贵州瓮安磷矿岩石学及沉积序列研究
Research on petrology and sedimentary sequences of phosphorites in Weng'an,Guizhou
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摘要: 对贵州瓮安含磷岩系的岩石学特征及其与沉积环境的联系进行了研究,分析了各层位磷块岩的结构构造、物质组分在剖面上的变化。其类型为碳酸盐岩型含磷岩系,磷块岩的各种结构类型显示了不同的成因及沉积环境的差异。对瓮安穿岩洞剖面进行沉积序列的划分,将陡山沱组含磷岩系划分为6个向上变浅的沉积序列。在海平面不断升降的背景下,富磷海水伴随着上升洋流节律性地涌入浅水区并发生沉积作用,具有纵向上的旋回性及多个序列的特点。Abstract: The Petrology Characteristics of phosphatic series inWeng'an and its connection to the sedimentary environments were discussed.And the diversification in profile of the characteristics of structure as well as material components of phosphorites in each layer have been studied too.The type was carbonatite phosphatic series, varieties of structural types of phosphorite showed different causes and different sedimentary environments. With undertaking the partition of sequence stratigraphic on the Chuan Yan-dong section inWeng'an,the strata of the Doushantuo Formation may be grouped into six shallowing-upward depositional sequences.Because the sealevel's rising and falling constantly,the plentiful phosphatic seawater carried by upwelling oceanic currents entered into the shallow marine areas rhythmicly and deposited.The sediments had the feature of cyclic in the vertical and multiple sequential.
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