FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2083659886> ?p ?o ?g. }

• W2083659886 endingPage "112" @default.
• W2083659886 startingPage "99" @default.
• W2083659886 abstract "During the Second Gas Hydrate Drilling Expedition in the Ulleung Basin (UBGH2), pore fluids were collected from sites that sampled sediments from the continental slope to the basin center, and included locations within and outside seismic identified chimney like features. At five non-chimney sites established during the UBGH2, discrete excursions to low Cl− concentrations within the gas hydrate occurrence zone (GHOZ) are associated with water enriched in δD and δ18O, as expected from gas hydrate dissociation during core recovery. Estimates of gas hydrate saturation values (Sh) based on Cl− and δD values are in good agreement, and show that when gas hydrate occurs in discrete horizons or within strata-bound fractures throughout the GHOZ, it occupies 5–65% of the pore space. Fluids recovered from three sites characterized by seismic inferred chimneys show massive hydrate accumulation near the seafloor, accompanied by the formation of shallow Cl− rich brines with δD and δ18O values lower than seawater. Chemical and isotopic data from fluids sampled at all drilled sites reveal significant fluid freshening below the gas hydrate stability zone (GHSZ). The distribution of Cl−, K+ and δD indicate that the observed freshening is predominantly caused by clay mineral dehydration (illitization). Previously reported heat flow values in the center of the basin indicate that the sediments deeper than 800 mbsf (meter below seafloor) are warm enough to expect clay diagenesis with the onset of smectite-to-illite transformation. Source fluid temperatures >70 °C are confirmed through the use of Na+–Li+ and Mg2+–Li+ geothermometry. Based on these observations we propose the following scenario for the evolution of formation fluids in the Ulleung Basin where high formation temperatures and rapid sedimentation at the basin center, led to sediment compaction and clay dehydration reactions that result in fluid overpressures and associated fracturing of the formation. Sediment fractures and fluid (possible gas) migration in the chimney features, imaged in seismic records, are consistent with our postulated upward transport of fluids from >800 m depth though the GHSZ and to the seafloor." @default.
• W2083659886 created "2016-06-24" @default.
• W2083659886 creator A5029787617 @default.
• W2083659886 creator A5029812148 @default.
• W2083659886 creator A5053211960 @default.
• W2083659886 creator A5057596349 @default.
• W2083659886 creator A5061352140 @default.
• W2083659886 creator A5067286446 @default.
• W2083659886 creator A5074340353 @default.
• W2083659886 date "2013-11-01" @default.
• W2083659886 modified "2023-10-16" @default.
• W2083659886 title "Pore fluid chemistry from the Second Gas Hydrate Drilling Expedition in the Ulleung Basin (UBGH2): Source, mechanisms and consequences of fluid freshening in the central part of the Ulleung Basin, East Sea" @default.
• W2083659886 cites W1528825861 @default.
• W2083659886 cites W1538984895 @default.
• W2083659886 cites W1670936298 @default.
• W2083659886 cites W1963967489 @default.
• W2083659886 cites W1964783670 @default.
• W2083659886 cites W1965243262 @default.
• W2083659886 cites W1965985936 @default.
• W2083659886 cites W1969844110 @default.
• W2083659886 cites W1975177396 @default.
• W2083659886 cites W1986690700 @default.
• W2083659886 cites W1996249396 @default.
• W2083659886 cites W2002135408 @default.
• W2083659886 cites W2004358238 @default.
• W2083659886 cites W2006325241 @default.
• W2083659886 cites W2008680648 @default.
• W2083659886 cites W2009136031 @default.
• W2083659886 cites W2011655159 @default.
• W2083659886 cites W2012897228 @default.
• W2083659886 cites W2013002804 @default.
• W2083659886 cites W2021195792 @default.
• W2083659886 cites W2023576950 @default.
• W2083659886 cites W2024203177 @default.
• W2083659886 cites W2024961541 @default.
• W2083659886 cites W2032381462 @default.
• W2083659886 cites W2032808902 @default.
• W2083659886 cites W2036252653 @default.
• W2083659886 cites W2042293006 @default.
• W2083659886 cites W2043843042 @default.
• W2083659886 cites W2046518911 @default.
• W2083659886 cites W2047125934 @default.
• W2083659886 cites W2050545875 @default.
• W2083659886 cites W2050750841 @default.
• W2083659886 cites W2052694638 @default.
• W2083659886 cites W2053984269 @default.
• W2083659886 cites W2054458234 @default.
• W2083659886 cites W2056035247 @default.
• W2083659886 cites W2056185678 @default.
• W2083659886 cites W2056546792 @default.
• W2083659886 cites W2059724668 @default.
• W2083659886 cites W2062325960 @default.
• W2083659886 cites W2062693948 @default.
• W2083659886 cites W2063240745 @default.
• W2083659886 cites W2070432948 @default.
• W2083659886 cites W2071452315 @default.
• W2083659886 cites W2071744268 @default.
• W2083659886 cites W2075651860 @default.
• W2083659886 cites W2076836425 @default.
• W2083659886 cites W2082718517 @default.
• W2083659886 cites W2083959934 @default.
• W2083659886 cites W2085233966 @default.
• W2083659886 cites W2085519620 @default.
• W2083659886 cites W2089614630 @default.
• W2083659886 cites W2091783608 @default.
• W2083659886 cites W2091790668 @default.
• W2083659886 cites W2093143169 @default.
• W2083659886 cites W2093553279 @default.
• W2083659886 cites W2096432977 @default.
• W2083659886 cites W2105483052 @default.
• W2083659886 cites W2117056102 @default.
• W2083659886 cites W2121368895 @default.
• W2083659886 cites W2126724874 @default.
• W2083659886 cites W2131372785 @default.
• W2083659886 cites W2133828667 @default.
• W2083659886 cites W2150064090 @default.
• W2083659886 cites W2151261306 @default.
• W2083659886 cites W2159722785 @default.
• W2083659886 cites W2161130424 @default.
• W2083659886 cites W2185308876 @default.
• W2083659886 cites W2486845754 @default.
• W2083659886 cites W278856262 @default.
• W2083659886 doi "https://doi.org/10.1016/j.marpetgeo.2012.12.011" @default.
• W2083659886 hasPublicationYear "2013" @default.
• W2083659886 type Work @default.
• W2083659886 sameAs 2083659886 @default.
• W2083659886 citedByCount "49" @default.
• W2083659886 countsByYear W20836598862013 @default.
• W2083659886 countsByYear W20836598862014 @default.
• W2083659886 countsByYear W20836598862015 @default.
• W2083659886 countsByYear W20836598862016 @default.
• W2083659886 countsByYear W20836598862017 @default.
• W2083659886 countsByYear W20836598862018 @default.
• W2083659886 countsByYear W20836598862019 @default.
• W2083659886 countsByYear W20836598862020 @default.
• W2083659886 countsByYear W20836598862021 @default.
• W2083659886 countsByYear W20836598862022 @default.
• W2083659886 countsByYear W20836598862023 @default.

• next