Travel time curves and isochron maps from the Borovoye digital archive for the Nevada and Semipalatinsk Nuclear Test Sites

K.S. Nepeina , Vadim An
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引用次数: 5

Abstract

The paper presents generalized parameters of digital seismograms of the Borovoye Geophysical Observatory (BRVK). The seismograms were obtained after reformatting the archive of the Institute of Geosphere Dynamics (IDG RAS). For this research, we consider looking at the most representative entries – underground nuclear explosions (UNE). The particular interest is the analysis of the P-wave travel times at the regional distances Δ≈5–7° and Δ≈89–91°. These deep paths cross the boundaries of the Earth crust, mantle and outer core. There are UNE digital records at the Semipalatinsk Test Site (ΔSTS ≈5.56–6.27°) and at the Nevada Test Site (ΔNTS≈89.77–90.15°). For this reason, we use UNEs from STS and NTS from 1967 to 1992. UNEs locations and magnitudes are taken from published open sources. The results for P-wave travel time curves on the BRVK – NTS and BRVK – STS paths and the isochron maps are obtained. The linear functions for travel time curves are defined by the linear regression. The resulting seismic travel time curves for P waves are compared to AK135. Because global one-dimensional seismic reference models are non-unique solution to regional seismic data, in terms of physical structure. The results help identify seismic wave velocities at the source-receiver travel paths and character of geologic media. Such physical models could significantly facilitate physical interpretation of seismic structures in the area of Central Asia (e.g. Tien Shan) and global.

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内华达和塞米巴拉金斯克核试验场Borovoye数字档案的旅行时间曲线和等时线地图
本文介绍了波罗沃耶地球物理观测站(BRVK)数字地震记录的广义参数。地震记录是对地球圈动力学研究所(IDG RAS)档案进行重新格式化后得到的。对于这项研究,我们考虑看看最具代表性的条目-地下核爆炸(UNE)。特别感兴趣的是在区域距离Δ≈5-7°和Δ≈89-91°处的p波传播时间的分析。这些深路穿过地壳、地幔和外核的边界。在塞米巴拉金斯克试验场(ΔSTS≈5.56-6.27°)和内华达试验场(ΔNTS≈89.77-90.15°)有UNE数字记录。出于这个原因,我们使用了1967年至1992年STS和NTS的UNEs。地震的位置和震级取自公开发布的资源。得到了BRVK - NTS和BRVK - STS路径上的纵波走时曲线和等时线图。旅行时间曲线的线性函数由线性回归定义。得到的地震走时曲线与AK135进行了比较。由于全球一维地震参考模型在物理结构方面不是区域地震资料的唯一解。这些结果有助于确定震源-接收地震波的传播路径和地质介质的特征。这种物理模型可以极大地促进中亚地区(如天山)和全球地震结构的物理解释。
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