CAREER: Illuminating the Tectonic History of North America with Seismic Models of Shear Attenuation and Velocity

职业：用剪切衰减和速度的地震模型阐明北美的构造历史

• 批准号: 1553367
• 负责人: Colleen Dalton
• 金额: $ 52.14万
• 依托单位: Brown University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2016
• 资助国家: 美国
• 起止时间: 2016-04-01 至 2023-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1553367&HistoricalAwards=false
• 关键词: CAREER; Illuminating; Tectonic; History; North

Title: CAREER: Illuminating the Tectonic History of North America with Seismic Models of Shear Attenuation and VelocityThe North American continent contains vastly diverse geology, from the volcanoes and mountains in the west to the interior plains that anchor the central United States and the broad Appalachian hills that roll into the Atlantic Ocean. This topography reflects the many episodes of continental collision, breakup, and modification that the land mass has experienced over billions of years. The movements of the tectonic plates at Earth?s surface are inextricably linked to the movement of rocks in Earth?s mantle (mantle convection). Understanding the connection between the Earth?s interior and surface is essential to addressing fundamental questions about how continents are created, how they evolve over time, and how they are destroyed. This study will use seismic waves generated by earthquakes to image the properties of the crust and mantle beneath North America, with particular emphasis on imaging in three dimensions the energy loss (attenuation) experienced by seismic waves. While it is generally acknowledged that seismic attenuation has the potential to be a valuable source of information about the Earth?s interior, it is difficult to isolate attenuation from other wave-propagation phenomena, which has historically limited its use by researchers. Integrated research and education activities will utilize data recorded by the NSF EarthScope USArray seismometers, which have recorded what is likely the best data set in existence to confront these challenges.This project will investigate, using new data analysis and seismic-wavefield simulations, the three-dimensional variations in shear attenuation beneath North America. This study will also develop a 3-D model of shear velocity in the upper mantle and, through joint interpretation with the attenuation model and laboratory measurements of attenuation and wave speed, place constraints on the variations in temperature, composition, partial melt, and water in the North American upper mantle. The attenuation model will be derived from measurements of Rayleigh wave amplitude and body-wave attenuation at USArray stations throughout the contiguous United States, and the velocity model will be derived from Rayleigh wave travel-time and local site-amplification observations. Separating the competing effects of focusing by elastic structure and anelastic decay on the Rayleigh wave amplitudes is the primary obstacle to imaging small-scale attenuation variations; spectral-element simulations with high-resolution elastic models for the U.S. that have been made possible by USArray will be used to compute focusing effects with greatly improved accuracy. The educational activities are targeted at high-school and undergraduate students. Educational seismometers will be installed at two Providence, RI area high schools. Data recorded by these seismometers and USArray stations will be used to engage the high-school students in earthquake science, fundamental properties of waves, and the tectonic history of North America. Teaching modules utilizing these data that address the Next Generation Science Standards (NGSS) will be developed and disseminated more widely. At the undergraduate level summer interns will carry out research projects at Brown during three summers, and a new field course in Environmental Geophysics will be developed.

职务名称：职业：用剪切衰减和速度的地震模型阐明北美的构造历史北美大陆包含着多种多样的地质，从西部的火山和山脉到锚住美国中部的内陆平原，再到广阔的阿巴拉契亚山脉，这些山脉一直延伸到大西洋。这种地形反映了数十亿年来大陆块经历的许多大陆碰撞，分裂和修改。地球板块的运动？地球的表面与地球上的岩石运动有着千丝万缕的联系？s地幔（地幔对流）。了解地球之间的联系？地球的内部和表面对于解决大陆是如何形成的，它们如何随着时间的推移而演变以及它们是如何毁灭的基本问题至关重要。这项研究将利用地震产生的地震波对北美地壳和地幔的特性进行成像，特别强调对地震波经历的能量损失（衰减）进行三维成像。虽然人们普遍认为，地震衰减有可能成为一个有价值的信息来源，对地球？由于它的内部，很难将衰减与其他波传播现象隔离开来，这在历史上限制了研究人员的使用。综合研究和教育活动将利用美国国家科学基金会EarthScope USAray地震仪记录的数据，这些地震仪记录的数据可能是应对这些挑战的现有最佳数据集，该项目将利用新的数据分析和地震波场模拟，调查北美地下剪切衰减的三维变化。这项研究还将开发一个上地幔剪切速度的三维模型，并通过与衰减模型和衰减和波速的实验室测量的联合解释，限制北美上地幔的温度，成分，部分熔融和水的变化。衰减模型将从美国邻近地区USAray台站的瑞利波振幅和体波衰减测量结果中得出，速度模型将从瑞利波走时和当地场地放大观测结果中得出。分离弹性结构和滞弹性衰减对瑞利波振幅的聚焦的竞争效应是成像小尺度衰减变化的主要障碍; USAray已经实现的美国高分辨率弹性模型的谱元模拟将用于计算聚焦效应，其精度大大提高。教育活动的对象是高中生和大学生。教育地震仪将安装在两个普罗维登斯，国际扶轮地区高中。这些地震仪和USAray台站记录的数据将用于让高中生参与地震科学、波的基本特性和北美的构造历史。将开发和更广泛地传播利用这些数据的教学模块，这些模块涉及下一代科学标准。在本科阶段，暑期实习生将在布朗大学开展为期三个夏季的研究项目，并将开发一门新的环境地球物理学实地课程。