Black Sea Methane Hydrate Stability Zone Contribution 11, by: L. Dimitrov and A. Vassilev Adapted from: Vassilev, A. and L. Dimitrov, Spatial and qualitative evaluation of methane hydrates in the Black Sea. Geology & Geophysics. 43(7):

The average water depth from which methane hydrate start to forms runs from 620 m to 700 m embracing a prone area of 288,100 km 2. The average thickness of the MHSZ is 303 m with a bulk of sediment running from 85,310 to 100,280 km 3. Generalized methods of estimation set the total methane content on 10-50x10 12 m 3 and more precise evaluations suggest x10 12 m 3 of methane are trapped within the Black Sea gas hydrates.

Black Sea Gas Hydrate Shows Core of the first gas hydrate finding in the Black Sea on the slope of Danube fan at water depth of 1950 m (43 o 35’ N - 31 o 08’ E) in (Dgigchenko, B.P., Hydrocarbon Gases. Nedra, Moscow, 112 p.) Core of the first gas hydrate finding in the Black Sea on the slope of Danube fan at water depth of 1950 m (43 o 35’ N - 31 o 08’ E) in (Dgigchenko, B.P., Hydrocarbon Gases. Nedra, Moscow, 112 p.)

Black Sea Gas Hydrate Shows ? ?

Several gas hydrate samples in the mud volcano area of Sorokin Trough (separate mud volcanoes are named). (Bouryak & Akhmetjanov, Marine Geology, 137: Bohrman et al., th Conference “Gas in Marine Sediments”, 7-12 October, Baku, Azerbaijan) Several gas hydrate samples in the mud volcano area of Sorokin Trough (separate mud volcanoes are named). (Bouryak & Akhmetjanov, Marine Geology, 137: Bohrman et al., th Conference “Gas in Marine Sediments”, 7-12 October, Baku, Azerbaijan)

BSRs observed along the northern Caucasian margin and eastern part of Cuban fan where Meisner and co-workers (1998) reported that more than 200 km 2 of continuous BSR.

Side-scan sonar image of supposed gas hydrate mounds on the seafloor (dark patches) and corresponding subbottom profiler section. (after Kruglyakova et al., Geology and Geophysics, 43 (7): ).

Lump of gas hydrate from the bottom of the core from the same location. (after Gibsburg and Soloviev, 1998)

Plates of gas hydrates in deformed muds from a mud volcano, offshore Crimea (44 o 17’40’’ N – 34 o 58’39’’). (Gibsburg, G. & V. Soloviev, Submarine Gas Hydrates. VNIIOkeangeologia, St.Petersburg) Plates of gas hydrates in deformed muds from a mud volcano, offshore Crimea (44 o 17’40’’ N – 34 o 58’39’’). (Gibsburg, G. & V. Soloviev, Submarine Gas Hydrates. VNIIOkeangeologia, St.Petersburg)

Two cores with gas hydrate finding taken in the Bulgarian zone of the continental slope in (C193 - water depth of 1970 m (42 o 53.6’ N - 29 o 10.2’ E; (C211 - water depth of 2100 m (42 o 09.4’ N - 29 o 32.7’ E) Institute of Oceanology, Varna, Bulgaria Two cores with gas hydrate finding taken in the Bulgarian zone of the continental slope in (C193 - water depth of 1970 m (42 o 53.6’ N - 29 o 10.2’ E; (C211 - water depth of 2100 m (42 o 09.4’ N - 29 o 32.7’ E) Institute of Oceanology, Varna, Bulgaria

4 gas hydrate findings sampled from two mud volcanoes in the abyssal plain in Konyuhov et al., Mud volcanoes and gas hydrates in the deep water parts of the Black Sea. (in Russian) Lithology and Mineral Resources, 137: gas hydrate findings sampled from two mud volcanoes in the abyssal plain in Konyuhov et al., Mud volcanoes and gas hydrates in the deep water parts of the Black Sea. (in Russian) Lithology and Mineral Resources, 137:

That’s all for now… Lyobomir That’s all for now… Lyobomir