Art

J-GLOBAL ID：200902138719740379   Reference number：02A0672322

Negative Ce Anomaly in the Indian Banded Iron Formations: Evidence for the Emergence of Oxygenated Deep-Sea at 2.9~2.7 Ga.

インドの縞状鉄鉱層中の負のCe異常 29~27億年前の酸化的深海の出現の証拠

Author (3)： KATO Y (Univ. Tokyo, Tokyo, JPN) ,  KANO T (Yamaguchi Univ., Yamaguchi, JPN) ,  KUNUGIZA K (Toyama Univ., Toyama, JPN)
Material： Resource Geology  (Resour Geol)
Volume： 52  Issue： 2  Page： 101-110  Publication year： 2002 
JST Material Number： G0131A  ISSN： 1344-1698  CODEN： REGEFQ  Document type： Article
Article type： 原著論文  Country of issue： Japan (JPN)  Language： ENGLISH (EN)

Thesaurus term： Archeozoic Era ,...
Semi thesaurus term： Archaean ,...

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JST classification (2)： Geochemistry of lithosphere in general  (DD01041C) ,  Metallic ore deposit  (DE09030H)

Reference (48)：

• ALIBERT, C. Rare earth element and neodymium isotopic compositions of the banded iron-formations and associated shales from Hamersley, western Australia. Geochim. Cosmochim. Acta. 1993, 57, 187-204
• BALAKRISHNAN, S. U-Pb ages for zircon and titanite from the Ramagiri area, southern India: evidence for accretionary origin of the eastern Dharwar Craton during the Late Archean. Jour. Geol. 1999, 107, 69-86
• BENDER, M. Geochemistry of three cores from the East Pacific Rise. Earth Planet. Sci. Lett. 1971, 12, 425-433
• BINNS, R. A. Hydrothermal oxide and gold-rich sulfate deposits of Franklin seamount, western Woodlark Basin, Papua New Guinea. Econ. Geol. 1993, 88, 2122-2153
• BYRNE, R. H. Rare earth element scavenging in seawater. Geochim. Cosmochim. Acta. 1990, 54, 2645-2656

Terms in the title (6)： インド ,  縞状鉄鉱層 ,  Ce ,  酸化 ,  深海 ,  証拠