Results 51 to 60 of about 207,177 (197)

Early–Late Carboniferous Tectonic Evolution of the Northern North China Craton (NE China): Constraints From Zircon Ages, Geochemistry, and Crustal Thickness Modeling

open access: yesGeochemistry, Geophysics, Geosystems, Volume 27, Issue 8, August 2026.
Abstract The tectonic evolution of the northern margin of the North China Craton (NCC) remains controversial. In this study, we obtained zircon U–Pb ages, geochemical data, and Sr–Nd isotopic data for volcanic rocks, and detrital zircon ages for sedimentary rocks from the Yufutun, Tongqigou, and Benxi formations in central‐southern Jilin Province, NE ...
Yunfei Chang   +6 more
wiley   +1 more source

Field excursion guide to the Geology of Fruška Gora (Southern Pannonian Basin, Serbia) [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva
Fruška Gora, a prominent inselberg within the southern margin of the Pannonian Basin, preserves a complex geological record of both orogenic and post‐orogenic processes in the central Balkans.
Kostić Bojan
doaj   +1 more source

The Contribution of Oil Signs to the Petroleum Prospect in the Erindi Region, Albania

open access: yesSmart Cities and Regional Development Journal, 2022
Many wells have been drilled in Albania to search oil traps in the carbonate reservoirs of the Ionian area. One of them is the Nokova-1 well, drilled in the overflow front of the Berati anticline belt.
Enkela NOÇKA   +2 more
doaj   +1 more source

Paleomagnetic Constraints on the Separation of the Olongbuluke Block From the North China Block During the Late Cambrian–Middle Ordovician and Its Tectonic Significance

open access: yesGeophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract The collisional evolution of the micro‐blocks in the northeastern Tibetan Plateau is relatively well constrained. However, the reason why a fragment of the North China Block, the Olongbuluke Block, became separated from North China by the Central Qilian Block (a fragment of the South China Block) remains unclear.
Teng Wang   +4 more
wiley   +1 more source

Kraški rob (landscape term) Geologic section along the motorway Kozina – Koper (Capodistria)

open access: yesGeologija, 2007
Geologic section along the motorway from Kozina to Koper in totality exposed geologic structure of the border belt between Adriatic-Apulian foreland and Dinarides that was formed by subthrusting of Adriatic-Apulian foreland (Istria, Friuli) underneath ...
Ladislav Placer
doaj  

Morfologija šavrinskega gričevja in njegovega obrobja

open access: yesActa Geographica Slovenica, 1956
Greatest part of the NW corner of Istria is composed of the Savrini Hills along rivers Rižana and Rokava (Dragogna). This hilly area, roughly NWof Buzet is built of beds of eocene flysch (sandstones and partly marls) deposited in the form of a syncline (
Vladimir Kokole
doaj   +1 more source

Late Campanian (74–71 Ma) Arabia–Eastern Anatolia Collision and Its Geodynamic Implications

open access: yesTectonics, Volume 45, Issue 7, July 2026.
Abstract The East Anatolian Plateau is a major collisional feature within the Tethyan realm formed as a late‐stage result of the collision between East Anatolia and the Arabian Platform. The timing of this collision is highly debated, with estimates from the Late Cretaceous to the Miocene.
Remziye Akdoğan   +7 more
wiley   +1 more source

A constrained African craton source for the Cenozoic Numidian Flysch: Implications for the palaeogeography of the western Mediterranean basin [PDF]

open access: yes, 2010
The provenance of the Numidian Flysch in the western Mediterranean remains a controversial subject which hinders understanding of this regionally widespread depositional system. The Numidian Flysch is a deep marine formation dated as Oligocene to Miocene
Thomas, M. F H   +7 more
core   +1 more source

Provenance of synorogenic deposits of the Upper Cretaceous–Lower Palaeogene Jarmuta–Proč Formation (Pieniny Klippen Belt, Western Carpathians)

open access: yesGeologica Carpathica, 2019
The Pieniny Klippen Belt contains thickening and coarsening upwards synorogenic sedimentary successions witnessing the collision of the Oravic ribbon continent with the Central Carpathian orogenic wedge after the closure of the Vahic Ocean in the Late ...
Madzin Jozef   +2 more
doaj   +1 more source

Tectonic evolution and high-pressure rock exhumation in the Qiangtang terrane, central Tibet [PDF]

open access: yesSolid Earth, 2015
Conflicting interpretations of the > 500 km long, east–west-trending Qiangtang metamorphic belt have led to very different and contradicting models for the Permo–Triassic tectonic evolution of central Tibet.
Z. Zhao   +4 more
doaj   +1 more source

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