- 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
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Asia
-
Himalayas (2)
-
Indian Peninsula
-
India (1)
-
Indus Valley (1)
-
Jammu and Kashmir
-
Ladakh (1)
-
-
Nepal (1)
-
-
Indus River (1)
-
Siwalik Range (1)
-
-
Atlantic Ocean
-
North Atlantic
-
Gulf of Mexico (1)
-
-
-
Canada
-
Western Canada
-
Alberta
-
Alberta Basin (1)
-
-
-
-
Europe
-
Alps
-
French Alps (1)
-
Prealps (1)
-
-
Carpathian Foredeep (1)
-
Carpathians (1)
-
Western Europe
-
France
-
Alpes-de-Haute Provence France (1)
-
Alpes-Maritimes France (1)
-
Aquitaine Basin (1)
-
French Alps (1)
-
Var France (1)
-
-
-
-
Front Range (1)
-
North America
-
Great Plains
-
Northern Great Plains (1)
-
-
Rocky Mountains
-
U. S. Rocky Mountains
-
Medicine Bow Mountains (1)
-
-
-
-
Platte River basin (1)
-
United States
-
Nebraska (1)
-
U. S. Rocky Mountains
-
Medicine Bow Mountains (1)
-
-
-
-
elements, isotopes
-
isotopes
-
radioactive isotopes
-
Al-26 (1)
-
Be-10 (1)
-
-
stable isotopes
-
Ne-21 (1)
-
-
-
metals
-
alkaline earth metals
-
beryllium
-
Be-10 (1)
-
-
-
aluminum
-
Al-26 (1)
-
-
-
noble gases
-
neon
-
Ne-21 (1)
-
-
-
-
geochronology methods
-
exposure age (1)
-
optically stimulated luminescence (1)
-
thermochronology (1)
-
-
geologic age
-
Cenozoic
-
Quaternary (1)
-
Tertiary
-
Neogene
-
Miocene
-
Ash Hollow Formation (1)
-
-
-
Paleogene
-
Eocene
-
Annot Sandstone (2)
-
-
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
quartzites (2)
-
-
turbidite (2)
-
-
Primary terms
-
Asia
-
Himalayas (2)
-
Indian Peninsula
-
India (1)
-
Indus Valley (1)
-
Jammu and Kashmir
-
Ladakh (1)
-
-
Nepal (1)
-
-
Indus River (1)
-
Siwalik Range (1)
-
-
Atlantic Ocean
-
North Atlantic
-
Gulf of Mexico (1)
-
-
-
Canada
-
Western Canada
-
Alberta
-
Alberta Basin (1)
-
-
-
-
Cenozoic
-
Quaternary (1)
-
Tertiary
-
Neogene
-
Miocene
-
Ash Hollow Formation (1)
-
-
-
Paleogene
-
Eocene
-
Annot Sandstone (2)
-
-
-
-
-
continental slope (1)
-
data processing (2)
-
deformation (1)
-
Europe
-
Alps
-
French Alps (1)
-
Prealps (1)
-
-
Carpathian Foredeep (1)
-
Carpathians (1)
-
Western Europe
-
France
-
Alpes-de-Haute Provence France (1)
-
Alpes-Maritimes France (1)
-
Aquitaine Basin (1)
-
French Alps (1)
-
Var France (1)
-
-
-
-
faults (3)
-
geochronology (1)
-
geomorphology (1)
-
isotopes
-
radioactive isotopes
-
Al-26 (1)
-
Be-10 (1)
-
-
stable isotopes
-
Ne-21 (1)
-
-
-
metals
-
alkaline earth metals
-
beryllium
-
Be-10 (1)
-
-
-
aluminum
-
Al-26 (1)
-
-
-
metamorphic rocks
-
quartzites (2)
-
-
noble gases
-
neon
-
Ne-21 (1)
-
-
-
North America
-
Great Plains
-
Northern Great Plains (1)
-
-
Rocky Mountains
-
U. S. Rocky Mountains
-
Medicine Bow Mountains (1)
-
-
-
-
orogeny (1)
-
paleogeography (1)
-
plate tectonics (1)
-
sedimentary rocks
-
carbonate rocks
-
limestone (1)
-
-
clastic rocks
-
conglomerate (3)
-
marl (1)
-
mudstone (1)
-
sandstone (2)
-
-
-
sedimentary structures
-
planar bedding structures
-
cross-bedding (1)
-
-
-
sediments
-
clastic sediments
-
gravel (2)
-
-
-
tectonics (2)
-
United States
-
Nebraska (1)
-
U. S. Rocky Mountains
-
Medicine Bow Mountains (1)
-
-
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
limestone (1)
-
-
clastic rocks
-
conglomerate (3)
-
marl (1)
-
mudstone (1)
-
sandstone (2)
-
-
-
turbidite (2)
-
-
sedimentary structures
-
channels (1)
-
sedimentary structures
-
planar bedding structures
-
cross-bedding (1)
-
-
-
-
sediments
-
sediments
-
clastic sediments
-
gravel (2)
-
-
-
turbidite (2)
-
Conglomerate recycling in the Himalayan foreland basin: Implications for grain size and provenance
Detrital cosmogenic 21 Ne records decoupling of source-to-sink signals by sediment storage and recycling in Miocene to present rivers of the Great Plains, Nebraska, USA
