By M. Sosson, N. Kaymakci, R. A. Stephenson, V. Starostenko, F. Bergerat
This vast sector of the Alpine-Himalayan belt advanced via a chain of tectonic occasions regarding the outlet and closure of the Tethys Ocean. In doing so it produced the biggest mountain belt of the area, which extends from the Atlantic to the Pacific oceans. The basins linked to this belt include valuable details on the topic of mountain development tactics and are the locus of wealthy hydrocarbon accumulations. even though, wisdom in regards to the geological evolution of the area is restricted in comparison to what they give. This has been frequently as a result trouble and inaccessibility of cross-country reviews. This designated e-book is devoted to the a part of the Alpine-Himalayan belt working from Bulgaria to Armenia, and from Ukraine to the Arabian Platform. It comprises twenty multidisciplinary stories overlaying subject matters in structural geology/tectonics; geophysics; geochemistry; palaeontology; petrography; sedimentology; stratigraphy; and subsidence and lithospheric modelling. This quantity studies effects got through the MEBE (Middle East Basin Evolution) Programme and similar initiatives within the circum Black Sea and peri-Arabian regions.The Geological Society of LondonFounded in 1807, the Geological Society of London is the oldest geological society on this planet, and one of many biggest publishers within the Earth sciences.The Society publishes a variety of fine quality peer-reviewed titles for lecturers and execs operating within the geosciences, and enjoys an enviable overseas popularity for the standard of its work.The many parts during which we post in include:-Petroleum geology-Tectonics, structural geology and geodynamics-Stratigraphy, sedimentology and paleontology-Volcanology, magmatic stories and geochemistry-Remote sensing-History of geology-Regional geology courses
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Extra info for Sedimentary Basin Tectonics from the Black Sea and Caucasus to the Arabian Platform - Special Publication 340 (Geological Society Special Publication)
The features of the present single Black Sea Basin formed in Anthropogene time are shown in Figure 3 with the accumulation of thick (more than 3 km) deposits within the Danube delta in the west and in the DonKuban delta in the east, over the Kerch-Taman shelf. 5–4 km) Mesozoic (and possibly older) succession below the Cenozoic strata (Tugolesov et al. 1985; Finetti et al. 1988). The Cretaceous succession is the most investigated among these. Correlation with strata on the flanks of the basin, on the Andrusov and Shatsky Ridges and within the EBS has allowed tentative age estimates to be made.
Structure and evolution of the Earth’s crust and upper mantle of the Black Sea. Bolletino di Geofisica Teorica ed Applicata, XXX/117-188, 109–196. , Spakman, W. & Engdahl, E. 1998. Closing the gap between regional and global travel time tomography. 1029/98JB02467. , Korotaev, M. , Ershov, A. V. & Nikishin, A. M. 2003. The South-Caspian Basin: a review of its evolution from subsidence modelling. Sedimentary Geology, 156, 119–148. Buryanov, V. B. & Soloviev, V. D. 1996. Study of gravity maxima of the northern and western frame of the Black Sea Depression.
YEGOROVA & V. GOBARENKO Fig. 4. Gravity field of the Black Sea and surrounded regions: Free Air anomalies offshore and Bouguer anomalies onshore (a) 4 km data discretization from European database (Wybraniec et al. 1998), and residual (sediment-free) anomalies; (b) dashed line in (a) indicates 200 m isobate of the seawater bathymetry, along which stripe gravity highs are distinguished. 65 Â 103 kg/m3) sediments. 85 Â 103 kg/m3. For the abbreviation see explanations to Figure 2; in addition BK, GA, CP indicate the Balkanides, Gubkin anomaly and Carpathian gravity low respectively.