Triassic, Upper Jurassic and upper Lower Cretaceous sedimentary formations were previously studied from the Transylvanian Depression basement, but the presence of lowermost Cretaceous (Berriasian-Valanginian) has not been confirmed paleontologically. The carbonate sequence cored from a borehole drilled in the central part of the Transylvanian Depression yields microfossil assemblages dominated by benthic foraminifera. These new data unequivocally document the presence of characteristic Berriasian-Valanginian taxa in these deposits
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
Tyt. z nagłówka.Art. jest abstr. referatu z konferencji.Bibliogr. s. 81.The objective of the present...
The Upper Jurassic and the Lower Cretaceous deposits of the eastern Rif foreland, which are subdivid...
The borehole 6042 Deleni is among the few wells located in the central part of the Transylvanian Dep...
Within the general succession of the Lower Cretaceous deposits from the Vârciorog-Dobreşti area (Păd...
The paper describes the Upper Jurassic – Lower Cretaceous deposits of the Bihor Unit from Pădurea Cr...
This study refers to some problems regarding the lithological succession, facies and carbonate micro...
Almost black shale filling fissures in the Štramberk Limestone belonging to the Silesian Unit, Outer...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
The Upper Jurassic – Lower Cretaceous limestones from Buila-Vânturariţa massif partly consisting of ...
During the Early Cretaceous a central part of the Carpathian Foreland was situated in the Peri-Tethy...
The Mesozoic limestones of Piatra Craiului Massif were deposited in the Dâmbovicioara sedimentary ar...
Marine Middle Miocene deposits at the top of Gârbova de Sus Formation preserve a particular foramini...
<p>The Transylvanian Nappes belongs to the Central – East – Carpathian Nappes System (the Dacides Me...
This is the first investigation on isolated Early Cretaceous foraminifera fauna from Hungary. The fa...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
Tyt. z nagłówka.Art. jest abstr. referatu z konferencji.Bibliogr. s. 81.The objective of the present...
The Upper Jurassic and the Lower Cretaceous deposits of the eastern Rif foreland, which are subdivid...
The borehole 6042 Deleni is among the few wells located in the central part of the Transylvanian Dep...
Within the general succession of the Lower Cretaceous deposits from the Vârciorog-Dobreşti area (Păd...
The paper describes the Upper Jurassic – Lower Cretaceous deposits of the Bihor Unit from Pădurea Cr...
This study refers to some problems regarding the lithological succession, facies and carbonate micro...
Almost black shale filling fissures in the Štramberk Limestone belonging to the Silesian Unit, Outer...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
The Upper Jurassic – Lower Cretaceous limestones from Buila-Vânturariţa massif partly consisting of ...
During the Early Cretaceous a central part of the Carpathian Foreland was situated in the Peri-Tethy...
The Mesozoic limestones of Piatra Craiului Massif were deposited in the Dâmbovicioara sedimentary ar...
Marine Middle Miocene deposits at the top of Gârbova de Sus Formation preserve a particular foramini...
<p>The Transylvanian Nappes belongs to the Central – East – Carpathian Nappes System (the Dacides Me...
This is the first investigation on isolated Early Cretaceous foraminifera fauna from Hungary. The fa...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
Tyt. z nagłówka.Art. jest abstr. referatu z konferencji.Bibliogr. s. 81.The objective of the present...
The Upper Jurassic and the Lower Cretaceous deposits of the eastern Rif foreland, which are subdivid...