Collaborative Research: High resolution passive seismic imaging beneath Valles Caldera

山谷火山口是北美三座超级火山之一，拥有悠久的火山活动历史，有记录的岩浆流动可追溯到约 70,000 年。地震成像可以通过使用地震波以类似于医学成像中的超声检查的方式对火山地下结构进行可视化。 直到最近，火山口山谷的地震成像仍然缺乏，这反过来又阻碍了对融化量、融化程度的估计和对管道系统的了解。 2019 年，德克萨斯大学埃尔帕索分校 (UTEP) 和新墨西哥大学 (UNM) 联合部署了一条 97 地震仪线，跨越整个火山口，持续 1 个月。 该计划的主要目标是解决火山口下熔体的空间范围和集中度，以及其他长期存在的问题，包括穹顶下方任何岩浆体的深度、火山口内填充物和断裂基底块的厚度以及地壳/地幔边界的性质。研究人员利用尖端技术探索并揭示了火山的地下岩浆系统，并促进了 UTEP 和 UNM 这两个少数族裔服务机构之间的合作。 该项目的成果改善了该地区的地震和火山灾害评估，并支持对科学领域代表性不足的少数族裔的研究生和本科生的培训。瓦莱斯火山口是一座第四纪活跃的超级火山，是火山口复活的教科书例子。在过去的二十年里，它基本上逃脱了地震审查。在这里，研究人员探测了山谷火山口下方的岩浆系统。 他们量化了熔体结构的空间范围、散射边界的深度和位置，并评估了火山口系统假定的抗震性质。利用环境噪声地震干涉测量来估计长周期瑞利波和洛夫波的色散曲线；这些将在跨维贝叶斯方案中与接收器函数、H/V 比和噪声自相关进行联合反演。 目标是准确估计山谷火山口下的速度结构。目标包括通过剪切波速度和 Vp/Vs 估计来界定熔体的空间范围和浓度，通过散射波分析确定复活穹顶下岩浆结构和破火山口填充的深度，以及检测和定位可能揭示岩浆和流体运动的任何局部地震活动。该项目补充了洛斯阿拉莫斯国家实验室稀疏的长期地震监测工作。它可以作为教育入门书，也是对使用火山口作为天然实验室的频繁地球物理学野外露营的补充。其成果改善了对火山生命周期阶段的评估，并可以更好地与其他第四纪超级火山进行比较。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。

The Valles caldera is one of three supervolcanoes in North America and has a long history of volcanism with documented magma flows as recent as ~70,000 years. Seismic imaging allows visualization of volcanic subterranean structures by using seismic waves in a similar way ultrasound sonography in medical imaging. Seismic imaging of the Valles Caldera was lacking until recently, which in turn has hindered estimate of melt volumes, melt extent, and understanding of the plumbing system. A joint University of Texas at El Paso (UTEP)/University of New Mexico (UNM) deployment in 2019 resulted in a 97-seismometer line crossing the entire caldera for 1 month. A primary objective of this initiative is to resolve the spatial extent and concentration of melt under the caldera, with other standing questions including the depth of any magma body underlying the dome, the thickness of intra-caldera fill and fractured basement blocks, and the nature of the crust/mantle boundary. Using cutting edge techniques, researchers probe and unveil the subterranean magmatic system of the volcano and foster a collaboration between UTEP and UNM, two minority serving institutions. The outcomes of this project improve earthquake and volcanic hazard assessment in the region, and support the training of graduate and undergraduate students from underrepresented minorities in science. The Valles caldera, a Quaternary-active supervolcanoes, is the textbook example of a resurgent caldera. It has largely escaped seismic scrutiny in the past two decades. Here the researchers probe the magmatic system beneath Valles caldera. They quantify the spatial extent of melt structures, the depth and emplacement of scattering boundaries, and assess the assumed aseismic nature of the caldera system. Ambient noise seismic interferometry is leveraged to estimate dispersion curves for long period Rayleigh and Love waves; these will be jointly inverted in a transdimensional Bayesian scheme with receiver functions, H/V ratios, and noise autocorrelations. The goal is to accurately estimate velocity structures under the Valles caldera. Targets include bounding the spatial extent and concentration of melt through shear-wave velocity and Vp/Vs estimates, depth to magmatic structures and caldera fill under the resurgent dome through scattered wave analysis, and detection and location of any local seismicity that may reveal magma and fluid movements. This project complements sparser long-term seismic monitoring efforts by Los Alamos National laboratory. It serves as an educational primer and complement to frequent geophysics field camps using the caldera as a natural laboratory. Its outcomes improve the assessment of the volcano life-cycle stage and allow better comparison with other Quaternary supervolcanoes.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.