Collaborative Research: Understanding lithospheric structure and deformation in Alaska via integration of seismic imaging and geodynamic modeling

合作研究：通过地震成像和地球动力学建模的整合了解阿拉斯加的岩石圈结构和变形

• 批准号: 1829421
• 负责人: Lucy Flesch
• 金额: $ 1.64万
• 依托单位: Purdue University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2018
• 资助国家: 美国
• 起止时间: 2018-08-01 至 2022-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1829421&HistoricalAwards=false
• 关键词: Collaborative; Research; Understanding; lithospheric; structure

In the state of Alaska, the Earth's surface is moving at rates of 10's of millimeters per year with respect to the rest of the North American plate. This motion indicates that the Earth's lithosphere (the more rigid outer layer of the Earth that makes up the tectonic plates) is deforming. In southern Alaska, where the Pacific plate lithosphere is subducting beneath the North American plate, the North American plate is being compressed, for example creating the mountains of the Alaska Range. However, the forces that drive surface motion and North American plate deformation in the interior of Alaska are much less clear. The goal of this project is to measure the structure of the North American plate, in particular its thickness and its internal strength, and to model how forces acting on the edges and base of the plate are transmitted to the surface. The properties of the North American plate and the underlying mantle will be measured using surface and body waves that emanate from distant earthquakes and are recorded at sensors in Alaska, in particular the stations of the NSF Earthscope Transportable Array. The measured North American plate properties will be incorporated in numerical models that will explain motions observed at the surface in Alaska with the forces exerted on the North American plate by other plates and the motion of the deeper mantle. This work will improve understanding of the forces that drive motion and earthquakes on the Denali fault and other faults and that have created the mountains in Alaska. This project will contribute to the education of graduate and undergraduate students at Brown University and Purdue University.Deformation in Alaska manifests dramatic variations, from convergence and uplift in southern Alaska associated with subduction to more enigmatic deformation in interior Alaska that includes southward surface velocities. The drivers of this deformation and their relationship to underlying crust and mantle structure are debated and not yet understood. This project will address these questions by obtaining new models of the seismic structure of North American lithosphere and underlying asthenosphere beneath Alaska (using data from the NSF EarthScope Transportable Array and other networks). These constraints will be incorporated into 3D geodynamic modeling of the driving forces of upper plate deformation that explain observed surface deformation (as constrained by GPS, geologic and seismicity data). To accomplish this the project team will: (1) Carry out individual and joint analyses and inversions of converted body waves (Sp and Ps) and Rayleigh surface waves to obtain detailed models of crust and mantle shear velocity that robustly image mantle discontinuities. Attenuation and azimuthal anisotropy will also be determined; (2) Use shear velocity and attenuation to place bounds on temperature, bulk composition, grain size, water content and partial melt, and use these parameter ranges to place bounds on viscosity and density, incorporating viscosity constraints from dynamic modeling of observed surface motion; (3) Integrate models of viscosity and density with 3D geodynamic modeling of observed surface deformation and test geodynamic models with observations of azimuthal anisotropy in Rayleigh wave phase velocities and SKS splitting. The proposed work will improve understanding of the seismic structure of North American lithosphere and underlying asthenosphere; its implications for crust and mantle rheology and density; and the impact of upper plate and asthenosphere density and rheology on the rates and dynamics of upper plate deformation. A range of key questions will be addressed, including: (1) What processes enable the high rates of deformation and uplift observed in Alaska, and what is the role of upper plate rheology? How coupled are the lithosphere and asthenosphere and what are the impacts of tractions from asthenospheric flow at the base of the upper plate? (2) How has subduction modified the upper plate lithosphere? What are the effects of Yakutat terrane subduction, and does Yakutat mantle have distinct thermal or compositional properties that make it anomalous in terms of viscosity or buoyancy? What is the relationship of Yakutat terrane subduction and the Denali volcanic gap or the Wrangell volcanic field? (3) How do upper plate structure and tectonics relate north of the subduction zone? Where do offsets in upper plate properties occur across terrane boundaries and strike-slip faults? The project will contribute to the education and career development of graduate students at Brown and Purdue. At least one undergraduate will work on this project at Brown through the Leadership Alliance, a program that recruits students from groups underrepresented in STEM fields; one to two Brown undergraduates will also participate. The project will also reach a broader group of students and postdocs at Brown and Purdue through research group meetings and courses, and will be featured in outreach with elementary schools in Providence, RI.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.

