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摘要: 概述 砂体成因的研究是项综合性工作,用于成因研究的指标有生物的、化学的和物理的。砂岩粒度分布是一个重要的物理标志。
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[1] H.布拉特等:沉积岩成因科学出版社1978. [2] Visher G, S.J:Grain size distributions and depositional processes sed.Petrology.Vol.39.P.1074-1106 [3] Gtaister R.P.and Nelson H.W.Grainsize distributions, an aid in facies identification Bull.Can Petroleum Geology Vol.22,, No.3.P.203-290. [4] Passega R; Texture as characteristic of elastic deposition Bull.Am.Assoc,Petroteum Geologists Vol.41.No.9.P.1952-1984. [5] Holmes D.W,,Oliver.T.A, Source and deposilional environments of the moose channel formatron northwest Territories Bull.Can.Petroteum Geology Vol.21 P.435-478. [6] Passega.R.Sigrificance of CM diagrams of sediments deposited by suspensions-sedimentology 1977.Vol.24 P.723-733.
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