Methane-hydrate Occurrence and Saturation Confirmed from Core Samples, Eastern Nankai Trough, Japan
Tetsuya Fujii, Masaru Nakamizu, Yoshihiro Tsuji, Takatoshi Namikawa, Toshiharu Okui, Masayuki Kawasaki, Koji Ochiai, Mizue Nishimura, Osamu Takano, 2009. "Methane-hydrate Occurrence and Saturation Confirmed from Core Samples, Eastern Nankai Trough, Japan", Natural Gas Hydrates—Energy Resource Potential and Associated Geologic Hazards, T. Collett, A. Johnson, C. Knapp, R. Boswell
Download citation file:
The Ministry of Economy, Trade and Industry, Japan, drilled the Tokai-oki to Kumano-nada exploratory test wells to obtain data for understanding the occurrence of methane hydrate and estimating the volume of gas stored as methane hydrates in the Nankai Trough, offshore central Japan. In this project, we conducted logging while drilling at 16 sites, coring at four sites, wireline logging at two sites, and long-term monitoring of formation temperature at a single site.
Massive or layered methane hydrates within muddy layers were recovered at sites 1 and 2 by drilling with a conventional wireline-core system. The methane-hydrate-bearing sediments in these sites are a combination of clay and silt, which is not commonly considered a favorable host sediment for hydrate formation; however, a significant decrease in core temperature was recorded within intervals of layered hydrates.
Pore-space-type hydrates were identified in sand layers from sites 4 and 13 within 82 m (269 ft) of recovered core using a pressure temperature core sampler (PTCS). Sediments within this core are mainly very fine- to fine-grained turbidite sand layers of several centimeters (inches) to 1.5 m (5 ft) in thickness (average of 20–40 cm [8–16 in.]). Core-temperature measurements and the relationship between well-log resistivity and grain-size distribution indicate that methane hydrate is concentrated within layers of coarse-grained sand. We identify five sedimentary facieson the basis of alithological column created from core and well-log data at sites 4 and 13. Facies analysis indicates that the depositional environment in hydrate-bearing zones at sites 4 and 13 consisted of distributary channels to distal lobes within a submarine-fan system. Shipboard hydrate dissociation tests on PTCS cores reveal that average hydrate saturation in the cored sand layers ranged from 55 to 68%, with the average sediment porosities ranging from 39 to 41%, based on the analysis of both well-log and core measurements.
Figures & Tables
In September 2004, the American Association of Petroleum Geologists (AAPG) convened a Hedberg Research Conference in Vancouver, British Columbia, Canada titled "Natural Gas Hydrates: Energy Resource Potential and Associated Geologic Hazards." As a continuation of the Hedberg Research Conference in Vancouver, the conveners of the conference and the editors of this Memoir have worked with more than 150 authors and coauthors to prepare this Memoir on gas hydrates. This publication follows the goals of the Hedberg conference; however, the contents of this Memoir were expanded to include all aspects of gas hydrates in nature. This Memoir contains 39 individual contributions, ranging from long topical summaries to shorter focused research papers. This Memoir has been published in two parts, with digital versions of all the complete research papers included on the enclosed CD. The hardcopy portion of the Memoir includes abstracts and several key figures for each of the contributions along with a complete copy of a gas hydrate technical review. The digital portion of this Memoir has been organized into a series of topical sections consisting of review articles, marine gas hydrate papers, and gas hydrate laboratory and modeling studies. Because of the rapidly emerging worldwide interest in gas hydrates, this comprehensive treatise on the geology of gas hydrates will be valuable to both the gas hydrate research community and exploration/development geologists working in arctic and deep marine environments.