在阿拉斯加州，地球表面相对于北美板块的其他部分每年以数十毫米的速度移动。 这种运动表明地球的岩石圈（构成构造板块的地球更坚硬的外层）正在变形。 在阿拉斯加南部，太平洋板块岩石圈正在俯冲到北美板块之下，北美板块正在被压缩，例如形成了阿拉斯加山脉的山脉。 然而，驱动阿拉斯加内部地表运动和北美板块变形的力量却不太清楚。 该项目的目标是测量北美板块的结构，特别是其厚度和内部强度，并模拟作用在板块边缘和底部的力如何传递到表面。 北美板块和底层地幔的特性将使用远距离地震发出的表面波和体波进行测量，并由阿拉斯加的传感器记录，特别是 NSF Earthscope 可移动阵列的站。 测量的北美板块特性将被纳入数值模型中，该模型将解释在阿拉斯加表面观察到的运动以及其他板块对北美板块施加的力以及更深地幔的运动。 这项工作将增进对驱动德纳利断层和其他断层运动和地震以及形成阿拉斯加山脉的力量的理解。 该项目将为布朗大学和普渡大学研究生和本科生的教育做出贡献。阿拉斯加的变形表现出巨大的变化，从阿拉斯加南部与俯冲相关的汇聚和隆起，到阿拉斯加内部更神秘的变形，包括向南的地表速度。 这种变形的驱动因素及其与底层地壳和地幔结构的关系存在争议，但尚未得到理解。该项目将通过获得北美岩石圈和阿拉斯加下方软流圈地震结构的新模型来解决这些问题（使用来自 NSF EarthScope 可移动阵列和其他网络的数据）。 这些约束将被纳入上板块变形驱动力的 3D 地球动力学建模中，以解释观测到的表面变形（受 GPS、地质和地震数据的约束）。 为了实现这一目标，项目团队将：（1）对转换体波（Sp和Ps）和瑞利表面波进行单独和联合分析和反演，以获得地壳和地幔剪切速度的详细模型，从而对地幔不连续性进行稳健成像。衰减和方位各向异性也将被确定； (2) 使用剪切速度和衰减对温度、本体成分、晶粒尺寸、含水量和部分熔化进行限制，并使用这些参数范围对粘度和密度进行限制，并结合观察到的表面运动的动态建模中的粘度约束； (3) 将粘度和密度模型与观测到的表面变形的 3D 地球动力学模型相结合，并通过瑞利波相速度和 SKS 分裂的方位各向异性观测来测试地球动力学模型。拟议的工作将增进对北美岩石圈和底层软流圈地震结构的了解；它对地壳和地幔流变学和密度的影响；以及上板块和软流圈密度和流变性对上板块变形速率和动力学的影响。 将解决一系列关键问题，包括：（1）什么过程导致阿拉斯加观察到的高变形和隆起率，以及上部板块流变学的作用是什么？ 岩石圈和软流圈的耦合程度如何？上板块底部软流圈流的牵引力有何影响？ (2)俯冲作用如何改变了上板块岩石圈？ 雅库塔特地体俯冲会产生什么影响？雅库塔特地幔是否具有独特的热或成分特性，使其在粘度或浮力方面出现异常？雅库塔地体俯冲与德纳利火山间隙或兰格尔火山场有何关系？ (3) 俯冲带以北的上板块结构与构造有何关系？ 跨地体边界和走滑断层上板块属性的偏移发生在哪里？该项目将为布朗大学和普渡大学研究生的教育和职业发展做出贡献。至少一名本科生将通过领导力联盟在布朗大学从事这个项目，该项目旨在从 STEM 领域代表性不足的群体中招募学生；一到两名布朗大学本科生也将参加。该项目还将通过研究小组会议和课程，接触到布朗大学和普渡大学更广泛的学生和博士后群体，并将在罗得岛州普罗维登斯小学的推广活动中进行宣传。该奖项反映了 NSF 的法定使命，并被认为值得支持通过使用基金会的智力优点和更广泛的影响审查标准进行评估。