期刊文献+

USArray及其近期科学发现 被引量:6

USArray and Latest Scientific Discoveries
下载PDF
导出
摘要 美国台阵(USArray)是EarthScope计划的主要内容之一。旨在探测北美大陆变形、结构及其演化。USArray主要由平移/滚动台阵和机动台阵两部分构成。滚动台阵由400个宽频带地震台站组成,以向前滚动的方式扫过美国本土和阿拉斯加。利用来自该台阵的数据,科学家能获得地球内部精细图像,藉此考察地震和火山的过程。作为滚动台阵的补充,机动台阵被用于对关键目标进行详细观测和短期测量。美国台阵计划启动5年来,采集的数据已经提供了足以令科学界考虑重新审视地震物理、火山过程、核幔结构、活动变形构造、大陆结构及其演化、地球动力学和地壳流体等基本科学问题的基础资料。 USArray is one key component of EarthScope experiment to explore the formation, structure and evolution of the North American continent. The most important element of the USArray is Transportable and Flexible Array. The transportable Array consists of 400 broadband seismic stations installed across the continental United States and Alaska in a roll-along fashion. With data from this dense network of seismometers, researchers will be able to collect detailed images of the Earth's interior and investigate the processes controlling earthquakes and volcanoes. As the complement of Transportable Array, Flexible Array is available to scientists for dispatching to targeted areas for very detailed and short period studies.During the 5 years since it was started, the data acquired by USArray sensors have been providing the anticipated foundation for scientific community actively gaining new insights into earthquake physics, volcanic processes, core-mantle interactions, active deformation and tectonics, continental structure and evolution, geodynamics, and crustal fluids.
出处 《地质学报》 EI CAS CSCD 北大核心 2010年第6期847-853,共7页 Acta Geologica Sinica
基金 国家自然科学基金项目(编号40830316 40874045) 国家专项"深部探测技术与实验研究"(编号Sinoprobe-02) 国土资源部公益性行业基金(编号200811021)联合资助成果
关键词 美国台阵 科学发现 西北美洲大陆 莫霍面 岩石圈/软流圈边界 岩石圈拆沉 背景噪声成像 USArray scientific discoveries western North America continent Moho lithosphere-asthenosphere boundary lithospheric drip ambient noise tomography
  • 相关文献

参考文献13

  • 1Burdick S, Li C, Martynov V, Cox T, Eakins J, Mulder T, Astiz L, Vernon F L, Pavlis G L, van der Hilst R. 2008. Upper mantle heterogeneity beneath North America from travel time tomography with global and USArray transportable array data. Seis. Res. Lett. , 79: 384-392.
  • 2Campillo M, Paul A. 2003. Long-range correlations in the diffuse seismic coda. Science, 299: 547-549.
  • 3Creager K C, LaRoeca M, Galluzzo D, Vidale J E, Malone S, Sweet J. 2008. Caseadia tremor depths constrained by S minus P times. In; Report on the Aseismic slip, tremor, and earthquakes workshop. Open-File Report- U. S. Geological Survey.
  • 4Miller M S, Levander A. 2009. Receiver function images of the Western U. S. lithosphere. EarthScope Onsite Newsletter.http://www. EarthScope. org/es _ doc/onsite/onSite summer09. pdf.
  • 5Ricket T J, Claerbout J. 1999. Acoustic raylight imaging via spectral factorization: helioseismology and reservoir monitoring. The Leading Edge, 18:957-960.
  • 6Roux P, Sabra K G, Gerstoft P, et al . 2005. P-waves from cross-correlation of seismic noise. Geophysical Research Letters, 32, L19303, doi :10. 1029/ 2005GL023803.
  • 7Shapiro N M, Campillo M. 2004. Emergence of broadband rayleigh waves from correlations of the ambient seismic noise.Geophysical Research Letters, 31, L0614, doi : 10. 1029/ 2004GL019491.
  • 8Shapiro N M, Campillo M, Stehly L, Ritzwoller M H. 2005. High-resolution surface-wave tomography from ambient seismic noise. Science, 307 : 1615 - 1618.
  • 9Shapiro N M, Ritzwoller M H, Bensen G D. 2006. Source location of the 26 sec microseism from cross correlations of ambient seismic noise. Geophysical Research Letters, 33, L18310, doi: 10. 1029/2006GL027010.
  • 10Wapenaar K, Thorbecke J, Draganov D. 2004. Relations between reflection and transmission responses of three-dimensional inhomogeneous media. Geophysical Journal International, 156:179-194.

同被引文献111

引证文献6

二级引证文献33

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部