Zobrazeno 1 - 7
of 7
pro vyhledávání: '"messinian unconformity"'
Autor:
Ivica Vulama
Publikováno v:
Geologia Croatica, Vol 50, Iss 1, Pp 89-103 (2010)
The Pliocene source rocks of the Middle Adriatic ridge appeared to be thermally immature, according to the geophysical and the geochemicalanalyses, but they may have produced biogene gas. Wireline logging confirmed their broad extent. Correlation bet
Externí odkaz:
https://doaj.org/article/c9f430e7392c4acfa1a3126635bb7c29
This study focuses on the so-called Pa(n)-4 sequence boundary or intra-Messinian unconformity and its appearance in the Drava Trough. A surface with similar geometric relations, i.e. folded/tilted lacustrine beds overlain by onlaps, can be observed i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::8b8e19cb997c110716e47e8bcc67db33
https://www.bib.irb.hr/1057148
https://www.bib.irb.hr/1057148
Autor:
Ivica Vulama
Publikováno v:
Geologia Croatica
Volume 50
Issue 1
Geologia Croatica, Vol 50, Iss 1, Pp 89-103 (2010)
Volume 50
Issue 1
Geologia Croatica, Vol 50, Iss 1, Pp 89-103 (2010)
The Pliocene source rocks of the Middle Adriatic ridge appearedto be thermally immature, according to the geophysical and the geochemicalanalyses, but they may have produced biogene gas. Wirelinelogging confirmed their broad extent. Correlation betwe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::85ba2bc79dd7a57ad3f8af8a07a1d1d6
https://hrcak.srce.hr/file/25435
https://hrcak.srce.hr/file/25435
Numerous seismic lines allow {he identification of a deep and long erosive canyon incised during the Messinian on shelfal and basinal deposits of Upper Tortonian and Messinian s.s. age. Reconstructions of the pre-erosional sedimentary architecture an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::4ee371e39e32da9f1f7e14abbad6c192
https://hdl.handle.net/10272/18111
https://hdl.handle.net/10272/18111
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Numerous seismic lines allow {he identification of a deep and long erosive canyon incised during the Messinian on shelfal and basinal deposits of Upper Tortonian and Messinian s.s. age. Reconstructions of the pre-erosional sedimentary architecture an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::4ee371e39e32da9f1f7e14abbad6c192
http://hdl.handle.net/10272/18111
http://hdl.handle.net/10272/18111
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