Chapter 61 The Neoproterozoic glaciogenic Lillfjället Formation, southern Swedish Caledonides
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- Type
- article
- Published
- 2011-01-01
- Cited by
- 17
- References
- 37
- OpenAlex
- https://openalex.org/W2005480363
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129581098
Keywords
Geology, Paleontology, Archaeology, Geography
References
- Neoproterozoic basin evolution in Fennoscandia, East Greenland and Svalbard
- Earth's pre-Pleistocene glacial record
- A probable glaciogenic sediment in the Särv Nappe, central Swedish Caledonides
- Attempted break-up of Rodinia at 850 Ma: geochronological evidence from the Seve–Kalak Superterrane, Scandinavian Caledonides
- The Dalradian of Scotland: missing link between the Vendian of northern and southern Scandinavia?
- Strain softening induced ductile flow in the Särv thrust sheet, Scandinavian Caledonides
- Om diabasen på Ottfjället i Jemtland
- Onset of seafloor spreading in the Iapetus Ocean at 608 Ma: precise age of the Sarek Dyke Swarm, northern Swedish Caledonides
- Upper Proterozoic stratigraphy and depositional environments of the Tossåsfjället Group, Särv Nappe, southern Swedish Caledonides
- 40Ar/39Ar data on the age and metamorphism of the Ottfjället dolerites, Särv Nappe, Swedish Caledonides
- The Periglacial Environment
- Baltica upside down: A new plate tectonic model for Rodinia and the Iapetus Ocean
- Sand-wedge polygons (tesselations) in the McMurdo Sound region, Antarctica; a progress report
- Chapter 59 Neoproterozoic glaciation of South Norway: from continental interior to rift and pericratonic basins in western Baltica
- Geochemical signature of the Egersund basaltic dyke swarm, SW Norway, in the context of late-Neoproterozoic opening of the Iapetus Ocean
- Caledonian nappe geometry in north-central Sweden and basin evolution on the Baltoscandian margin
- Was Baltica right-way-up or upside-down in the Neoproterozoic?
- Chapter 60 Evidence for late Neoproterozoic glaciation in the central Scandinavian Caledonides
- Chapter 58 Evidence of late Neoproterozoic glaciation in the Caledonides of NW Scandinavia
- [Part I Introduction]
Cited by
- Periglacial paleosols and Cryogenian paleoclimate near Adelaide, South Australia
- The Baltoscandian margin detrital zircon signatures of the central Scandes
- Detrital zircon signatures of the Baltoscandian margin along the Arctic Circle Caledonides in Sweden: The Sveconorwegian connection
- Pressure–temperature evolution of a kyanite–garnet pelitic gneiss from Åreskutan: evidence of ultra-high-pressure metamorphism of the Seve Nappe Complex, west-central Jämtland, Swedish Caledonides
- The Sub-Cambrian Peneplain in southern Norway: its geological significance and its implications for post-Caledonian faulting, uplift and denudation
- Baltoscandian margin, Sveconorwegian crust lost by subduction during Caledonian collisional orogeny
- The Metamorphic History ofthe Helags Mountain Area,Scandinavian Caledonides
- Nappe units along the Caledonian margin in central Scandinavia (Grong–Olden to Nasafjället): definition, distinction criteria and tectonic evolution
- New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age
- Late Neoproterozoic basin evolution of the magma rich Iapetus margin of Baltica
- Timing of deformation, metamorphism and leucogranite intrusion in the lower part of the Seve Nappe Complex in central Jämtland, Swedish Caledonides
- U-Pb baddeleyite age for the Ottfjället Dyke Swarm, central Scandinavian Caledonides: new constraints on Ediacaran opening of the Iapetus Ocean and glaciations on Baltica
- Towards a glacial subdivision of the Ediacaran Period, with an example of the Boston Bay Group, Massachusetts
- U-Pb baddeleyite age for the Ottfjället Dyke Swarm, central Scandinavian Caledonides: New constraints on Ediacaran opening of the Iapetus Ocean and glaciations on Baltica – a comment on the inferred age of Neoproterozoic glaciations
- Neoproterozoic Snowball Earth Extent Inferred From Paleosols In California
- Life through an Ediacaran glaciation: Shale- and diamictite-hosted organic-walled microfossil assemblages from the late Neoproterozoic of the Tanafjorden area, northern Norway
- eriglacial paleosols and Cryogenian paleoclimate near Adelaide , outh Australia
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