The eastern part of the Drava depression is an area with extensive source rock distribution in the Miocene formation. Source rock maturity has been determined from the formation resistivity. The formation resistivity of 32 Ohm*m is typical of the area and it represents the threshold value between immature and mature source rocks. The data has been correlated with existing geochemical analyses. Additional research has been undertaken at other localities (parts of the Drava and Sava depression and Middle Adriatic ridge). Various cross plots which have been obtained are useful for source rock determination from well logs, in very different p/T conditions and the lithologies which are characteristic for source rocks in Croatia
This article closely defines the stratigraphic-structural relations within the eastern part of the D...
Coastal parts of Croatia are dominated by the SW-verging Dinaric foldbelt, to the west and SW of whi...
The source of the clastic sediments in the Croatian part of the Pannonian Basin System (CPBS) during...
The eastern part of the Drava depression is an area with extensive source rock distribution in the M...
A Middle Miocene oil source rock has been identified by geochemicallogging of exploration wells in t...
The Sava Depression lies at the very south-western margin of the Pannonian Basin. There are 20 hydro...
The Pliocene source rocks of the Middle Adriatic ridge appeared to be thermally immature, according ...
Oil and gas in the eastern part of the Drava depression originated from source rocks of very good ge...
Neogene depositional environments in the Drava depression can be classified in two groups. One group...
Small possible hydrocarbon gas reservoirs were analysed in the Bjelovar Subdepression in Northern Cr...
Small possible hydrocarbon gas reservoirs were analysed in the Bjelovar Subdepression in Northern Cr...
A Middle Miocene oil source rock has been identified by geochemicallogging of exploration wells in t...
The eastern part of Sava Depression is bounded on the south with the Sava River and on the north wit...
AbstractFifty-two samples of Miocene pelitic sedimentary rock from outcrops on Medvednica, Moslavačk...
This article closely defines the stratigraphic-structural relations within the eastern part of the D...
This article closely defines the stratigraphic-structural relations within the eastern part of the D...
Coastal parts of Croatia are dominated by the SW-verging Dinaric foldbelt, to the west and SW of whi...
The source of the clastic sediments in the Croatian part of the Pannonian Basin System (CPBS) during...
The eastern part of the Drava depression is an area with extensive source rock distribution in the M...
A Middle Miocene oil source rock has been identified by geochemicallogging of exploration wells in t...
The Sava Depression lies at the very south-western margin of the Pannonian Basin. There are 20 hydro...
The Pliocene source rocks of the Middle Adriatic ridge appeared to be thermally immature, according ...
Oil and gas in the eastern part of the Drava depression originated from source rocks of very good ge...
Neogene depositional environments in the Drava depression can be classified in two groups. One group...
Small possible hydrocarbon gas reservoirs were analysed in the Bjelovar Subdepression in Northern Cr...
Small possible hydrocarbon gas reservoirs were analysed in the Bjelovar Subdepression in Northern Cr...
A Middle Miocene oil source rock has been identified by geochemicallogging of exploration wells in t...
The eastern part of Sava Depression is bounded on the south with the Sava River and on the north wit...
AbstractFifty-two samples of Miocene pelitic sedimentary rock from outcrops on Medvednica, Moslavačk...
This article closely defines the stratigraphic-structural relations within the eastern part of the D...
This article closely defines the stratigraphic-structural relations within the eastern part of the D...
Coastal parts of Croatia are dominated by the SW-verging Dinaric foldbelt, to the west and SW of whi...
The source of the clastic sediments in the Croatian part of the Pannonian Basin System (CPBS) during...