岩性油气藏 ›› 2012, Vol. 24 ›› Issue (1): 712.doi: 10.3969/j.issn.1673-8926.2012.01.002
刘化清,卫平生,李相博,洪忠,牛海青,张兆辉
LIU Huaqing, WEI Pingsheng, LI Xiangbo, HONG Zhong, NIU Haiqing, ZHANG Zhaohui
摘要:
地震沉积学自创建以来,关于其理论基础和理论创新方面的讨论较少。文中在分析前人研究成果 的基础上,结合勘探实践,认为作为一门利用地震资料研究沉积岩及其形成过程的新兴边缘学科,地震沉 积学以现代沉积学和地球物理学的基本原理为指导,其理论创新主要体现在:①地震数据体揭示沉积体 的平面几何形态比垂向形态更加容易;②地震反射同相轴具有穿时性,地震数据的频率控制了同相轴的 倾角和内部反射结构。同时认为这2 点是地震沉积学核心思想(发掘地震数据体中等时沉积界面上的地 震地貌信息来研究沉积相、沉积结构和沉积演化)的重要依据。
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