Structure of the crust and upper mantle beneath the Bransfield Strait (Antarctica) using P receiver functions

The Bransfield Strait is a tectonically active region of the Antarctic Ocean comprising the waters located between the South Shetland archipelago and the Antarctic Peninsula. Nowadays the Bransfield region is characterised by the presence of an incipient oceanic spreading ridge possibly driven by on...

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Bibliographic Details
Main Author: Parera Portell, Joan Antoni
Other Authors: Mancilla Pérez, Flor de Lis, Morales Soto, José, Universidad de Granada. Departamento de Física Teórica y del Cosmos, Universidad de Granada. Instituto Andaluz de Geofísica
Format: Master Thesis
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10481/57464
https://doi.org/10.30827/Digibug.57464