P- and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban - Geophysical Journal International, 2009 - academic.oup.com
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
[HTML][HTML] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro… - … Journal, Volume 179 …, 2009 - adsabs.harvard.edu
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30 N-
55 N, 5 W-40 E), extending in depth up to 700 km and constrained by inversion of data from …
55 N, 5 W-40 E), extending in depth up to 700 km and constrained by inversion of data from …
P‐ and S‐velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro… - Geophysical Journal …, 2009 - Wiley Online Library
We present a new tomographic model for P‐and S‐velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
[PDF][PDF] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, M Kaban, M Tesauro… - Geophysical Journal …, 2009 - gfzpublic.gfz-potsdam.de
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30◦
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro… - Geophysical Journal …, 2009 - ieeexplore.ieee.org
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …
[PDF][PDF] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro, S Cloetingh - Geophys. J. Int, 2009 - ipgg.sbras.ru
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30◦
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
[引用][C] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro… - Geophysical Journal …, 2009 - elibrary.ru
[PDF][PDF] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro, S Cloetingh - Geophys. J. Int, 2009 - Citeseer
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30◦
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
[PDF][PDF] P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro, S Cloetingh - Geophys. J. Int, 2009 - ivan-art.com
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30◦
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
P-and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data
I Koulakov, MK Kaban, M Tesauro, S Cloetingh - 2009 - ricerca.unityfvg.it
We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30◦
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …
N–55◦ N, 5◦ W–40◦ E), extending in depth up to 700 km and constrained by inversion of data …