Department of Earth Science and Astronomy, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo 153-8902, Japan;
Department of Earth Science and Astronomy, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo 153-8902, Japan;
Department of Chemistry, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo 153-8902, Japan;
Department of Chemistry, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo 153-8902, Japan;
Department of Chemistry, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro, Tokyo 153-8902, Japan;
moessbauer spectroscopy; iron; deep-sea chert; redox; toarcian;
机译:〜(57)Fe莫斯鲍尔分析三叠纪-下侏罗统深海cher石:跨越三叠纪-侏罗纪边界和Toarcian海洋缺氧事件的古-氧化还原历史
机译:57 sup> FeMössbauer对上三叠纪-下侏罗统深cher石的分析:跨越三叠纪-侏罗纪边界和Toarcian海洋缺氧事件的古氧化还原历史
机译:〜(57)Fe Moessbauer光谱分析的深海浮游硅质cher石:二次蚀变对古-氧化还原评价的影响
机译:〜(57)FE Moessbauer对侏罗纪深海燧石的射门分析:古雷诺历史,跨越三叠纪 - 侏罗纪边界和Toarcian海洋缺氧事件
机译:在三叠纪-侏罗纪灭绝的时候,三叠纪上层珊瑚礁生态系统的古生态及其消亡是潜在的海洋酸化事件。
机译:在Toarcian海洋缺氧事件发生之前海平面急剧下降:对早期侏罗纪气候和碳循环的影响
机译:深海深度古生代古生代的氧化还原条件:57FE深海壁画燧石的Moessbauer光谱研究