The first black Labrador dogs were used to work with fishermen. The first labs were black, or black with some brown markings. The black Labrador dog is the basic labrador retriever.
Top Facts About the Black Labrador Dog
The under explored Offshore Black Sea has gained more attention the latter years since more data has been collected. Upper Jurassic Reefs of the Western Caucasus-Crimea; Hydrocarbon Implications for the Eastern Black Sea Li Guo1, Stephen J. Vincent1, Samuel P. Rice1, and Vladimir Lavrishchev2. Kislovodskaya 203, Yessentuki, RussiaWidespread Upper Jurassic reefs are important potential reservoir facies in the Eastern Black Sea Basin. Outcrops of well-preserved Upper Jurassic reefs can be grouped into coral-dominated, siliceous sponge-microbial and microbial types. Patchy and massive coral-dominated reefs formed at shallow-water platform margins or in slightly restricted deeper-water mid shelf settings. Lithostratigraphy of the Upper Jurassic – Cretaceous Deposits and Hydrocarbon Perspective in the Romanian Shelf of the Black Sea Ovidiu Nicolae Dragastan, Faculty of Geology and Geophysics, Bucharest University, Bulevardul N Balcescu no. 1, Bucharest 010041 Romania, phone: 0040729610876, ovidiud@geo.edu.roIn the Romanian shelf of the Black Sea (offshore), Petromar Co. drilled and has obtained cores of Middle and Upper Jurassic- Cretaceous deposits, as well as Paleogene and Neogene ones. The Permo-Triassic deposits consist of three lithostratigraphic formations: Lower Red Detrital (LRD Fm) (Lower Triassic), Carbonatic-Evaporitic (C-E Fm) (Middle Triassic) and Upper Red Detrital (URD Fm) (Upper Triassic). The main reservoir is a very well sorted sandstone (“Bradesti sandstone”). Seismic profiles, well logs, cores as well as geological cross sections and maps show that during Alpine orogeny, the western part of the platform was gradually underthrusted by the Eastern Carpathian Orogene. Paleocene carbonate platform facies distribution (northern part of the Black Sea basin, Ukrainian offshore) Sergii Vakarchuk, Department of Complex Geology- Industrial Researches, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, Ukraine, phone: +380445850219, fax: +380442487101, vakarchuk@naukanaftogaz.kiev.ua, Piter Chepil, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, and Tetyana Dovzhok, Department of oil and gas geology problems, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, Ukraine. Carbonates of Paleocene occur at depth of 500-6000 m and extend over the most of structural-tectonic zones of the Black Sea basin. South Akcakoca Gas: A Black Sea Discovery 30 Years in the Making Michael J. Fitzgerald, III1, Ed Ramirez1, William Moulton2, and Al Garcia3. (1) Toreador Resources Corp, 4809 Cole Ave, Suite 108, Dallas, TX 75205, phone: 214-559-3933, fax: 214-559-3945, (2) Independent Consultant, (3) Integral Technology GroupSix Eurasian countries surround the Black Sea. This well tested approximately 12.0mmcfgpd from four Eocene age sands. Yayla thrust is composed mostly of shallow marine carbonates of Late Jurassic-Neocomian age. OMV Bulgaria is holding the “Varna Deep Sea” Exploration license in the near offshore from the city of Varna in Eastern Bulgaria. The correct reconstruction of the pre-Jurassic position of the Moesian Platform has important implications for the paleogeography of the Black Sea prior to its opening. late Eocene. The deeply incised canyon formed at that time, was rapidly filled by Oligocene-Miocene sediments, but late Miocene (Messinian?) draw-down of the Black Sea basin was reflected by yet a third period of erosional incision. Eight gas-condensate commercial fields have been discovered within the Odessa shelf (western part of the Ukrainian Black Sea) during last three decades. The productive horizons are located in Upper Cretaceous, Palaeocene, Eocene, Oligocene and Lower Miocene sequences. Last revision of offshore well data with modern technology have allowed to determinate additional prospect reservoirs. Gas chimneys are strong evidences for a likely HC generation system. Prospect reservoirs in water depths of 100 m to 2000 m have a potential to contain hundred million barrels of recoverable HC.Hydrocarbon Bearing Area in the