权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

Double-difference attenuation tomography method and pilot applications

双差衰减层析成像方法及试点应用

基本信息

批准号：
1724685
负责人：
Clifford Thurber
金额：
$ 8.63万
依托单位：
University of Wisconsin-Madison
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2017
资助国家：
美国
起止时间：
2017-06-01 至 2020-05-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1724685&HistoricalAwards=false
关键词：
Double difference attenuation tomography method

项目摘要

Seismologists use seismic waves to construct images of the Earth's internal structure, termed seismic tomography, analogous to the way doctors use X-rays to construct images of the human brain with CAT scans (Computerized Axial Tomography). In seismology, tomography is most often done using measured travel times of seismic waves to infer the seismic wave velocity structure within the Earth. Another possibility is to use the amplitudes of seismic waves at different frequencies to infer the Earth's attenuation structure, that is, to identify regions where seismic waves lose energy more or less than normal. In this project, the researchers will develop and test a new method to image attenuation structure, with fine spatial resolution, using measured attenuation differences between waves from pairs of nearby earthquakes. The effectiveness of the method will be evaluated on earthquake data from northern Honshu, Japan, and The Geysers geothermal field, California. In the former case, the researchers will endeavor to image three-dimensional attenuation variations deep within the Earth, which will provide insight into the zone where magmas originate that erupt at "Ring of Fire" volcanoes and also into the nature of deep earthquakes. In the latter case, the goal is to detect changes in attenuation structure within the geothermal system over time, which can be used to monitor fracturing changes due to geothermal exploitation or stimulation.This project will develop a new method termed ?double-difference attenuation tomography?, that will be tested on synthetic data, and applied to two regions of interest. The concept is to do for seismic attenuation imaging what double-difference location has done for hypocenter locations and double-difference tomography has done jointly for hypocenter locations and seismic velocity imaging. The key development is event-pair differential t* analysis, which contrasts with previous differential t* analysis methods, which have generally utilized either a phase-pair or a station-pair approach. A spectral ratio approach for nearby event pairs will be used to obtain the event-pair differential t* values, analogous to how waveform cross-correlation is used to obtain differential times for double-difference location and double-difference tomography. This method will be thoroughly tested on both synthetic and real data. Two areas have been selected for applying the new double-difference attenuation tomography method: The Geyser geothermal field, California, and Northern Honshu, Japan. These areas were chosen both for their intrinsic interest and for the availability of results from previous studies to which our results can be compared. This method has the potential for obtaining very high resolution images of seismic attenuation structure in the regions where earthquakes occur. Seismic attenuation is a strong complement to seismic velocity in efforts to distinguish lithology, saturation, fracturing, and temperature in the subsurface, and these factors can affect velocities and attenuation differently. In some of the applications that we envision, high-resolution detection of temporal changes in attenuation is a realizable goal. Many of the possible applications are to problems of high societal importance, such as geothermal energy, mining, wastewater disposal, fracking, CO2 sequestration, and volcanoes. The project will support a female early career scientist and a graduate student.

地震学家使用地震波构建地球内部结构的图像，称为地震断层扫描，类似于医生使用X射线通过CAT扫描(计算机化的轴向断层扫描)构建人脑图像的方式。在地震学中，层析成像通常使用测量的地震波传播时间来推断地球内部的地震波速度结构。另一种可能性是利用不同频率的地震波幅度来推断地球的衰减结构，即识别地震波损失能量高于或低于正常水平的区域。在这个项目中，研究人员将开发和测试一种新的方法来成像衰减结构，具有精细的空间分辨率，使用测量的附近地震波之间的衰减差异。该方法的有效性将在日本本州北部和加利福尼亚州间歇泉地热场的地震数据上进行评估。在前一种情况下，研究人员将努力成像地球深处的三维衰减变化，这将为洞察“火环”火山喷发的岩浆起源区域以及深部地震的性质提供洞察。在后一种情况下，目标是检测地热系统内衰减结构随时间的变化，可用于监测地热开采或刺激引起的破裂变化。该项目将开发一种名为“双差衰减层析成像”的新方法，该方法将在合成数据上进行测试，并应用于两个感兴趣的区域。这一概念是为了进行地震衰减成像，就像双差定位对震源位置所做的那样，双差层析成像对震源位置和地震速度成像联合进行。关键的发展是事件对差分t*分析，它不同于以往的差分t*分析方法，后者通常使用相位对或站对方法。将使用附近事件对的频谱比率方法来获得事件对差分t*值，类似于如何使用波形互相关来获得用于双差定位和双差层析成像的差分时间。这种方法将在合成数据和真实数据上进行彻底测试。已经选择了两个地区应用新的双差衰减层析成像方法：加利福尼亚州的间歇泉地热田和日本本州北部。选择这些领域既是因为它们的内在兴趣，也是因为我们可以与以前研究的结果进行比较。这种方法有可能获得发震地区的地震衰减结构的极高分辨率图像。在区分地下岩性、饱和度、裂缝和温度方面，地震衰减是对地震速度的有力补充，这些因素可能会以不同的方式影响速度和衰减。在我们设想的一些应用中，高分辨率检测衰减的时间变化是一个可以实现的目标。许多可能的应用是针对具有高度社会重要性的问题，例如地热能、采矿、废水处理、水力压裂、二氧化碳封存和火山。该项目将支持一名女性早期职业科学家和一名研究生。