A DIVISION OF CONTINENTAL SEQUENCE STRATIGRAPHY AND THE IDENTIFICATION OF ITS INTERFACE WITH HIGH RESOLUTION CORE ANALYSES AND WELL-LOGGING
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摘要: 本文提出了陆相盆地中存在有3种叠加方式4种类型的准层序组,即Ⅰ、Ⅱ型加积准层序组,进积准层序组及退积准层序组;论证了陆相层序地层学4分方案的可行性,并建议使用湖泊枯水体系域(LDST)、湖泊扩展体系域(LEST)、湖泊丰水体系域(LF-ST)以及湖泊萎缩体系域(LWST)等术语;总结出了层序界面的4种类型—区域角度不整合面、火山-局部不整合面、湖盆萎缩最大暴露冲刷面及区域性超覆不整合面;指出了生物富集层和油页岩的底界面以及低能量细碎屑与下伏钙质团决和滑塌构造层之间的界面是准层序界面,而规模较大的水深突增岩相界面、较厚的滑塌构造层顶界面以及颜色突然变深的较厚泥质沉积物分界面可作为准层序界面。Abstract: In a continental basin there are four types of parasequence with three patterns of overlappings, i. e. Ⅰ,Ⅱ typed aggradational parasequence set, aggressive parasequence set and regressive parasequence set I thereby the paper discussed the feasibility of the four-division plan for continental sequence stratigraphy, and proposed the terms of lacustrine dry system tract (LDST), lacustrine extend system tract (LEST), and lacustrine wrinkle system tract (LWST). It is summarized that sequence interfaces may be clarified into four types: regional angled unconformable contact, vocano-local unconformable contact, maximum exposural flushing surface of lacustrine wrinkle and regional onlapping unconformable contact, etc. Finally the paper suggested the followings may be considered as interfaces of parasequence: the bottom interface of oil-shale and organic-rich layer; the interface between the low-energy fine clastics and underlying calcareous concretion and slump structural layer, the rock facial plane characterized by a large scale abrupt increase of water depth I the top interface of a thick slump structural layer;and a thick muddy sedimental interface characterized by an abrupt color mutation.
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[1] 魏魁生.徐怀大.华北典型箕状盆地层序地层学模式及油气赋存关系.地球科学,1993.18(2):141-149 [2] 解习农,李思田.陆相盆地层序地层研究特点,地质科技情报,1993,12(1):22-26 [3] 王东坡,刘招君,刘立.松辽盆地演化与海平面升降.北京:地质出版社,1994 [4] 薛良清.层序地层学研究现状、方法与前景.石油勘探与开发,1995 22(5):8-12 [5] Embry A F. Transgressive-regressive (T-R) sequence analysis of the Jurassic succession of the Sverdrup Basin, Canadian Aretic Archipelago. Can. J. Earth. Sci. 1993,30:301-320
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