JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS16] [JJ] ガスハイドレートと地球環境・資源科学

2017年5月22日(月) 09:00 〜 10:30 A02 (東京ベイ幕張ホール)

コンビーナ:戸丸 仁(千葉大学理学部地球科学科)、八久保 晶弘(北見工業大学環境・エネルギー研究推進センター)、森田 澄人(国立研究開発法人 産業技術総合研究所 地質調査総合センター 地圏資源環境研究部門)、谷 篤史(神戸大学 大学院人間発達環境学研究科)、座長:戸丸 仁(千葉大学理学部地球科学科)

09:45 〜 10:00

[MIS16-04] Compositional and textural trends of microcrystalline dolomite found within massive gas hydrate in Joetsu Basin

*Glen Snyder1Ryo Matsumoto1Yoshihiro Kakizaki1Hitoshi Tomaru3Yohey Suzuki2 (1.Gas Hydrate Research Lab, Meiji Univeristy、2.Department of Earth and Planetary Science, University of Tokyo、3.Department of Earth Sciences, Chiba University)

キーワード:methane hydrate, dolomite, clathrate, Sea of Japan, Joetsu Basin

Recent exploratory drilling of massive gas hydrates in the Sea of Japan has revealed the presence of relatively pure, spherical growths of microcrystalline dolomite. The absence of sediment in association with the dolomite suggests that they were formed within hypersaline fluid inclusions which are situated inside of the hydrate itself. Stable isotope analysis of the dolomites suggests that the carbon isotopes are in equilibrium with the dissolved inorganic carbon in porewaters, while oxygen isotopes are consistent with the depletion of 18O during hydrate formation. Composition of the microcrystalline dolomite appears to be consistent with other hypersaline environments such as evaporative lagoons, where similar mineralization occurs, including characteristic pairing of sperical dolomite aggregates. XRD analysis indicates that other carbonates, such as aragonite and calcite, are completely absent and Mg/Ca ratios range from 0.76 to 1.04, with the highest ratios generally found in the deeper samples. SEM-EDS analysis of sections of polished grains indicates that the grains have hollow cores, and are uniform in Mg/Ca ratios from the outer portion to the inner portion. Anomalous Mg/Ca ratios in shallow hydrate may indicate areas where shallow hydrate exposures have been released from the seafloor, followed by renewed shallow hydrate growth.
Research was carried out on Expedition PS15 onboard the RV Poseidon. This study was conducted under the commission from AIST as a part of the methane hydrate research project funded by METI (the Ministry of Economy, Trade and Industry, Japan).