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Displacements and Kinematics of the February 1, 1944 Gerede Earthquake (North Anatolian Fault System, Turkey): Geodetic and Geological Constraints
North Anatolian Fault System Gerede fault zone Gerede earthquake coseismic deformation GPS triangulation
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2010/10/14
The North Anatolian Fault System (NAFS) is an approximately 2-110-km-wide, 1600-km-long right-lateral intra-continental transform fault boundary between the Anatolian platelet and the Eurasian plate. ...
Continuous measurements of atmospheric oxygen and carbon dioxide on a North Sea gas platform
Continuous measurements atmospheric oxygen carbon dioxide North Sea gas platform
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2010/2/8
A new atmospheric measurement station has been established on the North Sea oil and gas production platform F3, 200 km north off the Dutch coast (5°51' N, 4°44' E). Atmospheric concentrations of O2 an...
Partitioning of snowy and rainy precipitation in a case of a north Adriatic frontal passage
snowy rainy north Adriatic frontal passage
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2010/1/27
A case of snow fall in the plains of the Northern Italian region Veneto is presented from a forecasters' perspective. Contrasting forecast guidance came from the ECMWF global model and the limited are...
Landslide susceptibility assessment considering landslide typology. A case study in the area north of Lisbon (Portugal)
Landslide susceptibility assessment landslide typology the area north of Lisbon (Portugal)
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2009/12/9
The aim of the study is to confirm the importance of discriminate different types of slope movements for a better landslide susceptibility evaluation. The study was applied to the sample area of Calha...
Morphotectonic properties of the Lo River Fault near Tam Dao in North Vietnam
Morphotectonic properties the Lo River Fault near Tam Dao North Vietnam
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2009/12/9
The Lo River fault near Tam Dao, North Vietnam, is a young, right-lateral, normal fault which has been active throughout the Quaternary. Rates of dextral slip range between 1 and 2 mm/yr whereas rates...
Investigation of long period crustal deformation on the inactive branch of the North Anatolian Fault Zone
long period crustal deformation inactive branch North Anatolian Fault Zone
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2009/12/8
The western part of North Anatolian Fault (NAF) bifurcates around Mudurnu into two fault segments: northern and southern branch. The latter bifurcates again at west of Pamukova and creates middle stra...
Palaeomagnetic Results from the Sarmatian/Pannonian Boundary in North-Eastern Croatia (Vranovi Section,Našice Quarry)
Palaeomagnetism Palynology Sarmatian Pannonian Central Paratethys Croatia
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2009/12/8
The Sarmatian/Pannonian boundary in the Central Paratethys basin is marked by a major regressive event, which isolated the basin from the open sea and resulted in a palaeoenvironmental change from res...
Variable sources of beach sands of north Adriatic islands:examples from Rab and Susak
beach sands sediment supply framework composition heavy mineral Rab Susak Croatia
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2009/12/7
The composition of beach sands from the Islands of Rab and Susak (northern Adriatic) has been studied in order to determine how individual beaches are supplied with detritus. The beaches on both islan...
The Late Riphean Porsangerhalvøyan tectonometamorphic event in the North Norwegian Caledonides:a comment on nomenclature
tectonometamorphic event North Norwegian Caledonides comment nomenclature
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2009/12/3
A case is presented for replacing the name 'Porsanger' in 'Porsanger orogeny', in the Kalak Nappe Complex of the Finnmark Caledonides, by the adjectival 'Porsangerhalvøyan'.Moreover, until prov...
Geology of a magma transfer zone:the Hortavær Igneous Complex,north-central Norway
Geology magma transfer zone Hortavæ r Igneous Complex north-central Norway
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2009/12/3
The Hortavær intrusive complex consists of a wide range of plutonic rocks, from gabbro (calcic) to alkali feldspar syenite (alkalic). Emplacement at 456 ± 8 Ma (U-Pb, titanite) was primarily as ...
Fluid flow features in fjord-fill deposits,Ullsfjorden,North Norway
Fluid flow features fjord-fill deposits Ullsfjorden
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2009/12/3
Fluid flow features are found with high-resolution acoustic data from Ullsfjorden, North Norway. The glacimarine and marine fjord-fill sediments have a total thickness of up to 150 m. The seafloor is ...
The Larajæg’gi outcrop–a large combined Neoproterozoic/Pleistocene roche moutonnée at Karlebotn,Finnmark,North Norway
Larajæ g’gi outcrop Neoproterozoic/Pleistocene roche moutonnée Karlebotn
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2009/12/3
The gneiss hillocks , which emerge above the Karlebotn quartzite of the Neoproterozoic Smalfjord Formation in the Karlebotn area, North Norway,have been interpreted as primary, uneven basement relief ...
Deep-water sedimentary systems of Arctic and North Atlantic margins:An introduction
Deep-water sedimentary systems Arctic North Atlantic margins
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2009/12/3
The conference "Deep-water sedimentary systems of Arctic and North Atlantic margins" held in Stavanger, Norway from October 18th - 20th 2004 illustrated the wide temporal and spatial variability of Up...
Frequency and triggering mechanisms of submarine landslides of the North Norwegian continental margin
Frequency triggering mechanisms submarine landslides North Norwegian continental margin
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2009/12/3
The frequency of submarine landslides was investigated through the occurrence of sandy turbidites in a 16 m long piston core and a shorter gravity core from the abyssal plain of the Lofoten Basin, Nor...
The number,form and origin of sub-horizontal surfaces in north Ceredigion
number form origin sub-horizontal surfaces north Ceredigion
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2009/12/2
The number, form and origin of a stepped sequence of sub-horizontal surfaces in north Ceredigion, U.K., has been the subject of continuing controversy over nearly two centuries of investigation. Renew...