Lithostratigraphic units in the Drava Depression (Croatian and Hungarian parts) – a correlation / Korelacija litostratigrafskih jedinica u Dravskoj depresiji (hrvatski i mađarski dio) (CROSBI ID 188192)
Prilog u časopisu | izvorni znanstveni rad
Podaci o odgovornosti
Malvić, Tomislav ; Cvetković, Marko
hrvatski
Lithostratigraphic units in the Drava Depression (Croatian and Hungarian parts) – a correlation / Korelacija litostratigrafskih jedinica u Dravskoj depresiji (hrvatski i mađarski dio)
The lithostratigraphic division and correlation is one of the most common stratigraphic divisions. It is strictly connected with lithological content of the rocks or deposits. Sometimes lithostratigraphic units, especially in rank of formations and members, can be approximately correlated with particular chronostratigraphic units in range of stages or sub-stages, i.e. lithosratigraphic units have synchronous borders. In other cases, the borders are asynchronous. Croatian and Hungarian lithostratigraphic units in the Drava Depression are analysed here as well as the possibility of their correlation. Such correlation scheme can be useful in comparison of different units, especially because Croatian part is based on approximately synchronous, and Hungarian on asynchronous borders between units. Moreover, the Drava Depression in this region is an important hydrocarbon production province where lithostratigraphic correlation is widely used, even across state borders. Presented lithostratigraphic scheme, their lithological descriptions and correlation could help in any geological research or evaluation in the entire analysed depression.
litostratigrafska razradba; Dravska depresija; Hrvatska; Mađarska.
nije evidentirano
engleski
Lithostratigraphic units in the Drava Depression (Croatian and Hungarian parts) – a correlation
The lithostratigraphic division and correlation is one of the most common stratigraphic divisions. It is strictly connected with lithological content of the rocks or deposits. Sometimes lithostratigraphic units, especially in rank of formations and members, can be approximately correlated with particular chronostratigraphic units in range of stages or sub-stages, i.e. lithosratigraphic units have synchronous borders. In other cases, the borders are asynchronous. Croatian and Hungarian lithostratigraphic units in the Drava Depression are analysed here as well as the possibility of their correlation. Such correlation scheme can be useful in comparison of different units, especially because Croatian part is based on approximately synchronous, and Hungarian on asynchronous borders between units. Moreover, the Drava Depression in this region is an important hydrocarbon production province where lithostratigraphic correlation is widely used, even across state borders. Presented lithostratigraphic scheme, their lithological descriptions and correlation could help in any geological research or evaluation in the entire analysed depression.
lithostratigraphy; Drava Depression; Croatia; Hungary.
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano