Update search
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Reguibat Ridge (1)
-
West Africa
-
Mauritania (1)
-
-
-
Atlantic Ocean
-
North Atlantic
-
English Channel (5)
-
Gulf of Saint Lawrence (1)
-
Northwest Atlantic (1)
-
-
-
Avalon Zone (1)
-
Canada
-
Eastern Canada
-
Newfoundland and Labrador
-
Newfoundland
-
Avalon Peninsula (2)
-
-
-
-
-
Europe
-
Southern Europe
-
Iberian Peninsula
-
Spain (1)
-
-
-
Western Europe
-
France
-
Armorican Massif (1)
-
Brittany (4)
-
Loire River (1)
-
Normandy (2)
-
-
Iceland (1)
-
United Kingdom
-
English Channel Islands
-
Jersey (1)
-
-
Great Britain
-
England (1)
-
-
-
-
-
Grand Banks (1)
-
North America
-
Appalachians
-
Northern Appalachians (1)
-
Southern Appalachians (1)
-
-
-
-
fossils
-
Invertebrata
-
Mollusca (2)
-
-
microfossils (1)
-
palynomorphs (1)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Holocene (1)
-
Pleistocene
-
upper Pleistocene (1)
-
-
-
-
Paleozoic
-
Carboniferous (1)
-
-
Precambrian
-
upper Precambrian
-
Proterozoic (1)
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks
-
basalts (1)
-
-
-
ophiolite (1)
-
-
metamorphic rocks
-
ophiolite (1)
-
-
minerals
-
silicates
-
framework silicates
-
silica minerals
-
quartz (1)
-
-
-
-
-
Primary terms
-
Africa
-
Reguibat Ridge (1)
-
West Africa
-
Mauritania (1)
-
-
-
Atlantic Ocean
-
North Atlantic
-
English Channel (5)
-
Gulf of Saint Lawrence (1)
-
Northwest Atlantic (1)
-
-
-
Canada
-
Eastern Canada
-
Newfoundland and Labrador
-
Newfoundland
-
Avalon Peninsula (2)
-
-
-
-
-
Cenozoic
-
Quaternary
-
Holocene (1)
-
Pleistocene
-
upper Pleistocene (1)
-
-
-
-
continental shelf (1)
-
crust (1)
-
diagenesis (1)
-
earthquakes (1)
-
Europe
-
Southern Europe
-
Iberian Peninsula
-
Spain (1)
-
-
-
Western Europe
-
France
-
Armorican Massif (1)
-
Brittany (4)
-
Loire River (1)
-
Normandy (2)
-
-
Iceland (1)
-
United Kingdom
-
English Channel Islands
-
Jersey (1)
-
-
Great Britain
-
England (1)
-
-
-
-
-
faults (1)
-
geophysical methods (4)
-
igneous rocks
-
plutonic rocks
-
ultramafics (1)
-
-
volcanic rocks
-
basalts (1)
-
-
-
Invertebrata
-
Mollusca (2)
-
-
metamorphism (1)
-
North America
-
Appalachians
-
Northern Appalachians (1)
-
Southern Appalachians (1)
-
-
-
orogeny (3)
-
paleoclimatology (1)
-
paleogeography (1)
-
Paleozoic
-
Carboniferous (1)
-
-
palynomorphs (1)
-
plate tectonics (3)
-
Precambrian
-
upper Precambrian
-
Proterozoic (1)
-
-
-
sea-level changes (2)
-
sedimentary rocks
-
carbonate rocks
-
beachrock (1)
-
-
clastic rocks
-
conglomerate (3)
-
-
-
sediments
-
clastic sediments
-
boulders (2)
-
gravel (1)
-
loess (4)
-
outwash (1)
-
-
-
seismology (1)
-
structural geology (3)
-
tectonics (3)
-
tectonophysics (2)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
beachrock (1)
-
-
clastic rocks
-
conglomerate (3)
-
-
-
-
sediments
-
sediments
-
clastic sediments
-
boulders (2)
-
gravel (1)
-
loess (4)
-
outwash (1)
-
-
-
GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
Study of key structures associated with the indentation of the Southern Urals by the East European Craton: kinematics and age of the final impingement Open Access
Transit boosting of trans-Channel katabatic winds by depressions associated with the west European storms tracks: impact on Pleistocene loess deposits Available to Purchase
Did an earthquake located off Jersey trigger a mudflow preserving the only loess outcrop known under the seas? Available to Purchase
Transport of Late Pleistocene loess particles by katabatic winds during the lowstands of the English Channel Available to Purchase
The contribution of malacology in dating the Pleistocene submarine levels of the English Channel Available to Purchase
Mise en evidence de chevauchements cadomiens sur le profil sismique SWAT N. 10 leve en Manche Available to Purchase
Mise en evidence d'une virgation carbonifere induite par la dorsale Reguibat (Mauritanie) dans les Appalaches du Sud (U.S.A.); arguments geophysiques Available to Purchase
A new geophysical criterion to correlate the Acadian and Hercynian orogenies of western Europe and eastern America Available to Purchase
The evolution of the middle Paleozoic subduction in the South Armorican Massif (southern Brittany, France) is compared with that of the Petite Sole-Cordoba fault (western Spain and Portugal). This comparison suggests that this fault acted as a transform fault during Ordovician and Devonian times. The gravity and magnetic data compiled on both sides of the North Atlantic indicate that the southern end of the Cordoba fault links with a 2,400-km-long mafic body which extended from the South Portuguese zone to New England (U.S.A.) before the opening of the present Atlantic Ocean. The mafic body may be considered as the suture of the Theic Ocean. However, the closing of the South Armorican and Theic oceans did not occur at the same time; the South Armorican subduction ended in Late Devonian time, whereas the Theic closed in early Carboniferous time. This diachronous evolution could be explained by the existence of an Iberian (Spanish) microplate.