出现取决于地幔最上层（岩石圈）寒冷的岩石如何变形。当岩石变形时，它们会通过损伤过程而减弱，从而集中变形，导致更多损伤，等等。这种正反馈将岩石圈变形集中到薄弱的狭窄板块边界，这是大多数地震和火山活动的场所。该项目将通过理论和实验室相结合的方法，开发和应用岩石中矿物颗粒如何受损（称为“颗粒损坏”）的物理学。当矿物颗粒变形时，它们会积累缺陷，最终导致颗粒分解成更小的颗粒，这反过来又使岩石变得更脆弱。这一过程在称为糜棱岩的岩石中很明显，这种岩石经常出现在板块构造边界处。该项目将利用颗粒损伤物理学来了解早期地球上板块构造是如何以及何时出现的。该项目还将研究颗粒的损伤如何影响板块边界的地震周期，特别是岩石如何削弱、恢复并将应力传递到其他岩石，并最终引发更多地震。板块边界过程对人类有重大影响，包括板块边界断层系统的演化和地震复发。该项目通过两位早期职业女科学家的支持和专业发展，特别是理论和实验方法的跨学科培训，促进多样性。该项目还将为学生和年轻科学家组织一次关于板块边界演变的研讨会，并将在已建立的科学可视化设施中为教育和推广活动提供新的科学材料。该项目将推进岩石圈颗粒尺度物理和变形机制的研究，及其在板块构造生成和运行中的应用。 PI 将扩展岩石圈弱化和板块边界形成的颗粒损伤理论，以包括多矿物材料中的矿物相混合和位错动力学，并通过岩石变形实验进行校准和测试。这些新进展对于解决两个主要科学问题是必要的：1．板块构造的出现：古代太古代地球中的构造板块边界是如何形成的？早期地球的热学和岩石学演化，即冷却、地壳产量减少以及岩石圈成分的变化，是否影响了岩石圈变形的局部化和板块构造的出现？具体来说，PI的假设是温度和熔化影响矿物成分，然后通过颗粒损伤和岩石相之间的混合的正反馈影响岩石弱化。2．震后蠕变和岩石圈剪切带：岩石圈的瞬态延性行为以及晶粒尺寸和位错密度等微观结构的相关变化如何影响地震后应力的积累、传递和释放？这种反应如何影响地震复发周期和触发？遗传性岩石圈弱点以及板块边界的年龄是否会影响震后恢复和地震周期？为了解决这些问题，研究人员将使用实验确定的流变定律将颗粒尺度物理学的新发展与板块尺度地球动力学模型联系起来。这些多尺度模型将为将板块边界形成与上地幔的热化学演化以及地壳的地震行为耦合提供平台。该项目的最终科学目标是了解早期地球上板块构造的出现，以及板块边界演化和行为如何影响震后响应和地震周期。这些问题涵盖了地球表面深部演化的时间尺度、新构造环境的发展以及地震活动区的行为。拟议的工作将利用理论和实验来更好地了解地质和人类时间尺度上的地球构造过程。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。