Torres, Marta E; Tréhu, Anne M; Cespedes, N; Kastner, Miriam; Wortmann, Ulrich G; Kim, Jung-Hyun; Long, Philip E; Malinverno, Alberto; Pohlman, John W; Riedel, Michael; Collett, Tim S (2008): Sedimentology and gas hydrates of IODP Expedition 311 samples. PANGAEA, https://doi.org/10.1594/PANGAEA.716589, Supplement to: Torres, ME et al. (2008): Methane hydrate formation in turbidite sediments of northern Cascadia, IODP Expedition 311. Earth and Planetary Science Letters, 271(1-4), 170-180, https://doi.org/10.1016/j.epsl.2008.03.061
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Expedition 311 of the Integrated Ocean Drilling Program (IODP) to northern Cascadia recovered gas-hydrate bearing sediments along a SW-NE transect from the first ridge of the accretionary margin to the eastward limit of gas-hydrate stability. In this study we contrast the gas gas-hydrate distribution from two sites drilled ~ 8 km apart in different tectonic settings. At Site U1325, drilled on a depositional basin with nearly horizontal sedimentary sequences, the gas-hydrate distribution shows a trend of increasing saturation toward the base of gas-hydrate stability, consistent with several model simulations in the literature. Site U1326 was drilled on an uplifted ridge characterized by faulting, which has likely experienced some mass wasting events. Here the gas hydrate does not show a clear depth-distribution trend, the highest gas-hydrate saturation occurs well within the gas-hydrate stability zone at the shallow depth of ~ 49 mbsf. Sediments at both sites are characterized by abundant coarse-grained (sand) layers up to 23 cm in thickness, and are interspaced within fine-grained (clay and silty clay) detrital sediments. The gas-hydrate distribution is punctuated by localized depth intervals of high gas-hydrate saturation, which preferentially occur in the coarse-grained horizons and occupy up to 60% of the pore space at Site U1325 and > 80% at Site U1326. Detailed analyses of contiguous samples of different lithologies show that when enough methane is present, about 90% of the variance in gas-hydrate saturation can be explained by the sand (> 63 µm) content of the sediments. The variability in gas-hydrate occupancy of sandy horizons at Site U1326 reflects an insufficient methane supply to the sediment section between 190 and 245 mbsf.
Median Latitude: 48.636087 * Median Longitude: -126.992113 * South-bound Latitude: 48.627133 * West-bound Longitude: -127.000845 * North-bound Latitude: 48.645017 * East-bound Longitude: -126.983317
311-U1325B * Latitude: 48.644900 * Longitude: -126.983317 * Elevation: -2194.8 m * Recovery: 141.17 m * Campaign: Exp311 (Cascadia Margin Gas Hydrates) * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 28 cores; 205.5 m cored; 68.7 % recovered; 1 m drilled; 206.5 m penetrated
311-U1325C * Latitude: 48.645017 * Longitude: -126.983450 * Elevation: -2194.8 m * Recovery: 62.49 m * Campaign: Exp311 (Cascadia Margin Gas Hydrates) * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 115.5 m cored; 54.1 % recovered; 188.8 m drilled; 304.3 m penetrated
Datasets listed in this publication series
- Torres, ME; Tréhu, AM; Cespedes, N et al. (2008): (Appendix A) Gas hydrate abundance in samples of different lithologies of IODP Site 311-U1325. https://doi.org/10.1594/PANGAEA.716587
- Torres, ME; Tréhu, AM; Cespedes, N et al. (2008): (Appendix A) Gas hydrate anundance in samples of different lithologies of IODP Site 311-U1326. https://doi.org/10.1594/PANGAEA.716588
- Torres, ME; Tréhu, AM; Cespedes, N et al. (2008): (Table 2) Mineral composition of selected coarse-grained samples from IODP Site 311-U1325. https://doi.org/10.1594/PANGAEA.716585
- Torres, ME; Tréhu, AM; Cespedes, N et al. (2008): (Table 2) Mineral composition of selected coarse-grained samples from IODP Site 311-U1326. https://doi.org/10.1594/PANGAEA.716586