NSFGEO-NERC: Global ultralow-velocity zone properties from seismic waveform modeling

该项目旨在通过记录全球发生的地震所产生的地震波形，对地球深处的内部进行成像。我们还没有确切的岩石样本，对地球深处的结构、组成和动态运动进行限制，对于理解从形成到现在积极塑造地球的力量，以及地球深处产生的地表火山活动等危险，都是至关重要的。本研究的重点是结合数据分析和地震波形预测的一种新的建模方法的技术开发，该方法将应用于核幔边界的成像特征，称为超低速度带（ULVZs）。这些ulvz的存在是有据可证的，过去的一些研究已经将它们与重要的全球地球过程联系起来，比如熔融，地核铁流入地幔，或者早期熔融地球的残余。然而，ulvz在物理上代表什么仍然是一个问题。这项研究的目的是根据它们的组成、位置以及与地球内部过去和现在的过程的关系来确定ulvz是什么。这项工作将为了解地球是如何形成的、目前地球内部正在进行的动态运动是什么，以及这些运动与夏威夷和黄石公园等地表热点火山活动的关系提供关键的限制。该项目旨在开发一种新的地震波形建模方法，该方法将允许对我们从世界各地的地震中常规记录的复杂地震波形的起源以及这些地震波对地球内部小尺度特征的敏感程度有新的认识。在这个项目中开发的方法和软件将被公开分享，并将适用于广泛的研究人员，他们可能希望将这些技术应用于不同的目标领域。此外，这项研究还使大量研究确定地球结构和过程以及它们与地表过程的关系的研究人员受益。该项目在英国和美国之间建立了一个新的国际合作研究项目，并将支持培训两名博士后研究员，一名在英国，一名在美国。具体的项目目标是开发一种变革性的联合波形建模和数据分析方法，以表征全局ULVZ结构。主要任务是：(1)收集对超低频振动结构敏感的新的全球地震波形数据库；(2)利用地震波场建模的最新发展，包括全波灵敏度核和差分波场映射，以确定地震到达对超低频振动结构的敏感性，并确定可能用于研究超低频振动特性的其他地震到达；(3)使用快速三维Born波形建模方法进一步发展波场建模方法，以便预测任何所需输入模型的地震波形，从而允许(4)通过贝叶斯概率反演确定全球ULVZ结构，以及(5)通过测试当前ULVZ的矿物物理模型来评估ULVZ的物理起源。这种方法代表了一种全新的研究地球深处局部结构的方法。这项工作的最终目的是从各个角度重新评估ulvz，并减少其性质，位置和组成的不确定性。最终，该项目将对极低频区存在情况进行全球评估，并确定其组成和地理范围，以及它们与地球内部其他动态特征的关系。

This project aims to image the Earth's deep interior using recordings of seismic waveforms generated by earthquakes occurring globally. Constraining the structure, composition and dynamic motions of the deep Earth, from which we have no definitive rock samples, is crucial to understanding both the forces that are actively shaping our Earth from formation to present, and hazards such as surface volcanism that arise from deep within the Earth. This study focuses on technical development of a new modeling approach combining data analysis and prediction of seismic waveforms, which will be applied to imaging features at the core-mantle boundary called ultralow-velocity zones (ULVZs). The existence of these ULVZs is well documented, and several past studies have linked them to important global Earth processes, such as melting, influx of core iron into the mantle, or the leftover remnants from a molten Earth early in its history. Yet what ULVZs physically represent remains in question. This research is aimed at determining what ULVZs are in terms of their composition, location, and relation to past and present processes inside the Earth. This work will provide crucial constraints on understanding how the Earth formed, what the ongoing dynamic motions within the Earth currently are, and how these motions are related to surface hot spot volcanism such as Hawaii and Yellowstone. This project aims to develop a new seismic waveform modeling approach that will allow for a new understanding of the origin of the complex seismic waveforms we routinely record from earthquakes worldwide and how these seismic waves are sensitive to small-scale features within the Earth. The methods and software developed in this project will be shared openly and will be applicable to a broad range of researchers who may wish to apply these techniques to different target areas. In addition, this research benefits a large area of researchers who work on determining Earth structure and processes and how they relate to surface processes. This project establishes a new international collaborative research effort between the United Kingdom and the USA and will support the training of two post-doctoral researcher fellows, one in the UK and one in the USA.The specific project goal is to develop a transformative joint waveform modeling and data analysis approach to characterize global ULVZ structure. The primary tasks are to (1) collect a new global database of seismic waveforms sensitive to ULVZ structure, (2) use recent developments in seismic wavefield modeling that includes full-wave sensitivity kernels and differential wavefield mapping to determine the sensitivity of seismic arrivals to ULVZ structure and to identify additional seismic arrivals that may be utilized to study ULVZ properties, (3) further the development of wavefield modeling approaches using a fast 3-D Born waveform modeling approach in order to predict seismic waveforms for any desired input model, which allows for (4) the determination of global ULVZ structure through a Bayesian probabilistic inversion, and (5) assess the physical origin of ULVZs by testing current mineral physics models of ULVZs. The approach represents an entirely new line of interrogating localized structures in the deep Earth. The ultimate aim of this work is to fundamentally reassess ULVZs from all angles, and reduce uncertainties in their properties, location, and composition. Ultimately this project will produce a global assessment of ULVZ existence as well as to determine their compositional and geographic scope, and how they are related to other dynamic features inside the Earth.