Results 41 to 50 of about 193,636 (174)
The effect of positive reinforcement on adolescent seat belt use [PDF]
, 2002 Plan BSeveral different programs nationwide have attempted to increase seat belt use among young drivers. Programs producing increased seat belt use characteristically have strong student involvement, incentives, and educational components.
Kirby, Kevin W.
core
Field excursion guide to the Geology of Fruška Gora (Southern Pannonian Basin, Serbia) [PDF]
Geološki Anali Balkanskoga PoluostrvaFruška 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
Smart 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
Late Campanian (74–71 Ma) Arabia–Eastern Anatolia Collision and Its Geodynamic Implications
Tectonics, 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
Mélange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview
, 2022 The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous–Miocene folding, thrusting and uplifting.
Włodzimierz Jerzy Mościcki +8 more
core +1 more source
Morfologija šavrinskega gričevja in njegovega obrobja
Acta 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
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Tectonics, Volume 45, Issue 6, June 2026.Abstract While the evolution of individual passive marginal and foreland basins is well understood, the subsidence pattern of passive margins near convergence zones—where thrust loading overprints earlier extension and the typical wedge and foredeep are obscured—remains poorly understood.
Penggao Fang +3 more
wiley +1 more source
Kraški rob (landscape term) Geologic section along the motorway Kozina – Koper (Capodistria)
Geologija, 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
Geologica 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]
Solid 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