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OALib Journal期刊
ISSN: 2333-9721
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黑碳在开封古城黄泛地层沉积旋回划分中的指示意义
DOI: 10.11821/dlxb201505005, PP. 730-738
Keywords: 黄泛地层,沉积旋回,黑碳,代用指标,开封市
Abstract:
多次黄河泛滥使现今开封城市地面以下叠置数座古城,出现“城摞城”奇观。泛滥之后的城市重建等人类活动常常扰动正常的沉积层序,给粒度旋回划分带来巨大困难,因此需要寻找其他代用指标。分别在“城摞城”中心区（ZKsz）和郊区（ZKjm）获取25m连续岩芯,以10cm间隔分样;用激光粒度法结合筛分开展沉积物粒度分析,用Lim法（1996）测定黑碳含量,用小波分析划分沉积旋回。结果表明ZKjm岩芯的粒度旋回界线大多与黑碳旋回一致,表明黑碳含量可以作为划分沉积旋回的代用指标。ZKsz钻芯深度8.8~23.5m之间的地层,粒度旋回和黑碳旋回的数量及其界限基本相同;北宋以后地层（深度0.3~8.8m）的粒度旋回只有2个,而黑碳旋回有7个,表明黑碳含量适用于城市扰动地层的沉积旋回划分。
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