Seismoacoustic Study of the Shallow Gas Transport and ... - E-LIB

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Chapter 4 Klaucke, I., Sahling, H., Weinrebe, W., Blinova, V., Bürk, D., Lursmanashvili, N., and Bohrmann, G, 2006. Acoustic investigation of cold seeps offshore Georgia, eastern Black Sea. Marine Geology, 231: 51-67. Kotelnikova S, 2002. Microbial production and oxidation of methane in deep subsurface. Earth-Sci Rev 58: 367-395 Kou-Yuan Huang and King-Sun Fu, 1984. Detection of bright spots in seismic signal using tree classifiers. Geoexploration 23, 121-145. Krastel, S., Spiess, V., Ivanov, M.K., Weinrebe, W., Bohrmann, G. and Shashkin, P., 2003. Acoustic images of mud volcanoes in the Sorokin Trough, Black Sea. Geo-Marine Letters, 23: 230-238. Lericolais, G., Bulois, C., Gillet, H., and Guichard, F., 2009, High frequency sea level fluctuations recorded in the Black Sea since the LGM: Global and Planetary Change, Volume 66, Issues 1–2, 65-75 Limonov, A.F., van Weering, Tj.C.E., Kenyon, N.H., Ivanov, M.K., and Meisner, L.B., 1997. Seabed morphology and gas venting in the Black Sea mud volcano area: Observation with the MAK-1 deeptow side scan sonar and bottom profiler. Marine Geology, 137: 121-136. Limonov, A.F., Woodside, J.M., and Ivanov, M.K. (Eds.), 1994. Mud volcanism in the Mediterranean and Black Seas and shallow structure of the Eratostenes Seamount. Initial results of the geological and geophysical investigations during the third UNESCO-ESF 'Training Through Research' Cruise of RV Gelendzhik, June-July 1993. UNESCO Rep. Mar. Sci., 64. 173 pp. Max, M.D., 1990. Gas hydrate and acoustically laminated sediments: probable environmental cause of anomalously low acoustic-interaction bottom loss in deep ocean sediments. Naval Research Laboratory report, 9235: 68pp. Mazzini, A., Ivanov, M.K., Parnell, J., Stadnitskaya, A., Cronin, B.T., Poludetkina, E., Mazurenko, L., and van Weering, T.C.E., 2004. Methane-related authigenic carbonates from the Black Sea: geochemical characterisation and relation to seeping fluids. Marine Geology, 212: 153-181. Michaelis, W., Seifert, R., Nauhaus, K., Treude, T., Thiel, V., Blumenberg, M., Knittel, K., Gieseke, A., Peterknecht, K., Pape, T., Boetius, A., Amann, R., Jörgensen, B.B., Widdel, F., Peckmann, J., Pimenov, N.V., and Guli, M.B., 2002. Microbial reefs in the Black Sea fuelled by anaerobic oxidation of methane. Science, 297: 1013-1015. Milkov, A.V., Dickens, G.R., Claypool, G.E., Lee, Y.-J., Borowski, W.S., Torres, M.E., Xu, W., Tomaru, H., Tréhu, A.M., and Schultheiss, P., 2004. Co-existence of gas hydrate, free gas, and brine within the regional gas hydrate stability zone at Hydrate Ridge (Oregon margin): evidence from prolonged degassing of a pressurized core. EPSL, 222: 829-843. Naudts, L., Greinert, Jens, Artemov, Yu., Staelens, P., Poort, J., Vans Regenbergen, P. and De Batist, M., 2006. Geological and morphological setting of 2778 methane seeps in the Dnepr paleo-delta, northwestern Black Sea Marine Geology, 227 (3/4). pp. 177-199. Nikishin, A.M., Korotaev, M.V., Ershov, A.V., Brunet, M.-F., 2003. The Black Sea basin: tectonic history and Neogene–Quaternary rapid subsidence modelling. Sedimentary Geology 156, 121
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Seismoacoustic Study of the Shallow
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Table of contents Table of contents
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Abstract Abstract In recent years,
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Outline of the Dissertation Outline
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Chapter 1 Chapter 1. Introduction 1
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Chapter 1 reflections, interpreted
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Chapter 1 Submarine gas seeps, pock
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Chapter 1 which have documented act
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Chapter 1 fluid migration related t
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Chapter 1 Evidence of gas seepage
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Chapter 1 The three main different
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Chapter 1 from deeper sources in th
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Chapter 1 numerous countries such a
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Chapter 1 1.5 Geological setting of
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Chapter 1 main sequences consist of
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Chapter 1 craterlike depressions wi
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Chapter 1 Jurassic - Paleogene, Upp
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Chapter 1 respectively, and one wat
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Chapter 1 During the seismic data p
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Chapter 1 1.6.2 The Parasound sedim
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Chapter 1 Caress, D.W., and Chayes,
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Chapter 1 Hovland, M., Gardner, J.V
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Chapter 1 Luo, X.R. and Vasseur, G.
