scholarly journals An Overview of Mud Volcanoes Associated to Gas Hydrate System

10.5772/51270 ◽  
2012 ◽  
Author(s):  
Umberta Tinivella ◽  
Michela Giustiniani
Keyword(s):  
Gas Hydrate ◽  
Mud Volcanoes

The Evolution of Gas Hydrate Accumulations in Zones of Deep-Sea Mud Volcanoes

2019 ◽  
Vol 13 (2) ◽  
pp. 107-111
Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov
Keyword(s):  
Gas Hydrate ◽  
Deep Sea ◽  
Mud Volcanoes ◽  
Sea Mud

Gas hydrate and mud volcanoes on the southwest African continental margin off South Africa

Geology ◽  
2002 ◽  
Vol 30 (10) ◽  
pp. 927 ◽  
Author(s):  
Zvi Ben-Avraham ◽  
George Smith ◽  
Moshe Reshef ◽  
Eric Jungslager
Keyword(s):  
South Africa ◽  
Continental Margin ◽  
Gas Hydrate ◽  
Mud Volcanoes

scholarly journals Relations between mud volcanoes, thrust deformation, slope sedimentation, and gas hydrate, offshore north Panama

1990 ◽  
Vol 7 (1) ◽  
pp. 44-54 ◽  
Author(s):  
Donald L. Reed ◽  
E.A. Silver ◽  
J.E. Tagudin ◽  
T.H. Shipley ◽  
P. Vrolijk
Keyword(s):  
Gas Hydrate ◽  
Mud Volcanoes

First discovery and formation process of authigenic siderite from gas hydrate–bearing mud volcanoes in fresh water: Lake Baikal, eastern Siberia

2008 ◽  
Vol 35 (5) ◽  
Author(s):  
Alexey Krylov ◽  
Oleg Khlystov ◽  
Tamara Zemskaya ◽  
Hirotsugu Minami ◽  
Akihiro Hachikubo ◽  
...  
Keyword(s):  
Fresh Water ◽  
Lake Baikal ◽  
Gas Hydrate ◽  
Formation Process ◽  
Eastern Siberia ◽  
Mud Volcanoes ◽  
Water Lake ◽  
Fresh Water Lake

Isotopic composition of dissolved inorganic carbon in subsurface sediments of gas hydrate-bearing mud volcanoes, Lake Baikal: implications for methane and carbonate origin

2010 ◽  
Vol 30 (3-4) ◽  
pp. 427-437 ◽  
Author(s):  
Alexey A. Krylov ◽  
Oleg M. Khlystov ◽  
Akihiro Hachikubo ◽  
Hirotsugu Minami ◽  
Yutaka Nunokawa ◽  
...  
Keyword(s):  
Isotopic Composition ◽  
Lake Baikal ◽  
Gas Hydrate ◽  
Inorganic Carbon ◽  
Dissolved Inorganic Carbon ◽  
Mud Volcanoes ◽  
Subsurface Sediments

scholarly journals Evolution of gas hydrates accumulation in zones of submarine mud volcanoes

2019 ◽  
pp. 45-51
Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov
Keyword(s):  
Mathematical Model ◽  
Numerical Modeling ◽  
Gas Hydrates ◽  
Gas Hydrate ◽  
Sedimentary Basins ◽  
Feeder Layer ◽  
Mud Volcanoes ◽  
Layer Depth ◽  
Medium Temperature ◽  
Hydrate Saturation

The article examines the processes of evolution of gas hydrate accumulations, related to submarine mud volcanoes. A mathematical model and the results of numerical modeling of the accumulation of gas hydrates in the seabed in the deep structures of underwater mud volcanoes are presented. Numerical analysis of the influence held feeder layer depth and pressure therein to the evolution of gas hydrate saturation confined to deep water mud volcanoes were performed. Modeling quantitatively showed that hydrate saturation in areas of underwater mud volcanoes is not constant and its evolution depends on the geophysical properties of the bottom medium (temperature gradient, porosity, permeability, physical properties of sediments) and the depth of the supply reservoir and pressure in it, and the rate of hydrate accumulation in tens and hundreds times the rate of hydrate accumulation in the sedimentary basins of passive continental margin.

scholarly journals Evolution of gas hydrates accumulation in zones of submarine mud volcanoes

2019 ◽  
pp. 45-51 ◽  
Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov
Keyword(s):  
Mathematical Model ◽  
Numerical Modeling ◽  
Gas Hydrates ◽  
Gas Hydrate ◽  
Sedimentary Basins ◽  
Feeder Layer ◽  
Mud Volcanoes ◽  
Layer Depth ◽  
Medium Temperature ◽  
Hydrate Saturation

The article examines the processes of evolution of gas hydrate accumulations, related to submarine mud volcanoes. A mathematical model and the results of numerical modeling of the accumulation of gas hydrates in the seabed in the deep structures of underwater mud volcanoes are presented. Numerical analysis of the influence held feeder layer depth and pressure therein to the evolution of gas hydrate saturation confined to deep water mud volcanoes were performed. Modeling quantitatively showed that hydrate saturation in areas of underwater mud volcanoes is not constant and its evolution depends on the geophysical properties of the bottom medium (temperature gradient, porosity, permeability, physical properties of sediments) and the depth of the supply reservoir and pressure in it, and the rate of hydrate accumulation in tens and hundreds times the rate of hydrate accumulation in the sedimentary basins of passive continental margin.

Active mud volcanoes in the gas hydrate potential area of the upper Kaoping Slope, off southwest Taiwan

2014 ◽  
Author(s):  
Song-Chuen Chen ◽  
Shu-Kun Hsu ◽  
Yunshuen Wang ◽  
San-Hsiung Chung ◽  
Po-Chun Chen ◽  
...  
Keyword(s):  
Gas Hydrate ◽  
Mud Volcanoes ◽  
Potential Area
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