Platform-basin transitions and their role in Alpine-style collision systems : a comparative approach [PDF]
CB acknowledges financial support from Optimus (Aberdeen) ltd. Petroceltic International plc are thanked for providing access to the subsurface data used in this study and for permission to publish images used here. Schlumberger are thanked for providing
Bell, Cameron, Butler, Robert W. H.
core +2 more sources
The Buzet Thrust Fault in Istria and overturned carbonate megabeds in
Detailed geological mapping undertaken in the framework of monitoring of the motorway construction works in SW Slovenia has revealed the existence of a large-scale thrust fault between Buzet and Koper (termed the Buzet Thrust Fault) and extensive thrust ...
Ladislav Placer +4 more
doaj
The serpulid worm Rotularia spirulaea from Eocene beds near Gračišće in Istria, Croatia
In paper several selected specimens of sedentary Polychaetes of species Rotularia spirulaea (Lamarck, 1818) are presented. They were found in Middel Eocene – Lutetian calcareous breccias and conglomerates, respectively olistostromes,below the village of ...
Vasja Mikuž
doaj
Land use changes in the area of Movraški Kras and adjacent flysch areas between 1830 and 2008
Agricultural landscape, as a result of human interference and management, has drastically changed in the last 180 years within the area. The process of land abandonment is the most evident, along with overgrowing of grasslands, field fragmentation and ...
Danijel Ivajnšič +2 more
doaj +1 more source
Cretaceous (Aptian/Albian-?Cenomanian) age of "black flysch" and adjacent deposits of the Grajcarek thrust-sheets in the Małe Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians) [PDF]
Several sections record the relation between the "black flysch" and Upper Cretaceous red shales in the Grajcarek thrust-sheets. In all the sections studied the "black flysch" appears in the core of imbricated folds or thrust-sheets, whereas the limbs are
Malata, Ewa +2 more
core +1 more source
Erosion and deposition in interplain channels of the Maury channel system [PDF]
Large turbidity currents originating on the insular margin of southern lceland have flowed clown a 2 500 km-long pathway comprising rise valleys, unchanneled plains and segments of erosional and depositional deep-sea channels that are collectively called
Hollister, C. D. +2 more
core +1 more source
Geological structure and evolution of the Pieniny Klippen Belt to the east of the Dunajec River : a new approach (Western Outer Carpathians, Poland) [PDF]
The area studied, known as the Małe (Little) Pieniny Mts., belongs to the Pieniny Klippen Belt (PKB), a suture zone that separates the Central Carpathians from the Outer Carpathian accretionary wedge. Along its northern boundary the PKB is separated from
Oszczypko, Nestor +1 more
core +1 more source
Late Miocene – Early Pleistocene paleogeography of the onshore central Hawke’s Bay sector of the forearc basin, eastern North Island, New Zealand, and some implications for hydrocarbon prospectivity [PDF]
The timing of trap formation in relation to the timing of source rock burial and maturation are important considerations in evaluating the hydrocarbon prospectivity of onshore parts of the forearc basin in central Hawke’s Bay.
Bland, Kyle J. +2 more
core
Neogene stratigraphic architecture and tectonic evolution of Wanganui, King Country, and eastern Taranaki Basins, New Zealand [PDF]
Analysis of the stratigraphic architecture of the fills of Wanganui, King Country, and eastern Taranaki Basins reveals the occurrence of five 2nd order Late Paleocene and Neogene sequences of tectonic origin.
Bland, Kyle J. +9 more
core +2 more sources
Performance of Ground Anchors Built in a Flysch Deposit
AbstractThe ultimate pull-out tensile load of ground anchors is strongly dependent onsoil nature,grout injection and effective stress state around the bulb. In this paper, the comparison between the results of conventional pull-out testson instrumented anchors built in a flysch formation and those of small scale pull-out tests performed in the ...
Di Gregorio, M. C. . +5 more
openaire +3 more sources

