2009年10月
Ni-Fe alloy possibly associated with reduced magmatic fluids in lower-crustal gabbro, IODP Hole U1309D, Atlantis Massif, Mid-Atlantic Ridge
JOURNAL OF MINERALOGICAL AND PETROLOGICAL SCIENCES
- ,
- ,
- ,
- 巻
- 104
- 号
- 5
- 開始ページ
- 290
- 終了ページ
- 295
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.2465/jmps.090622c
- 出版者・発行元
- JAPAN ASSOC MINERALOGICAL SCIENCES
A Ni-Fe alloy (Ni3.8Fe0.1Co0.1) was found in olivine-poor gabbro recovered from the Integrated Ocean Drilling Program (IODP) Hole U1309D, Atlantis Massif, 30 degrees N on the Mid-Atlantic Ridge. Ni-Fe alloys are one of the unique minerals formed during serpentinization; however, our finding establishes that Ni-Fe alloys are also formed in the gabbroic crust possibly associated with extremely reduced magmatic fluids. The occurrence of the Ni-Fe alloy suggests that oceanic lower-crustal gabbros as well as serpentinites may be potential reservoirs of abiogenic CH4.
- リンク情報
- ID情報
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- DOI : 10.2465/jmps.090622c
- ISSN : 1345-6296
- eISSN : 1349-3825
- CiNii Articles ID : 10025445045
- Web of Science ID : WOS:000271423400004