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

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Chapter 3 Figure 3 (a) Uninterpreted migrated seismic Line GeoB07-137 in Area 1. (b) Six seismic units are indicated based on identified unconformities and boundaries between different domains of seismic amplitude. Six basal horizons for the six units are named H1 to H6. Different seismic facies can be identfied as marked. Three upbending reflection structures are marked by black dotted ellipses and named I, II, III. The truncation and unconformity surfaces are indicated by the green arrows in the enlarged figures. See the location of the profile in Figure 2. 73
Chapter 3 Figure 4 (a) Uninterpreted migrated seismic Line GeoB07-141 in Area 1. (b) Interpreted seismic Line GeoB07-141, showing seismic facies A, B, D, E, F and G, and seismic units (1-6). (c) Seismic facies G, green arrows indicate the downlap. See Figure 2 for location. 74
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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
Page 28 and 29: Chapter 1 1.5 Geological setting of
Page 30 and 31: Chapter 1 main sequences consist of
Page 32 and 33: Chapter 1 craterlike depressions wi
Page 34 and 35: Chapter 1 Jurassic - Paleogene, Upp
Page 36 and 37: Chapter 1 respectively, and one wat
Page 38 and 39: Chapter 1 During the seismic data p
Page 40 and 41: Chapter 1 1.6.2 The Parasound sedim
Page 42 and 43: Chapter 1 Caress, D.W., and Chayes,
Page 44 and 45: Chapter 1 Hovland, M., Gardner, J.V
Page 46 and 47: Chapter 1 Luo, X.R. and Vasseur, G.
Page 48 and 49: Chapter 1 Schroot, B.M., Klaver, G.
Page 50 and 51: Chapter 2 Chapter 2. Shallow Gas Tr
Page 52 and 53: Chapter 2 times. Seismically imaged
Page 54 and 55: Chapter 2 spike noise were marked a
Page 56 and 57: Chapter 2 The 2D high resolution se
Page 58 and 59: Chapter 2 Figure 4 A close-up of se
Page 60 and 61: Chapter 2 within the upper sediment
Page 62 and 63: Chapter 2 volcanoes between 66 and
Page 64 and 65: Chapter 2 Figure 7 Geo-seismic sect
Page 66 and 67: Chapter 2 In the study area, many b
Page 68 and 69: Chapter 2 volcanism could be calcul
Page 70 and 71: Chapter 2 along the feeder channel
Page 72 and 73: Chapter 2 Evpatoriya). Soviet Geol
Page 74 and 75: Chapter 3 Chapter 3. Sedimentary Ev
Page 76 and 77: Chapter 3 South (Fig. 2). The water
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 126 and 127: Chapter 4 Klaucke, I., Sahling, H.,
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Chapter 4 Wagner-Friedrichs, M., 20
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Chapter 5 deposited; during lowstan
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Chapter 5 accumulations. An acousti
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Acknowledgements Acknowledgements I
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