长江荆江段现代沉积研究
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CoNTEMPoRARY DEPoSⅡ1s OF THE JINGJIANG RⅣER REACH oF THE YANGTZE RⅣER
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    摘要:

    本文系统地报道了长江荆江段河流沉积学最新研究成果。荆江段发育众多 的不同类型的沉积砂体,包括了河流沉积所有微地貌单元,计有:心滩、江心洲、 高弯曲流边滩、低弯曲流边滩、分流河口三角滩、决口扇、牛轭湖等。系统地阐述 了沉积物碎屑成分、化学成分和微量元素、粘土矿物及有机碳、岩石相类型及组 合等特征。对于五种占主导地位的沉积砂体,结合水槽实验,全面分析了其沉积 过程和加积规律以及建筑结构要素,根据砂体不同单元的沉积特点,进一步划 分了微相带,并提出了沉积作用模式。

    Abstract:

    The paper systematically reports the latest research results of the fluvial deposits of the Jingjiang river reach of the Yangtze River.There are numerous sedimentary sand hodies of dif- ferent types in this reach,including all the microtopographic units of fluvial deposits,for exam- ple,channel bars,eyots,high and low meander point bars,distributary mouth cuspate bars, crevasse splays and bayous.The detrital composition,chemical composition,trace elements,clay minerals and Qrganic carbon in the deposits and rock facies types and assemblages are discussed systematically.On that basis combined with flume experiments,the process of deposition,regu— larity of accretion and architectural elements of five dominant types of sandbody are analyzed. According to the sedimentary feature of different units of the sandbody,microfacies zones are distinguished and sedimentary models are advanced.

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曹跃华,张春生,刘忠保,赖志云.1996.长江荆江段现代沉积研究[J].地质论评,42(sup):137-146,[DOI].
cao yuehua, zhang chunsheng, liu zhongbao, lai zhiyun.1996. CoNTEMPoRARY DEPoSⅡ1s OF THE JINGJIANG RⅣER REACH oF THE YANGTZE RⅣER[J]. Geological Review,42(sup):137-146.

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