Collaborative Research: Three-dimensional Onshore-Offshore MT Investigation of Cascadia Margin--Interpretation Phase

该项目的主要目标是了解地球深处沿着北美西北边缘的水分布情况，在那里，胡安·德富卡海洋板块俯冲到大陆之下，在地质历史上曾产生毁灭性的特大逆冲地震。 被困在俯冲板块和上覆大陆之间的水被假设为在控制这些地震的发生和震级以及该地区的其他地壳和地幔变形模式方面发挥重要作用。 本研究利用覆盖俄勒冈州和华盛顿大陆边缘的海岸-海上传感器阵列最近收集的电磁地球物理数据，构建地壳和地幔电导率的三维图像。由于这一物理性质对地球中流体的浓度很敏感，我们的结果将为流体和物理状态的空间变化提供独特的约束。 这些信息将被纳入从该地区丰富的地球物理和地质研究中得出的综合地震危险模型。该项目的第二个目标是开发强大的建模软件，用于大规模陆上-海上电磁阵列数据的三维解释，这是迄今为止很少尝试的。 通过该项目开发的工具和方法将广泛应用于未来的构造成像两栖电磁研究，以及能源和矿产勘探的两栖商业电磁调查。现在有相当多的证据表明，流体在最近发现的幕式震颤和滑动现象中起着重要作用。 至少，流体控制俯冲和上覆板块的流变特性，并降低沿板块界面沿着的有效正应力;更推测的是，流体可能是至关重要的幕式震颤和滑动动力学的机制，范围从渗透泵送和水力压裂，速率和状态相关的摩擦滑动。沿板块界面沿着倾斜的低地震速度层，以及只能用超压流体解释的低Vp/Vs比值区域，进一步暗示了俯冲大逆冲断层旋回中的流体。大地电磁数据对流体的存在和连通性高度敏感，因此代表了对系统的这一关键组成部分进行成像的理想地球物理工具。 在最近NSF资助的活动中收集了大约150个大地电磁站点（一半在陆上，一半在海上），横跨俄勒冈州和华盛顿南部边缘，结合EarthScope计划（可移动和柔性阵列）的数据和该地区的遗留数据，代表了一个独特的数据集，用于详细研究俯冲带环境中的流体。 该项目的主要重点是对这一合并的两栖大地电磁数据集进行完整的分析和三维反演，对从传入板块到岩浆弧附近的流体分布进行成像。海上数据的可用性将使人们更好地了解不太了解，但关键的细节，如流体输入的沟槽，他们对？锁定区域？两个板块之间，以及从下行板块释放的流体的分布，包括沿着发生幕式震颤和滑动的过渡带。相对密集的三维阵列覆盖范围将大大改善我们对边缘分割的理解，解决沿着Siletzia和克拉马斯省的结构和流体分布以及这些与幕式震颤和滑动的空间模式的关系。该项目还将导致开发更好的方法和工具，用于对两栖大地电磁数据集进行三维解释，这将对正在进行和计划进行的大陆边研究举措具有价值，并将有助于支持培训下一代跨学科电磁研究人员。

The principal goal of this project is to understand the distribution of water deep in the Earth along the northwest margin of North America, where the subduction of the Juan de Fuca oceanic plate beneath the continent has produced devastating mega-thrust earthquakes in the geologic past. Water trapped between the subducting plate and overlying continent is hypothesized to play an important role in controlling the occurrence and magnitude of these earthquakes, as well as other modes of crust and mantle deformation in the region. This study uses electromagnetic geophysical data that was collected recently with an onshore-offshore array of sensors covering the Oregon and Washington continental margin, to construct a three-dimensional image of crust and mantle electrical conductivity. Since this physical property is sensitive to the concentration of fluids in the Earth, our results will provide unique constraints on spatial variations of fluids and physical state. This information will be integrated into comprehensive seismic hazard models derived from the wealth of geophysical and geological studies in this region. A secondary goal of this project is to develop robust modeling software for the three-dimensional interpretation of large-scale onshore-offshore electromagnetic array data, something that has rarely, if ever, been attempted to date. The tools and methods developed through this project will have broad application to future amphibious electromagnetic studies for tectonic imaging, as well as amphibious commercial electromagnetic surveys for energy and mineral exploration.There is now considerable evidence that fluids play an important role in the relatively recently discovered phenomenon of episodic tremor and slip. At the least, fluids control rheological properties in the subducting and overriding plates and reduce effective normal stress along the plate interface; more speculatively fluids may be critical to episodic tremor and slip dynamics through mechanisms which range from permeability pumping and hydrofracturing, to rate-and-state dependent frictional slip. Dipping low seismic velocity layers along the plate interface, and regions of low Vp/Vs ratios that can only be explained by over-pressured fluids, further implicate fluids in the subduction megathrust cycle. Magnetotelluric data are highly sensitive to the presence and connectivity of fluids, and thus represent an ideal geophysical tool for imaging this critical component of the system. Approximately 150 magnetotelluric sites (half onshore and half offshore) collected in a recent NSF funded campaign across the Oregon and southern Washington margin, combined with data from the EarthScope program (transportable and flex array) and legacy data from the region, represent a unique dataset for a detailed study of fluids in a subduction zone setting. The main focus of this project is a complete analysis and three dimensional inversion of this merged amphibious magnetotelluric dataset, imaging the distribution of fluids from the incoming plate to near the magmatic arc. The availability of offshore data will allow improved understanding of poorly understood but critical details, such as fluid inputs at the trench, their impacts on the ?locked zone? between the two plates, and the distribution of fluids released from the down-going slab, including along the transitional zone where episodic tremor and slip occurs. The relatively dense three dimensional array coverage will greatly refine our understanding of margin segmentation, resolving the structure and fluid distribution along the Siletzia and Klamath provinces and the relationship of these to the spatial pattern of episodic tremor and slip. The project will also lead to development of improved methodologies and tools for three dimensional interpretation of amphibious magnetotelluric datasets, which will be of value to ongoing and planned initiatives for studies of continental margins, and will help support training of the next generation of interdisciplinary electromagnetic researchers.