Proceedings of the Ocean Drilling Program 1996
DOI: 10.2973/odp.proc.ir.164.101.1996
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Leg 164 Introduction

Abstract: The BSR pins the boundary at which three phases (hydrate-gaswater) coexist. Thus, in theory, if one knows the chemical composi-

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Cited by 2 publications
(5 citation statements)
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“…Despite a slight increase in calcium content at about 500 mbsf in the study site, the model shows a good match with the reference site's data. An additional source of calcium in the sediment and change in abundance of authigenic carbonate [51] could explain the difference between the model and data.…”
Section: Solid Phase and Pore Water Concentrationmentioning
confidence: 77%
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“…Despite a slight increase in calcium content at about 500 mbsf in the study site, the model shows a good match with the reference site's data. An additional source of calcium in the sediment and change in abundance of authigenic carbonate [51] could explain the difference between the model and data.…”
Section: Solid Phase and Pore Water Concentrationmentioning
confidence: 77%
“…After around three million years, when about 350 m of sediment accumulated, methane in pores below about 180 mbsf becomes supersaturated and gas hydrate forms. This depth is the upper edge of the zone with dispersed gas hydrate in sediments is described in the ODP report for site 997 [51]. As more methane is produced with time, more gas hydrate is formed.…”
Section: Methane Phase Behaviormentioning
confidence: 95%
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