Margin architecture and seismic attenuation in the central Costa Rican forearc

Autor: Zhu, J., Kopp, H., Papenberg, C., Klaeschen, D., Flueh, E.R., Planert, L.

Publikováno v: In Marine Geology 2010 276(1):30-41

Structure of the Makran subduction zone from wide-angle and reflection seismic data

Autor: Kopp, C. ^*, Fruehn, J., Flueh, E.R., Reichert, C., Kukowski, N., Bialas, J., Klaeschen, D.

Publikováno v: In Tectonophysics 2000 329(1):171-191

Seismic tomography with local earthquakes in Costa Rica

Autor: Sallarès, V. ^*, Dañobeitia, J.J., Flueh, E.R.

Publikováno v: In Tectonophysics 2000 329(1):61-78

Rupture and accretion of the Celebes Sea crustrelated to the North–Sulawesi subduction: combinedinterpretation of reflection and refraction seismicmeasurements

Autor: Kopp, C. ^{1, *}, Flueh, E.R. ¹, Neben, S. ²

Publikováno v: In Journal of Geodynamics 25 February 1999 27(3):309-325

Deep structure of the central Lesser Antilles Island Arc: Relevance for the formation of continental crust

Autor: Kopp, H., Weinzierl, W., Becel, A., Charvis, P., Evain, M., Flueh, E.R., Gailler, A., Galve, A., Hirn, A., Kandilarov, A., Klaeschen, D., Laigle, M., Papenberg, C., Planert, L., Roux, E., Thales And Trail, Teams

Publikováno v: Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2011, 304 (1-2), pp.121-134. ⟨10.1016/j.epsl.2011.01.024⟩
Earth and Planetary Science Letters, 2011, 304 (1-2), pp.121-134. ⟨10.1016/j.epsl.2011.01.024⟩

Oceanic island arcs are sites of high magma production and contribute to the formation of continental crust. Geophysical studies may provide information on the configuration and composition of island arc crust, however, to date only few seismic profi

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