Eastern Part of the Ukrainian Black Sea Sergiy Stovba, “Naukanaftogaz” – Scientific Research Institute of Oil and Gas Industry of National Joint-Stock Company “Naftogaz of Ukraine”, Kyiv, Ukraine, phone: +38 044 5852765, stovba@naukanaftogaz.kiev.ua and Oxana Khriachtchevskaia, Naukanaftogaz, Uritskogo Str., 45, Kyiv, 03035, Ukraine. A regional investigation of the eastern part of the Ukrainian Black Sea has been carried using a vast set of regional seismic reflection profiles, including the new set of regional seismic profiles by Naftogaz of Ukraine. In the easternmost part of the Ukrainian Black Sea a number of high-amplitude anticlines has been mapped in shallow water depth and a huge Mesozoic structure of 400 sq. km in deep water depth (150-700 m). Eocene, Oligocene and Miocene sediments are considered as source rocks with good generative potential for hydrocarbons. There are strong direct hydrocarbon indicators on seismic data. The drilling of Subbotina well up to 4300 m has confirmed the high oil and gas potential of Kerch shelf. Plenty of oil and gas reservoirs were determined along the section of the well. The Black Sea formed within a complicated area. After the Miocene Arabia/Eurasia final collision, Black Sea began shortening as far east as Zonguuldak. We compare this with that of the Tarim Basin and suggest that the Tarim is perhaps a palaeo-Black Sea.Geological History and Hydrocarbon Potential of the Eastern Black Sea Region Anatoly M. Nikishin, Geological Faculty, Moscow State University, Moscow, 119992, Russia, phone: (495) 939 49 31, fax: (495) 939 38 65, nikishin@geol.msu.ru and Aleksandr P. Afanasenkov, YUKOS oil companie, Moscow, Russia. The Eastern Black Sea Basin originated as a back-arc basin during the Cretaceous times. Both the Western and Eastern Black Sea basins have been opened nearly simultaneously during Cenomanian to Coniacian times. Shatsky Ridge was a carbonate platform and zone of pinnacle-type reefs during the Late Jurassic. Shatsky Ridge has a Miocene river system. Hydrocarbon potential of the Shatsky Ridge, Tuapse Basin and Sorokin Basin is connected with: (1) Late Jurassic carbonate platform and system of large pinnacle-type reefs: (2) Possible Paleocene bioclastic limestones; (3) possible Eocene nummulite limestones; (4) possible Oligocene turbitites with sandstone bodies; (5) Miocene river system; (6) Miocene and Pliocene horizons of sandstones.The Impact of Recent Data on the Interpretation of the Geologic Evolution and Petroleum System of the Eastern Black Sea Basin, Offshore Georgia Ryan J. Wilson, Neil Mountford, Paul Maguire, and Richard Hedley. Anadarko Algeria Corporation, 1 Harefield Road, Uxbridge, UB8 1YH, United Kingdom, phone: +44 (0)1895 209400, he genesis and sediment-fill history of the Eastern Black Sea Basin, offshore Georgia has been largely understudied with little new data being acquired since the Soviet Era. Late Miocene to present day depositional systems have a south-easterly provenance of volcanic/lithic origins.In 2005, the first deepwater well in the Eastern Black Sea Basin was drilled offshore Turkey but did not penetrate the northerly-sourced reservoir system. (1) Marine Technology – Environmental Research, Bremen University, Klagenfurter Strasse, Bremen, D-24359, Germany, phone: +49-421-2184598, skrastel@uni-bremen.de, (2) Marine Geology and Hydrocarbon potential department, Okeangeofizika Research Institute, Krymskaja Str. 18, Gelendzhik, 353470, Russia, (3) Marine Geology, Bremen University, Klagenfurter Strasse, Bremen, 28359, Germany, (4) Moscow State UniversityThe Sorokin Trough forms structural depression along the south-eastern margin of the Crimean Peninsula. The lowest sequence consists of the Low Jurassic thick black shales, deposited on the top of Paleozoic basement. Upper Jurassic-Eocene section consists of mainly carbonate rocks. This section contains the reservoir quality rocks. Presence of Upper Jurassic reefs, Eocene nummulitic limestone points to a shallow marine sedimentation. The last thrusting age is progressively older toward the east from Middle Eocene through Late Eocene to Late Eocene/Oligocene. The offshore thrustbelt exhibits thrusting followed by Oligocene-Neogene extension.