FN Archimer Export Format
PT J
TI Arrival angles of teleseismic fundamental mode Rayleigh waves across the AlpArray
BT 
AF KOLINSKY, Petr
   BOKELMANN, Goetz
   HETENYI, Gyorgy
   ABREU, Rafael
   ALLEGRETTI, Ivo
   APOLONER, Maria-Theresia
   AUBERT, Coralie
   BESANCON, Simon
   BES DE BERC, Maxime
   BOKEL-MANN, Gotz
   BRUNEL, Didier
   CAPELLO, Marco
   CARMAN, Martina
   CAVALIERE, Adriano
   CHEZE, Jerome
   CHIARABBA, Claudio
   CLINTON, John
   COUGOULAT, Glenn
   CRAWFORD, Wayne C.
   CRISTIANO, Luigia
   CZIFRA, Tibor
   D'ALEMA, Ezio
   DANESI, Stefania
   DANIEL, Romuald
   DANNOWSKI, Anke
   DASOVIC, Iva
   DESCHAMPS, Anne
   DESSA, Jean-Xavier
   DOUBRE, Cecile
   EGDORF, Sven
   FIKET, Tomislav
   FISCHER, Kasper
   FRIEDERICH, Wolfgang
   FUCHS, Florian
   FUNKE, Sigward
   GIARDINI, Domenico
   GOVONI, Aladino
   GRACZER, Zoltan
   GROSCHL, Gidera
   HEIMERS, Stefan
   HEIT, Ben
   HERAK, Davorka
   HERAK, Marijan
   HUBER, Johann
   JARIC, Dejan
   JEDLICKA, Petr
   JIA, Yan
   JUND, Helene
   KISSLING, Edi
   KLINGEN, Stefan
   KLOTZ, Bernhard
   KOLINSKY, Petr
   KOPP, Heidrun
   KORN, Michael
   KOTEK, Josef
   KUHNE, Lothar
   KUK, Kreso
   LANGE, Dietrich
   LOOS, Jurgen
   LOVATI, Sara
   MALENGROS, Deny
   MARGHERITI, Lucia
   MARON, Christophe
   MARTIN, Xavier
   MASSA, Marco
   MAZZARINI, Francesco
   MEIER, Thomas
   METRAL, Laurent
   MOLINARI, Irene
   MORETTI, Milena
   NARDI, Anna
   PAHOR, Jurij
   PAUL, Anne
   PEQUEGNAT, Catherine
   PETERSEN, Daniel
   PESARESI, Damiano
   PICCININI, Davide
   PIROMALLO, Claudia
   PLENEFISCH, Thomas
   PLOMEROVA, Jaroslava
   PONDRELLI, Silvia
   PREVOLNIK, Snjezan
   RACINE, Roman
   REGNIER, Marc
   REISS, Miriam
   RITTER, Joachim
   RUMPKER, Georg
   SALIMBENI, Simone
   SANTULIN, Marco
   SCHERER, Werner
   SCHIPPKUS, Sven
   SCHULTE-KORTNACK, Detlef
   SIPKA, Vesna
   SOLARINO, Stefano
   SPALLAROSSA, Daniele
   SPIEKER, Kathrin
   STIPCEVIC, Josip
   STROLLO, Angelo
   SULE, Balint
   SZANYI, Gyongyver
   SZUCS, Eszter
   THOMAS, Christine
   THORWART, Martin
   TILMANN, Frederik
   UEDING, Stefan
   VALLOCCHIA, Massimiliano
   VECSEY, Ludek
   VOIGT, Rene
   WASSERMANN, Joachim
   WEBER, Zoltan
   WEIDLE, Christian
   WESZTERGOM, Viktor
   WEYLAND, Gauthier
   WIEMER, Stefan
   WOLF, Felix
   WOLYNIEC, David
   ZIEKE, Thomas
   ZIVCIC, Mladen
   ZLEBCIKOVA, Helena
AS 1:1;2:1;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:;31:;32:;33:;34:;35:;36:;37:;38:;39:;40:;41:;42:;43:;44:;45:;46:;47:;48:;49:;50:;51:;52:1;53:;54:;55:;56:;57:;58:;59:;60:;61:;62:;63:;64:;65:;66:;67:;68:;69:;70:;71:;72:;73:;74:;75:;76:;77:;78:;79:;80:;81:;82:;83:;84:;85:;86:;87:;88:;89:;90:;91:;92:;93:;94:;95:;96:;97:;98:;99:;100:;101:;102:;103:;104:;105:;106:;107:;108:;109:;110:;111:;112:;113:;114:;115:;116:;117:;118:;119:;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:;31:;32:;33:;34:;35:;36:;37:;38:;39:;40:;41:;42:;43:;44:;45:;46:;47:;48:;49:;50:;51:;52:;53:;54:;55:;56:;57:;58:;59:;60:;61:;62:;63:;64:;65:;66:;67:;68:;69:;70:;71:;72:;73:;74:;75:;76:;77:;78:;79:;80:;81:;82:;83:;84:;85:;86:;87:;88:;89:;90:;91:;92:;93:;94:;95:;96:;97:;98:;99:;100:;101:;102:;103:;104:;105:;106:;107:;108:;109:;110:;111:;112:;113:;114:;115:;116:;117:;118:;119:;
C1 Univ Vienna, Dept Meteorol & Geophys, A-1090 Vienna, Austria.
C2 UNIV VIENNA, AUSTRIA
IF 2.574
TC 10
UR https://archimer.ifremer.fr/doc/00690/80172/83241.pdf
   https://archimer.ifremer.fr/doc/00690/80172/83242.docx
LA English
DT Article
CR ALPARRAY LEG1
BO Pourquoi pas ?
DE ;Structure of the Earth;Europe;Time-series analysis;Surface waves and free oscillations;Wave propagation;Wave scattering and diffraction
AB The dense AlpArray network allows studying seismic wave propagation with high spatial resolution. Here we introduce an array approach to measure arrival angles of teleseismic Rayleigh waves. The approach combines the advantages of phase correlation as in the two-station method with array beamforming to obtain the phase-velocity vector. 20 earthquakes from the first two years of the AlpArray project are selected, and spatial patterns of arrival-angle deviations across the AlpArray are shown in maps, depending on period and earthquake location. The cause of these intriguing spatial patterns is discussed. A simple wave-propagation modelling example using an isolated anomaly and a Gaussian beam solution suggests that much of the complexity can be explained as a result of wave interference after passing a structural anomaly along the wave paths. This indicates that arrival-angle information constitutes useful additional information on the Earth structure, beyond what is currently used in inversions. 
PY 2019
PD JUN
SO Geophysical Journal International
SN 0956-540X
PU Oxford Univ Press
VL 218
IS 1
UT 000470320500008
BP 115
EP 144
DI 10.1093/gji/ggz081
ID 80172
ER

EF