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

Author(s):  
Umberta Tinivella ◽  
Michela Giustiniani
Keyword(s):  
2019 ◽  
Vol 13 (2) ◽  
pp. 107-111
Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov
Keyword(s):  
Deep Sea ◽  

Geology ◽  
2002 ◽  
Vol 30 (10) ◽  
pp. 927 ◽  
Author(s):  
Zvi Ben-Avraham ◽  
George Smith ◽  
Moshe Reshef ◽  
Eric Jungslager

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):  

2008 ◽  
Vol 35 (5) ◽  
Author(s):  
Alexey Krylov ◽  
Oleg Khlystov ◽  
Tamara Zemskaya ◽  
Hirotsugu Minami ◽  
Akihiro Hachikubo ◽  
...  

2010 ◽  
Vol 30 (3-4) ◽  
pp. 427-437 ◽  
Author(s):  
Alexey A. Krylov ◽  
Oleg M. Khlystov ◽  
Akihiro Hachikubo ◽  
Hirotsugu Minami ◽  
Yutaka Nunokawa ◽  
...  

Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov

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.


Author(s):  
A. L. Sobisevich ◽  
E. I. Suetnova ◽  
R. A. Zhostkov

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.


Author(s):  
Song-Chuen Chen ◽  
Shu-Kun Hsu ◽  
Yunshuen Wang ◽  
San-Hsiung Chung ◽  
Po-Chun Chen ◽  
...  

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