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中心式喷发火山岩三维地震刻画方法 被引量:3

Volcanic 3-D Seismic Characterization of Central Eruption Style
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摘要 基于火山岩溢流相的高连续强振幅和火山通道相的低连续弱振幅2种截然相反的地震反射特征,提出了振幅-方差体地震属性分级-拾取-融合技术刻画火山岩时空展布的解释新方法。具体流程是通过振幅分级显示,拾取强振幅刻画溢流相的空间展布;通过方差体分级,拾取高值部分刻画火山通道相的空间展布;最后将二者融合显示。通过渤海湾盆地莱州湾凹陷垦利6-A区块实例分析,表明该方法可以直观、有效地刻画火山岩的三维时空展布特征。研究成果有助于火山岩的三维刻画,可以广泛运用于与火山岩相关的含油气盆地。 Based on the contrast of seismic reflections between volcanic channel facies (high continuity and strong seismic amplitude) and overflow facies (low continuity and weak seismic amplitude), the new meth- od of seismic amplitude and variance cube thresholding, pickup, and merge display is built to describe the spatial and temporal distribution of volcanics and eruption phases. The workflow is characterized by: (1) Describing spatial distribution of volcanic channel facies through seismic amplitude thresholding display and strong amplitude pickup; (2) Characterizing spatial distribution of volcanic overflow facies using vari- ance cube thresholding display and high value pickup; (3) Merging display of volcanic channel and over- flow facies. The applicability of this method has been validated in the Kenli6-A block of Laizhouwan Sag, Bohai Bay Basin, showing one high effective method to characterize volcanic 3-D distribution. The method built in the paper should serve as a useful reference for volcanic 3-D seismic characterization and be used extensively in the volcanic-related basin.
出处 《地质科技情报》 CAS CSCD 北大核心 2015年第1期185-190,共6页 Geological Science and Technology Information
基金 国家科技重大专项"近海大中型油气田形成条件与分布"(2011ZX05023-006) 教育部科技项目霍英东教育基金会资助项目(132020)
关键词 火山岩3-D刻画 振幅分级-拾取 方差体分级-拾取 融合显示 volcanic 3-D characterization seismic amplitude thresholding and pickup variance cubethresholding and pickup merge display
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