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Source Specific Station Corrections for Regional Phases at Fennoscandian Stations

机译:Fennoscandian站的区域阶段的特定于源站的校正

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摘要

— The IASPEI91 global travel-time curves are used as the default for event location at the Prototype International Data Center (PIDC). In order to improve event location, a 1-D Baltic travel-time model was implemented at the PIDC in 1997 for locating events using regional phases from Fennoscandian stations. Where a single model is insufficient for characterizing the regional geology, path-dependent corrections, or Source Specific Station Corrections (SSSCs), are more appropriate for event locations. We have developed SSSCs for regional phases at the Fennoscandian stations by interpolating travel times through different 1-D models. SSSCs for stations NRIS and SPITS are also derived, given the fact that paths from both stations to high latitude events are within the Fennoscandia regionalization as Baltic.¶Validation testing of the SSSCs demonstrates that using SSSCs in event location is superior to not using SSSCs, a nd, in most cases, to using the 1-D model directly when locating events. For a ground-truth data set which includes events in the Baltic Shield with location accuracy better than 2 km, the average improvement in location due to SSSCs is 9 km, and the median coverage ellipse is reduced by 2710 km2 (from 3830 to 1120 km2). These results are similar to those obtained using the 1-D Baltic model. For a CEB (Calibration Event Bulletin) data set which includes events along the North Atlantic oceanic ridge and in central/southern Europe, using SSSCs the ridge events move closer to the ridge axis, and the European events move closer to CEB locations than 1-D Baltic locations. For a constrained JHD (Joint Hypocenter Determination) data set of events in the Novaya Zemlya region, when using SSSCs or the 1-D Baltic model, relative to the JHD locations mislocations are less or similar to those without SSSCs. All coverage ellipses are smaller but sti ll contain the JHD solutions.¶Our SSSCs are strongly dependent on the 1-D regional models and regionalization. Future development in 1-D velocity models and travel-time curves should improve such SSSCs, event locations, and uncertainties. It is hoped that the implementation and demonstration of SSSCs in the PIDC software will encourage these further developments. These SSSCs were implemented at the PIDC for Reviewed Event Bulletin (REB) location in April 1999.
机译:— IASPEI91全球旅行时间曲线被用作原型国际数据中心(PIDC)上事件位置的默认值。为了改善事件的位置,1997年在PIDC实施了1-D波罗的海旅行时间模型,用于使用Fennoscandian站的区域阶段来定位事件。如果单个模型不足以描述区域地质特征,则更适合于事件位置,尤其是路径依赖的校正或源特定站校正(SSSC)。我们通过插值不同一维模型的旅行时间,为芬诺斯坎迪安站开发了区域阶段的SSSC。假设从两个站到高纬度事件的路径都在Fennoscandia区域内(如波罗的海),也得出了NRIS和SPITS站的SSSC。对SSSC的验证测试表明,在事件位置使用SSSC优于不使用SSSC,并且在大多数情况下,在定位事件时直接使用一维模型。对于包含波罗的海盾事件且定位精度优于2 km的地面真实数据集,SSSC导致的位置平均改善为9 km,中位覆盖椭圆率降低了2710 km2 (从3830至1120 km2 )。这些结果类似于使用一维波罗的海模型获得的结果。对于CEB(校准事件公告)数据集,该数据集包括沿北大西洋海脊和中欧/南欧的事件,使用SSSC时,海脊事件更靠近海脊轴,而欧洲事件则比1-更靠近CEB位置。 D波罗的海地区。对于Novaya Zemlya地区中受约束的JHD(联合震源确定)数据集,当使用SSSC或一维波罗的海模型时,相对于JHD位置而言,错位比没有SSSC的错位少或相似。所有的覆盖椭圆都较小,但包含JHD解决方案。¶我们的SSSC强烈依赖于一维区域模型和区域化。一维速度模型和行程时间曲线的未来发展应改善此类SSSC,事件位置和不确定性。希望PIDC软件中SSSC的实现和演示将鼓励这些进一步的发展。这些SSSC在1999年4月的PIDC审查事件公告(REB)地点实施。

著录项

  • 来源
    《Pure and Applied Geophysics》 |2001年第2期|35-57|共23页
  • 作者单位

    Science Applications International Corporations Center for Monitoring Research 1300 N. 17th Street Arlington VA 22209 USA. E-mail: xiaoping@cmr.gov;

    Science Applications International Corporations Center for Monitoring Research 1300 N. 17th Street Arlington VA 22209 USA. E-mail: xiaoping@cmr.gov;

    Science Applications International Corporations Center for Monitoring Research 1300 N. 17th Street Arlington VA 22209 USA. E-mail: xiaoping@cmr.gov;

    Science Applications International Corporations Center for Monitoring Research 1300 N. 17th Street Arlington VA 22209 USA. E-mail: xiaoping@cmr.gov;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Key words: SSSCs; Fennoscandia; travel time; event location; IMS; PIDC.;

    机译:关键字:SSSC;芬诺斯堪迪亚;旅行时间;活动地点;IM小号;PIDC。;

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