Possible biological origin of the 3.46 Ga Marble Bar banded iron chert, Pilbara Craton, Western Australia

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概要

• 論文の詳細を見る
• 2004-09-22

著者

• Suganuma Yusuke

  Ori. Uni. Tokyo

• Tazaki Kazue

  Kanazawa Univ. Ishikawa Jpn

• Nedachi Munetomo

  Kagoshima Uni. Sci.

• NIITSUMA Sachiko

  Tohoku Uni. Sci.

• HOASHI Masamichi

  Kagoshima Uni. Sci.

• Niitsuma S

  Tohoku Uni.sci.

• Tazaki Kazue

  Kanazawa Uni. Sci.

関連論文

• Sulfide mineralization in the 3.46 Ga Towers formation at the Salgash area, Pilbara Craton, Western Australia
• Possible biological origin of the 3.46 Ga Marble Bar banded iron chert, Pilbara Craton, Western Australia
• ロシア極東のヒンガン-オホーツク火山深成複合岩地帯における白亜紀中期のエピソディックな火成活動と錫の鉱化作用
• Structural Change and Cobalt Fixation in the Hydrothermally Synthesized Zeolite Phases from a Si-Al-Co Hydrous Oxide
• Synthesis and Phase Relationships between Smectite and Low-silica Zeolites(Teaching Clay Science,Proceedings of the 13^ International Clay Conference)

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