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pro vyhledávání: '"Sistema Bético"'
Autor:
Barcos Murcia, Leticia
Programa de Doctorado en Estudios Medioambientales
Transpressive high-strain zones are common features in the lateral parts of orogenic arcs where oblique convergence usually occurs. The strain within these zones is highly partitioned when they
Transpressive high-strain zones are common features in the lateral parts of orogenic arcs where oblique convergence usually occurs. The strain within these zones is highly partitioned when they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3034::3b3fa0373b1c7e54ae00eefd7656f895
https://hdl.handle.net/10433/2139
https://hdl.handle.net/10433/2139
Autor:
Barcos Murcia, Leticia
Publikováno v:
RIO: Repositorio Institucional Olavide
Universidad Pablo de Olavide (UPO)
RIO. Repositorio Institucional Olavide
instname
Universidad Pablo de Olavide (UPO)
RIO. Repositorio Institucional Olavide
instname
Programa de Doctorado en Estudios Medioambientales Transpressive high-strain zones are common features in the lateral parts of orogenic arcs where oblique convergence usually occurs. The strain within these zones is highly partitioned when they are l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3b3fa0373b1c7e54ae00eefd7656f895
http://hdl.handle.net/10433/2139
http://hdl.handle.net/10433/2139