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基于磁化率与色度残差耦合分析的松辽盆地青一段土伦期—康尼亚克期古气候阶段性演化
({{custom_author.role_cn}}), {{javascript:window.custom_author_cn_index++;}}Turonian --Coniacian staged paleoclimate evolution of Member 1 of Qingshankou Formation in Songliao Basin based on coupled magnetic susceptibility and color-residual analysis
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