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Chapter 1 Schroot, B.M., Klaver, G.
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Chapter 2 Chapter 2. Shallow Gas Tr
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Chapter 2 times. Seismically imaged
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Chapter 2 spike noise were marked a
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Chapter 2 The 2D high resolution se
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Chapter 2 Figure 4 A close-up of se
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Chapter 2 within the upper sediment
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Chapter 2 volcanoes between 66 and
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Chapter 2 Figure 7 Geo-seismic sect
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Chapter 2 In the study area, many b
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Chapter 2 volcanism could be calcul
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Chapter 2 along the feeder channel
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Chapter 2 Evpatoriya). Soviet Geol
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Chapter 3 Chapter 3. Sedimentary Ev
Page 76 and 77: Chapter 3 South (Fig. 2). The water
Page 78 and 79: Chapter 3 Figure 3 (a) Uninterprete
Page 80 and 81: Chapter 3 Seven seismic facies type
Page 82 and 83: Chapter 3 Seismic Unit 5 ranges in
Page 84 and 85: Chapter 3 3.4.3.5. Seismic Unit 2 A
Page 86 and 87: Chapter 3 Figure 11 (a) Uninterpret
Page 88 and 89: Chapter 3 Figure 13 (a) Uninterpret
Page 90 and 91: Chapter 3 boundary between the Plio
Page 92 and 93: Chapter 3 Seismic Unit 6 belongs to
Page 94 and 95: Chapter 3 subsidence was coincident
Page 96 and 97: Chapter 3 Acknowledgements We thank
Page 98 and 99: Chapter 3 Tugolesov, D.A., Gorshkov
Page 100 and 101: Chapter 4 study area at ~900 m wate
Page 102 and 103: Chapter 4 Figure 2 Bathymetry of th
Page 104 and 105: Chapter 4 University of Bremen). At
Page 106 and 107: Chapter 4 and Ridge R2 (GeoB07-139)
Page 108 and 109: Chapter 4 flares location. Anticlin
Page 110 and 111: Chapter 4 GeoB07-145. Green arrows
Page 112 and 113: Chapter 4 4.4.3.2.3. Other anomalou
Page 114 and 115: Chapter 4 Slope fan deposits with f
Page 116 and 117: Chapter 4 Figure 12 Possible locati
Page 118 and 119: Chapter 4 bulk hydrate or even high
Page 120 and 121: Chapter 4 may add to gas accumulati
Page 122 and 123: Chapter 4 The narrow-beam Parasound
Page 124 and 125: Chapter 4 River fan deposits. Being
Page 128 and 129: Chapter 4 Wagner-Friedrichs, M., 20
Page 130 and 131: Chapter 5 deposited; during lowstan
Page 132 and 133: Chapter 5 accumulations. An acousti
Page 134 and 135: Acknowledgements Acknowledgements I
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