Preliminary Moho depth determination from receiver function analysis using AlpArray stations in Hungary
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作者:
Dániel Kalmár
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机构:Eötvös Loránd University,Department of Geophysics and Space Science, Institute of Geography and Earth Sciences
Dániel Kalmár
Bálint Süle
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机构:Eötvös Loránd University,Department of Geophysics and Space Science, Institute of Geography and Earth Sciences
Bálint Süle
István Bondár
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机构:Eötvös Loránd University,Department of Geophysics and Space Science, Institute of Geography and Earth Sciences
István Bondár
机构:
[1] Eötvös Loránd University,Department of Geophysics and Space Science, Institute of Geography and Earth Sciences
[2] Hungarian Academy of Sciences (MTA CSFK GGI KRSZO),Kövesligethy Radó Seismological Observatory, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences
Pannonian Basin;
AlpArray project;
Receiver function analysis;
Moho discontinuity;
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摘要:
Receiver function analysis is applied to the western part of the Pannonian Basin, a rather complex region both geologically and geodynamically. Previous receiver function analyses in this region had to deal with much smaller station density and time span than those available to us. In the analysis we used the data of some 48 seismological stations. These include not only the permanent stations from Hungary and permanent stations from neighbouring countries (Slovakia and Slovenia), but also the temporary broadband stations that were installed within the framework of the AlpArray project. Having applied rather strict manual quality control on the calculated radial receiver functions we stacked the receiver functions. Using the H–K grid search method we determined the Moho depth and the Vp/Vs ratio beneath the seismological stations in the western part of the Pannonian Basin. The unprecedented density of the AlpArray network, combined with the permanent stations, allowed us to derive high resolution Moho and Vp/Vs maps for the West Pannonian Basin, together with uncertainty estimates. Our preliminary results agree well with previous studies and complement them with finer details on the Moho topography and crustal thickness.
机构:
Univ Illinois, Dept Earth Sci & Environm Change, Champaign, IL 61820 USA
Peking Univ, Sch Earth & Space Sci, State Key Lab Deep Earth & Mineral Explorat, Beijing, Peoples R ChinaUniv Illinois, Dept Earth Sci & Environm Change, Champaign, IL 61820 USA
机构:
Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
Univ Chinese Acad Sci, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
Song, Penghan
Zhang, Xuemei
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机构:
China Earthquake Networks Ctr, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
Zhang, Xuemei
Liu, Youshan
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机构:
Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
Liu, Youshan
Teng, Jiwen
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机构:
Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R ChinaChinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China