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Ordovician sedimentation and basin development in the North Armorican Massif, NW France: Field evidence from the northern Cotentin Peninsula
by
Went, David J.
in
Armorican Massif
/ biogenic structures
/ Cambrian
/ clastic rocks
/ Continental margins
/ Cotentin Peninsula
/ Dapingian
/ Darriwilian
/ Europe
/ Fault lines
/ Fossils
/ France
/ Geology
/ Gres Armoricain Formation
/ Gres de May Formation
/ Gres de Moitiers d'Allonne Formation
/ hummocky cross-stratification
/ La Hague France
/ lebensspuren
/ lithofacies
/ Manche France
/ marine environment
/ Massifs
/ Metamorphism
/ Middle Ordovician
/ mudstone
/ Ocean basins
/ Ocean engineering
/ Oceans
/ Offshore
/ Ordovician
/ Original Article
/ paleogeography
/ Paleozoic
/ planar bedding structures
/ Regional analysis
/ Regional planning
/ Sandstone
/ Schistes d'Urville Formation
/ Schistes de Beaumont Formation
/ Sedimentary facies
/ Sedimentary rocks
/ sedimentary structures
/ Sedimentation & deposition
/ sedimentology
/ shale
/ shallow-water environment
/ shelf environment
/ storm environment
/ Strata
/ Stratification
/ Stratigraphy
/ Subsidence
/ unconformities
/ Unconformity
/ Uplift
/ Western Europe
2023
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Ordovician sedimentation and basin development in the North Armorican Massif, NW France: Field evidence from the northern Cotentin Peninsula
by
Went, David J.
in
Armorican Massif
/ biogenic structures
/ Cambrian
/ clastic rocks
/ Continental margins
/ Cotentin Peninsula
/ Dapingian
/ Darriwilian
/ Europe
/ Fault lines
/ Fossils
/ France
/ Geology
/ Gres Armoricain Formation
/ Gres de May Formation
/ Gres de Moitiers d'Allonne Formation
/ hummocky cross-stratification
/ La Hague France
/ lebensspuren
/ lithofacies
/ Manche France
/ marine environment
/ Massifs
/ Metamorphism
/ Middle Ordovician
/ mudstone
/ Ocean basins
/ Ocean engineering
/ Oceans
/ Offshore
/ Ordovician
/ Original Article
/ paleogeography
/ Paleozoic
/ planar bedding structures
/ Regional analysis
/ Regional planning
/ Sandstone
/ Schistes d'Urville Formation
/ Schistes de Beaumont Formation
/ Sedimentary facies
/ Sedimentary rocks
/ sedimentary structures
/ Sedimentation & deposition
/ sedimentology
/ shale
/ shallow-water environment
/ shelf environment
/ storm environment
/ Strata
/ Stratification
/ Stratigraphy
/ Subsidence
/ unconformities
/ Unconformity
/ Uplift
/ Western Europe
2023
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Ordovician sedimentation and basin development in the North Armorican Massif, NW France: Field evidence from the northern Cotentin Peninsula
by
Went, David J.
in
Armorican Massif
/ biogenic structures
/ Cambrian
/ clastic rocks
/ Continental margins
/ Cotentin Peninsula
/ Dapingian
/ Darriwilian
/ Europe
/ Fault lines
/ Fossils
/ France
/ Geology
/ Gres Armoricain Formation
/ Gres de May Formation
/ Gres de Moitiers d'Allonne Formation
/ hummocky cross-stratification
/ La Hague France
/ lebensspuren
/ lithofacies
/ Manche France
/ marine environment
/ Massifs
/ Metamorphism
/ Middle Ordovician
/ mudstone
/ Ocean basins
/ Ocean engineering
/ Oceans
/ Offshore
/ Ordovician
/ Original Article
/ paleogeography
/ Paleozoic
/ planar bedding structures
/ Regional analysis
/ Regional planning
/ Sandstone
/ Schistes d'Urville Formation
/ Schistes de Beaumont Formation
/ Sedimentary facies
/ Sedimentary rocks
/ sedimentary structures
/ Sedimentation & deposition
/ sedimentology
/ shale
/ shallow-water environment
/ shelf environment
/ storm environment
/ Strata
/ Stratification
/ Stratigraphy
/ Subsidence
/ unconformities
/ Unconformity
/ Uplift
/ Western Europe
2023
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Ordovician sedimentation and basin development in the North Armorican Massif, NW France: Field evidence from the northern Cotentin Peninsula
Journal Article
Ordovician sedimentation and basin development in the North Armorican Massif, NW France: Field evidence from the northern Cotentin Peninsula
2023
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Overview
Field evidence from the northern Cotentin Peninsula and regional data are used to construct a tectono-stratigraphic model for the Ordovician which characterizes basin development in the North Armorican Massif. In La Hague, 15 m of transgressive marine sandstone belongs to the Dapingian age Grès Armoricain Formation which onlaps lower Cambrian, rift-fill deposits via an unconformity. Approximately 450 m of overlying Darriwilian strata are dominated by shallow marine sandstone showing hummocky cross-stratification with subordinate shales containing trace and body fossils. Together, these facies support an interpretation of offshore shallow marine strata overlying a break-up unconformity. Regional analysis indicates the time gap at the unconformity is 20–40 Ma and formed from crustal upwarping, which was greatest in the north of the Armorican Massif. Dapingian strata (Grès Armoricain) thins irregularly to the north (0–94 m), interpreted to reflect passive onlap onto residual relief associated with the uplift and the initiation of thermal subsidence on the margin. The succeeding Darriwilian strata (Schistes de Beaumont to Grès de May) conversely display a steady thickening (161–623 m) to the north, the stratal patterns suggesting that from the Darriwilian onwards, the ocean basin to the north was firmly established as the main locus of subsidence on the continental margin.
Publisher
Cambridge University Press
Subject
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