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Combination Distribution Characteristics and Corresponding Material Sources of Surface Clay Minerals in Beibu Gulf, China

机译:北武海湾地表粘土矿物的组合分布特征及相应材料来源

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Clay minerals are the main ingredients of the ocean floor sediments, which completely record a lot of geological information and have important meanings in the studies of source material, sedimentary environment, global climate change, sea-level fluctuation and ocean currents evolution. This paper studies composition and combination distribution characteristics of 312 surface clay mineral samples and makes the mineral mapping in Beibu gulf. The results show that the components of clay minerals in Beibu gulf are mainly mixed layer of illite and montmorillonite, kaolinite, chlorite and illite and each average content are 49.95%, 24.69%, 14.07% and 11.28%, respectively. According to combination and content of the clay minerals, the distribution areas of clay minerals in Beibu gulf can be divided into four divisions of 1, 2, 3 and 4 divisions. The differences of 4 divisions are closely related with the source area parent rocks and circulation.
机译:粘土矿物是海底沉积物的主要成分,全面记录了大量地质信息,在源材料,沉积环境,全球气候变化,海平波动和洋流演变中具有重要意义。本文研究了312种表面粘土矿物样品的组合物和组合分布特性,使北武海湾矿物映射。结果表明,北武海湾的粘土矿物的组分主要是伊尔菊和蒙脱石,高岭石,氯酸盐和伊利石的混合层,每个平均含量分别为49.95%,24.69%,14.07%和11.28%。根据粘土矿物的组合和含量,北武湾粘土矿物的分布区域可分为1,2,3和4个部门的四个分歧。 4个部门的差异与源区父母岩石和循环密切相关。

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