[HTML][HTML] Detrital zircon U–Pb age analysis of last glacial loess sources and proglacial sediment dynamics in the Northern European Plain
Loess deposits along the northern fringe of the European loess belt potentially record past
changes in dust emission from areas proximal to former ice sheets. Recent chronologies …
changes in dust emission from areas proximal to former ice sheets. Recent chronologies …
[HTML][HTML] Eurasian Ice Sheet derived meltwater pulses and their role in driving atmospheric dust activity: Late Quaternary loess sources in SE England
The role of Quaternary ice sheet fluctuations in driving meltwater pulses and ocean
circulation perturbations is widely acknowledged. What is less clear is the role of these …
circulation perturbations is widely acknowledged. What is less clear is the role of these …
A non‐collisional, accretionary Sveconorwegian orogen
T Slagstad, NMW Roberts, M Marker, TS Røhr… - Terra …, 2013 - Wiley Online Library
Terra Nova, 25, 30–37, 2013 Abstract The late Mesoproterozoic Sveconorwegian orogen in
southwest Baltica is traditionally interpreted as the eastward continuation of the Grenville …
southwest Baltica is traditionally interpreted as the eastward continuation of the Grenville …
Circum-Arctic Lithosphere Evolution (CALE) Transect C: displacement of the Arctic Alaska–Chukotka microplate towards the Pacific during opening of the Amerasia …
This paper synthesizes the framework and geological evolution of the Arctic Alaska–
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Provenance of Triassic sandstones on the southwest Barents Shelf and the implication for sediment dispersal patterns in northwest Pangaea
EJ Fleming, MJ Flowerdew, HR Smyth, RA Scott… - Marine and Petroleum …, 2016 - Elsevier
Thick Triassic siliciclastic units form major reservoir targets for hydrocarbon exploration on
the Barents Shelf; however, poor reservoir quality, possibly associated with variation in …
the Barents Shelf; however, poor reservoir quality, possibly associated with variation in …
Neoproterozoic recycling of the Sveconorwegian orogenic belt: Detrital-zircon data from the Sparagmite basins in the Scandinavian Caledonides
Arkose-dominated sequences exposed in the Lower and Middle Allochthons of the
Scandinavian Caledonides, known as the Sparagmites, are the product of sedimentation …
Scandinavian Caledonides, known as the Sparagmites, are the product of sedimentation …
A pericratonic model for the Pearya terrane as an extension of the Franklinian margin of Laurentia, Canadian Arctic
T Hadlari, WJ Davis, K Dewing - Bulletin, 2014 - pubs.geoscienceworld.org
New detrital zircon sensitive high-resolution ion microprobe (SHRIMP) geochronology and
published framework geology of Neoproterozoic to Silurian strata are integrated to …
published framework geology of Neoproterozoic to Silurian strata are integrated to …
207Pb/206Pb ages and Hf isotope composition of zircons from sedimentary rocks of the Ukrainian shield: crustal growth of the south-western part of East European …
The results of simultaneous LA-ICP-MS measurements of 207 Pb/206 Pb and Hf isotope
ratios are reported for zircons separated from five Ukrainian shield sedimentary rocks:(1) c …
ratios are reported for zircons separated from five Ukrainian shield sedimentary rocks:(1) c …
Segmentation of the Caledonian orogenic infrastructure and exhumation of the Western Gneiss Region during transtensional collapse
The (ultra) high-pressure Western Gneiss Region of the Norwegian Caledonides represents
an archetypical orogenic infrastructure of a continent–continent collision zone. To test …
an archetypical orogenic infrastructure of a continent–continent collision zone. To test …
Does continental crust transform during eclogite facies metamorphism?
DJ Young, ARC Kylander‐Clark - Journal of Metamorphic …, 2015 - Wiley Online Library
Eclogites within exhumed continental collision zones indicate regional burial to depths of at
least 60 km, and often more than 100 km in the coesite‐stable, ultra‐high pressure (UHP) …
least 60 km, and often more than 100 km in the coesite‐stable, ultra‐high pressure (UHP) …