大庆石油地质与开发

2013, v.32;No.159(05) 7-11

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陆相河流—湖泊沉积体系准层序识别原理
IDENTIFYING PRINCIPLE OF THE SUBSEQUENCES FOR CONTINENTAL FLUVIAL-LACUSTRINE SEDIMENTARY SYSTEM

李延平,郝艳春,王庆考,闫议丹
LI Yanping,HAO Yanchun,WANG Qingkao,YAN Yidan

摘要(Abstract):

由于不存在海(湖)泛面这样的界面,相对于海(湖)相地层而言,陆相河流相准层序的识别变得更加困难。将河流相沉积与湖泊相沉积有机联系,通过河流—湖泊沉积体系沉积基准面的升降变化及沉积物供给速率的综合分析,认为存在多种类型的河湖相准层序,不仅存在向上水变浅的准层序,也存在向上水变深的准层序。用基准面升降旋回分析河湖相准层序具有重大意义,经分析指出河流相准层序是基准面短周期抬升沉积的结果,且下降半旋回有时不发育或遭受剥蚀,仅由基准面上升半旋回组成,重要的是不能简单套用一个完整的河湖相准层序存在上升半旋回和下降半旋回的模式,应当全面和具体分析。
Because of the lack of the marine(lacustrine) overflow interface,corresponding to the marine(lacustrine)-facies strata,the identification of fluvial facies parasequences is more difficulty.By means of the organic integration between the fluvial and lacustrine facies depositions and comprehensive analyses of the base-level changes and rate of sediments of fluvial-lacustrine depositional system,it is considered that there exist many kinds of fluvial and lacustrine facies parasequence i.e.not only the subsequences shallowed upward for the water,but the ones deepened upward.It is greatly significant for the sequence analyses with the help of lifting and droping baselevel cycles,and moreover the analyses show that the subsequences are resulted from the cyclic uplift sedimentation of the base level and furthermore are composed of the semicycles of the base-level uplift;it is important that the model with lifting and droping base-level semicycles is cannot simply and mechanically introduced within a complete fluvial and lacustrine facies parasequence;on the contrary,the comprehensive and specific analyses should be conducted.

关键词(KeyWords): 河流—湖泊沉积体系;准层序;基准面旋回;沉积物供给速率
fluvial-lacustrine depositional system;subsequence/parasequence;base-level cycle;the rate of sediment alimentation

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目“基于不可逆热力学和热流学原理的油藏复杂渗流机理研究”(51176023)

作者(Author): 李延平,郝艳春,王庆考,闫议丹
LI Yanping,HAO Yanchun,WANG Qingkao,YAN Yidan

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