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Autor:
Ingo Grevemeyer, Timothy J. Henstock, Anke Dannowski, Milena Marjanovic, Helene-Sophie Hilbert, Yuhan Li, Daman A. H. Teagle
Our view on the structure of oceanic crust is largely based the interpretation of seismic refraction and wide-angle experiments, revealing that the upper basaltic crust (layer 2) is a region of strong velocity gradients. In contrast, the lower gabbro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36b83301a0ec1b90ba11ba046138d243
https://doi.org/10.5194/egusphere-egu23-4289
https://doi.org/10.5194/egusphere-egu23-4289