吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (3): 626-639.doi: 10.13278/j.cnki.jjuese.20170323
张冠杰, 方石, 张新荣, 高先超, 沈伟
Zhang Guanjie, Fang Shi, Zhang Xinrong, Gao Xianchao, Shen Wei
摘要： 水进砂在水进过程中被侵蚀、淘洗、搬运，其沉积特征明显有别于背景砂体，表现出明显的穿时性。水进砂的发现完善了层序地层学理论，同时它在油气储存运移、原油物性预测以及油气勘探开发方面也有重要价值。本文从砂体的性质、来源、所处背景砂体的环境以及发育的构造条件4个方面对水进砂进行了分类，并总结了具代表性的形成机制：地层响应模型、水进型三角洲模型、海侵—海退模型、水动力模型、下切谷模型和潮汐改造的沙脊模型。近年来，相关学者在传统沉积学的基础上，又运用水动力学、遗迹学和不整合面识别等比较独特的方法对水进砂进行了研究。未来水进砂的研究工作将不再局限于海相砂体中，同时将运用更精细的方法对水进砂进行更深入的研究。
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