2020
DOI: 10.1016/j.marpetgeo.2019.104146
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A unified contact cementation theory for gas hydrate morphology detection and saturation estimation from elastic-wave velocities

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Cited by 17 publications
(2 citation statements)
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“…The geophysical properties of solid structures are largely controlled by their mechanical properties: fabric, stiffness, volume, permeability, porosity, mineralogy [32][33]. For example, there is a correlation between the elastic compressibility and conductivity of the saturated rocks with porosity [34], gas hydration [35][36][37], or hydrate saturation in the clay-rich marine sediments with compressional wave and shear wave velocity [38]. The geometrical properties of specimen (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…The geophysical properties of solid structures are largely controlled by their mechanical properties: fabric, stiffness, volume, permeability, porosity, mineralogy [32][33]. For example, there is a correlation between the elastic compressibility and conductivity of the saturated rocks with porosity [34], gas hydration [35][36][37], or hydrate saturation in the clay-rich marine sediments with compressional wave and shear wave velocity [38]. The geometrical properties of specimen (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…The Guangzhou Marine Geological Survey conducted the GMGS5 cruise, drilling multiple times in strata with obvious continuous seabed-like bottom-simulating reflectors (BSRs), finding that hydrate-bearing layer thicknesses in different wells range from 4 to 165 metres, presenting significant differences. Due to ongoing research on saturation calculations based on resistivity or acoustic logging, it is difficult to determine the enrichment of hydrates in geological formations (Pan et al, 2020Li et al, 2022Wan et al, 2022;Zhu et al, 2022b;Zhu et al, 2023a). This study is based on K-means clustering and the Adaboost method and provides reliable reservoir classification results.…”
mentioning
confidence: 99%