Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Automatic calcimeter"'
Thickness and (%) CaCO3 contents in the marl-limestone couplets of the Danian (Sopelana, Basque Arc)
Autor:
Domínguez, E., Echeberria, J., Gómez Urtasun, I., Ibisate, Ruth, Martínez García, Blanca, Elorza, Javier
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Sopelana sea-cliff section exposes, a continuous marl-limestone alternation from the Danes in the deep Basque Arc domain. The 95 rhythms studied represent ~1180 ka and correspond to ~20cm/20ka. The limestone layers are thicker than marls and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::2a51348849a3a7f3ec29d55b83759880
http://hdl.handle.net/10272/8467
http://hdl.handle.net/10272/8467
Autor:
Domínguez, E., Echeberria, J., Gómez Urtasun, I., Ibisate, Ruth, Martínez García, Blanca, Elorza, Javier
The Sopelana sea-cliff section exposes, a continuous marl-limestone alternation from the Danes in the deep Basque Arc domain. The 95 rhythms studied represent ~1180 ka and correspond to ~20cm/20ka. The limestone layers are thicker than marls and the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::2a51348849a3a7f3ec29d55b83759880
https://hdl.handle.net/10272/8467
https://hdl.handle.net/10272/8467
Autor:
Baguer, A., Martínez López de Sabando, M., Múgica, J., Pérez García, J. R., Unanue, L., Elorza, Javier, Álvarez Llano, Irantzu
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Sopelana sea-cliff section exposes, in very good conditions, a continuous marl-limestone alternation from the Lower Maastrichtian in the deep Basque Arc domain. The 55 rhythms studied represent ~1100 ka and correspond to ~60cm/20ka. The marls are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::e4fb05439443261d04c8fb2638d56149
http://hdl.handle.net/10272/8684
http://hdl.handle.net/10272/8684
Autor:
Baguer, A., Martínez López de Sabando, M., Múgica, J., Pérez García, J. R., Unanue, L., Elorza, Javier, Álvarez Llano, Irantzu
The Sopelana sea-cliff section exposes, in very good conditions, a continuous marl-limestone alternation from the Lower Maastrichtian in the deep Basque Arc domain. The 55 rhythms studied represent ~1100 ka and correspond to ~60cm/20ka. The marls are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::e4fb05439443261d04c8fb2638d56149