Moho depth across the Trans-European Suture Zone from P- and S-receiver functions
B Knapmeyer-Endrun, F Krüger… - Geophysical Journal …, 2014 - academic.oup.com
The Mohorovičić discontinuity, Moho for short, which marks the boundary between crust and
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
[引用 ][C] Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun, F Kruger - Geophysical Journal International, 2014 - cir.nii.ac.jp
Moho depth across the Trans-European Suture Zone from P- and S-receiver functions | CiNii
Research CiNii国立 情報 学 研究所 学術 情報 ナビゲータ[サイニィ] 詳細 へ移動 検索 フォームへ移動 …
Research CiNii
[PDF][PDF] Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun - Geophys. J. Int, 2014 - researchportal.helsinki.fi
SUMMARY The Mohorovicic discontinuity, Moho for short, which marks the boundary
between crust and mantle, is the main first-order structure within the lithosphere …
between crust and mantle, is the main first-order structure within the lithosphere …
[PDF][PDF] Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun - Geophys. J. Int, 2014 - helda.helsinki.fi
SUMMARY The Mohorovicic discontinuity, Moho for short, which marks the boundary
between crust and mantle, is the main first-order structure within the lithosphere …
between crust and mantle, is the main first-order structure within the lithosphere …
Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun, F Krüger - Geophysical Journal …, 2014 - ieeexplore.ieee.org
The Mohorovičić discontinuity, Moho for short, which marks the boundary between crust and
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
[PDF][PDF] Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
Geophys. J. Int, 2014 - researchgate.net
SUMMARY The Mohorovicic discontinuity, Moho for short, which marks the boundary
between crust and mantle, is the main first-order structure within the lithosphere …
between crust and mantle, is the main first-order structure within the lithosphere …
[PDF][PDF] Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
Geophys. J. Int, 2014 - core.ac.uk
SUMMARY The Mohorovicic discontinuity, Moho for short, which marks the boundary
between crust and mantle, is the main first-order structure within the lithosphere …
between crust and mantle, is the main first-order structure within the lithosphere …
Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun, F Krüger… - Geophysical …, 2014 - ui.adsabs.harvard.edu
The Mohorovičić discontinuity, Moho for short, which marks the boundary between crust and
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun, F Krüger - Geophysical journal …, 2014 - publishup.uni-potsdam.de
The Mohorovicic discontinuity, Moho for short, which marks the boundary between crust and
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
mantle, is the main first-order structure within the lithosphere. Geodynamics and tectonic …
Moho depth across the Trans-European Suture Zone from P-and S-receiver functions
B Knapmeyer-Endrun, F Kruger… - Geophysical …, 2014 - researchportal.helsinki.fi
Abstract The Mohorovicic discontinuity, Moho for short, which marks the boundary between
crust and mantle, is the main first-order structure within the lithosphere. Geodynamics and …
crust and mantle, is the main first-order structure within the lithosphere. Geodynamics and …