Number of items: 17.
B
Berhorst, A.,
Flueh, E. R.,
McIntosh, K.,
Ranero, C.,
Silver, E.,
Walther, C.,
Dole, J. and
Strauch, W.
(2002)
The crustal structure of the convergent Nicaraguan margin from a combined reflection and refraction study.
[Talk]
In: EGS XXVII General Assembly. , 21.- 26.04.2002, Nice, France .
Berhorst, A.,
Flueh, E. R.,
McIntosh, K.,
Ranero, C.,
Silver, E.,
Walther, C. H.,
Dole, J. and
Strauch, W.
(2002)
The crustal structure of the convergent Nicaraguan margin from a combined MCS and refraction study.
[Talk]
In: DGG - 62. Jahrestagung. , 03.- 08.03.2002, Hannover, Germany .
E
F
Flüh, E. R.,
Bialas, J. ,
Walther, C. H. E.,
Fekete, N.,
Thierer, P. O.,
Charvis, P.,
Collot, J. Y. and
Sallares, V.
(2002)
SO159 - SALIERI: Krustenstruktur des Carnegie Rückens und des ecuadorianischen Kontinentalrandes.
[Talk]
In: DGG - 62. Jahrestagung. , 03.- 08.03.2002, Hannover, Germany .
Fretzdorff, S.,
Garbe-Schönberg, C. D.,
Fietzke, J. ,
Livermore, R. A. and
Stoffers, P.
(2002)
High precision U-series isotope measurements of East Scotia back-arc basalts using single-collector -sector-field ICPMS.
[Talk]
In: Goldschmidt Tagung 2002. , 18.- 23.08.2002, Davos, Schweiz .
K
L
M
R
S
Sauter, A.,
DeShon, H. R.,
Schwartz, S.,
Newman, A.,
Protti, M.,
Dixon, T. H. and
Flueh, E. R.
(2002)
Seismic attenuation in the subduction zone of Costa Rica.
[Talk]
In: EGS XXVII General Assembly. , 21.- 26.04.2002, Nice, France .
Sauter, A.,
Schwartz, S.,
DeShon, H. R.,
Newman, A.,
Protti, M.,
Bilek, S. L.,
Flueh, E. R. and
Dixon, T. H.
(2002)
Seismic Attenuation in the Subduction Zone of Costa Rica.
[Talk]
In: AGU Fall Meeting 2002. , 06.- 10.12.2002, San Francisco, USA .
W
Weinrebe, R. W.,
Bohrmann, G.,
Ranero, C.,
Masson, D.,
Huguen, D.,
Sahling, H.,
Hühnerbach, V. and
Klaucke, I.
(2002)
Multiscale high-resolution mapping of the Pacific convergent margin off Costa Rica - first results of the cruise SO-163.
[Talk]
In: AGU Fall Meeting 2002. , 06.- 10.12.2002, San Francisco, USA .
This list was generated on Mon Jan 27 20:49:43 2025 CET.