Squeezing river catchments through tectonics: Shortening and erosion across the Indus Valley, NW Himalaya
Foreland basin subsidence driven by topographic growth versus plate subduction
Punctuated thrust deformation in the context of doubly vergent thrust wedges: Implications for the localization of uplift and exhumation
Depositional Evolution of Confined Turbidite Basins
Delta-Fed Turbidites Infilling Topographically Complex Basins: A New Depositional Model for the Annot Sandstones, SE France
The Balkan Thrust Wedge and Foreland Basin of Eastern Bulgaria: Structural and Stratigraphic Development
Abstract The Balkan Mountains of Bulgaria run east-west and outcrop along the north-south-running Black Sea coastline. Immediately north of the Balkan thrust front is the Kamchia Depression, which has been interpreted to repre-sent the North Balkan foreland basin. To the south is the Srednogorie Zone, comprising Cretaceous calc-alkaline volcanics representing a remnant vol-canic arc. A north-south structural cross section can be generated by the inte-gration of coastal exposures, with deeper level constraint from onshore and offshore seismic data. In this section, the Balkans comprise two large syn- clines bounded by major faults. This folding and thrusting detached at a horizon within the Jurassic succession at ~5 km depth. Section restoration across the Balkans from the remnants of the volcanic arc in the south to the Balkan thrust front in the north gives a minimum of 18 km of shortening. Seismic stratigraphy indicates two periods of shortening across the Balkans. Initially, deep-seated normal faults that offset the Triassic were reactivated as reverse faults at the end of the Cretaceous. The sea-floor topography generated during this compression was subsequently draped by Paleocene and lower and middle Eocene strata. At end-middle Eocene times, thin-skinned thrusts propagated into the basin, initiating the main Balkan structures. The termination of shortening is recorded by the blanketing of thrust-related topography at end-Oligocene times. Therefore, the>18 km of shortening took place from early Paleocene to end-Oligocene times; this indicates a time-averaged rate of shortening of ~0.5 km/m.y. The sedimentary fill of the Kamchia Depression is intimately linked to the growth of the Balkan Mountain belt. At end Cretaceous/early Tertiary times, it was characterized by emergence in the north linked to the deep-level fault reactivation, and deepening in the south to bathyal depths, where calci-turbidites accumulated. During the early Eocene times, siliciclastics were deposited in the south and center of the basin, and the northern margin experienced a marine transgression; this is thought to be related to the load-induced subsidence of the southern margin of the Moesian Platform by the Balkan Mountains. By the middle Eocene, immediately prior to thrust encroachment into the basin, the northern margin underwent mass wasting in the form of debris flows, slumps, and gravity glide sheets. At a similar time, micropaleontological indicators suggest reduced oceanic circulation, possibly linked to physical isolation of the Black Sea region by growing mountain belts to the south. Subsidence analysis offshore indicates accelerated tectonic subsidence during middle and upper Eocene times, thus strengthening the proposed link between early thrusting and deepening of the basin. The structural, sed-imentological, and subsidence history of this basin strongly supports its interpretation as the north Balkan retro-arc foreland basin. Rates of tectonic subsidence (>0.05 km/m.y.) and crustal shortening (<0.5 km/m.y.) are slow compared to other thrust wedge/foreland basin settings.