Results 171 to 180 of about 3,373,518 (212)

Evolution of the Greater Caucasus Basement and Formation of the Main Caucasus Thrust, Georgia

open access: yesTectonics, 2020
Abstract Along the northern margin of the Arabia‐Eurasia collision zone in the western Greater Caucasus, the Main Caucasus Thrust (MCT) juxtaposes Paleozoic crystalline basement to the north against Mesozoic metasedimentary and volcaniclastic rocks to the south.
Eric S. Cowgill   +2 more
exaly   +4 more sources

Subducted, Detached, and Torn Slabs Beneath the Greater Caucasus [PDF]

open access: yesGeoResJ, 2015
The Greater Caucasus Mountains contain the highest peaks in Europe and define, for over 850km along strike, the leading edge of the second-largest active collisional orogen on Earth. However, the mechanisms by which this range is being constructed remain
Charles C. Trexler   +2 more
exaly   +2 more sources

Sedimentary Response to a Collision Orogeny Recorded in Detrital Zircon Provenance of Greater Caucasus Foreland Basin Sediments

open access: yesBasin Research, 2021
The Greater Caucasus orogen on the southern margin of Eurasia is hypothesized to be a young collisional system and may present an opportunity to probe the structural, sedimentary and geodynamic effects of continental collision. We present detrital zircon
Fakhraddin Kadirov   +2 more
exaly   +2 more sources
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Active Convergence Between the Lesser and Greater Caucasus in Georgia: Constraints on the Tectonic Evolution of the Lesser–Greater Caucasus Continental Collision

Earth and Planetary Science Letters, 2018
Abstract We present and interpret newly determined site motions derived from GPS observations made from 2008 through 2016 in the Republic of Georgia, which constrain the rate and locus of active shortening in the Lesser–Greater Caucasus continental collision zone.
Robert King   +2 more
exaly   +2 more sources

Between the Greater and Lesser Caucasus

2021
This article presents a new study of three burial contexts from the important Tli graveyard located in the Southern Caucasus. The three tombs contained bronze belts with features mainly pertaining to an Assyro-Urartian tradition. An analysis of the belts’ iconographic apparatuses is given, together with a new chronological position proposed for the ...
Bonfanti, Annarita   +2 more
openaire   +1 more source

Quantifying Arabia–Eurasia Convergence Accommodated in the Greater Caucasus by Paleomagnetic Reconstruction

open access: yesEarth and Planetary Science Letters, 2018
Since the late Eocene, convergence and subsequent collision between Arabia and Eurasia was accommodated both in the overriding Eurasian plate forming the Greater Caucasus orogen and the Iranian plateau, and by subduction and accretion of the Neotethys ...
Derya Gürer   +2 more
exaly   +2 more sources

Central Greater Caucasus

2018
This chapter provides the geomorphological characteristics of the central Greater Caucasus sub-zone. Orographic units are reviewed in detail, such as: the central Greater Caucasus main watershed range, the Enguri River and its tributaries, Egrisi (Samegrelo) and Svaneti ranges, the Tskhenistskali River and its tributaries, Lechkhumi Range, the Rioni ...
Levan Tielidze   +3 more
openaire   +1 more source

Eastern Greater Caucasus

2018
This chapter presents the geomorphological characterization of the sub-region of the eastern Greater Caucasus. The orographical units are considered in detail, including: the main watershed range of the eastern Greater Caucasus, Khokhi Range, the gorges of the Tergi River and its tributaries, Kuro, Shavana and Kidegani ranges, the Asa River gorge ...
Levan Tielidze   +2 more
openaire   +1 more source

A New Look at the Old Deposit of the Greater Caucasus

Geomodel 2020, 2020
Summary This paper stresses the need for reinterpretation of seismic data for brown fields on the basis of data from the field located on the territory of the Greater Caucasus. Emergence of new technologies stimulates operators to shift their focus to traditional oil provinces that were explored a long time ago.
T.A. Yurkina, G.R. Gataulin
openaire   +1 more source

The Mesozoic-Cenozoic tectonic evolution of the Greater Caucasus

Geological Society, London, Memoirs, 2006
Abstract The Greater Caucasus (GC) fold-and-thrust belt lies on the southern deformed edge of the Scythian Platform (SP) and results from the Cenozoic structural inversion of a deep marine Mesozoic basin in response to the northward displacement of the Transcaucasus (lying south of the GC) subsequent to the Arabia-Eurasia collision.
Saintot, A.N.   +7 more
openaire   +2 more sources

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