Zobrazeno 1 - 4
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pro vyhledávání: '"Nearshore clastics"'
Nearshore Deposits in the Middle Eocene Clastic Succession in Northern Dalmatia (Dinarides, Croatia)
Autor:
Ljubomir Babić, Jožica Zupanič
Publikováno v:
Geologia Croatica, Vol 51, Iss 2, Pp 175-193 (2010)
The Middle Eocene clastic sliccess ion in the Radovin Syncline isapproximate ly 900 m thick and consists of hemipelag ic and nyschtypedepos its in its lower part, and shallow-marine sediments in itsupper portio n. The upper portion embraces a unit of
Externí odkaz:
https://doaj.org/article/25fad50952c247148df872de991de827
Nearshore Deposits in the Middle Eocene Clastic Succession in Northern Dalmatia (Dinarides, Croatia)
Autor:
Babić, Ljubomir, Zupanič, Jožica
Publikováno v:
Geologia Croatica, Vol 51, Iss 2, Pp 175-193 (2010)
The Middle Eocene clastic sliccess ion in the Radovin Syncline isapproximate ly 900 m thick and consists of hemipelag ic and nyschtypedepos its in its lower part, and shallow-marine sediments in itsupper portio n. The upper portion embraces a unit of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::555d4939b10bf95704808379fb9d29d0
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/285
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/285
Nearshore Deposits in the Middle Eocene Clastic Succession in Northern Dalmatia (Dinarides, Croatia)
Autor:
Lj. Babić, J. Zupanić
Publikováno v:
Geologia Croatica
Volume 51
Issue 2
Volume 51
Issue 2
The Middle Eocene clastic succession in the Radovin Syncline is approximately 900 m thick and consists of hemipelagic and flysch-type deposits in its lower part, and shallow-marine sediments in its upper portion. The upper portion embraces a unit of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______951::ecaa43afd5397528d07662548ac7f702
https://hrcak.srce.hr/file/6404
https://hrcak.srce.hr/file/6404
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