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氧化还原敏感微量元素地球化学揭示 白垩纪松辽古湖间歇性水体分层: 来自边缘相青山口组青一二段的证据
({{custom_author.role_cn}}), {{javascript:window.custom_author_cn_index++;}}Redox-sensitive trace element geochemistry reveals intermittent water column stratification in Cretaceous Songliao Paleo-lake: evidence from marginal facies of members 1 and 2 of Qingshankou Formation
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