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Feature of the Caspian seafloor
The Apsheron Sill, Absheron Sill, Apsheron Ridge or Apsheron Threshold is a major northwest-southeast-trending bathymetric high that runs for about 250
Apsheron_Sill
Seafloor barrier restricting water movement between basins
transtensional regime, thereby forming the gateway. Apsheron Threshold Camarinal Sill Denmark Strait Espartel Sill Mona Passage Beach evolution Coastal management
Aquatic_sill
Major sedimentary and hydrocarbon province in the Caspian Sea
Dag to the east. It is separated from the Central Caspian by the Apsheron Sill (Apsheron-Pribalkhan fault zone), a prominent structural lineament running
South_Caspian_Basin
Earthquake in Turkmenistan
main structure in the Caspian Sea is the Apsheron Sill, a zone of active subduction. The trend of the Apsheron sill is quite oblique to the overall plate
2000_Turkmenistan_earthquake
6.8 earthquake in Baku, Azerbaijan
the North Caucasus thrust belt that continues to the east along the Apsheron Sill, which is interpreted to be a zone of active subduction. Earthquakes
2000_Baku_earthquake
Earthquake in Georgia
Caucasus are a result of active thrust tectonics, linking eastwards to the Apsheron sill. To the south, the Lesser Caucasus mountains are also a result of active
2002_Tbilisi_earthquake
Lake in Eurasia
Island and Cape Tiub-Karagan. The Middle–Southern boundary is the Apsheron Threshold, a sill of tectonic origin between the Eurasian continent and an oceanic
Caspian_Sea
Earthquake in Turkmenistan
and the Eurasian plate. The main structure in the Caspian Sea is the Apsheron Sill, a zone of active subduction. Tsunami waves formed in the Caspian Sea
1895_Balkan_earthquake
Earthquake in Iran
Bitlis-Zagros belt in the south to the Greater Caucasus Mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains in the north. The epicentral area is
856_Damghan_earthquake
Earthquake in West Asia
Bitlis-Zagros belt in the south to the Greater Caucasus Mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains in the north. In Armenia the collision
1679_Armenia_earthquake
Earthquake in Armenia
Bitlis-Zagros belt in the south to the Greater Caucasus Mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains in the north. In Armenia the collision
893_Dvin_earthquake
Geologic zone
and along the zone formed by the Greater Caucasus Mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains further north again. The Zagros FTB extends
Zagros_fold_and_thrust_belt
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APSHERON SILL
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APSHERON SILL
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