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Distributional Feature of Detrital Minerals in the Superficial Sediment of South Yellow Sea

机译:南黄海表层沉积物中碎屑矿物的分布特征

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摘要

The composition of detrital minerals with grades of 0.063 - 0.25 mm in the superficial sediment of South Yellow Sea is mainly studied in the paper. The research result shows that the minerals can be divided into more than fifty sorts. The light minerals are mainly feldspar, quartz, mica, etc. The heavy minerals are mainly composed of amphibole, epidote, mica, autogeny pyrite, magnetite, hematite, garnet, zircon and so on, which mainly distribute in the sediments of silty clay and lutaceous silt. According to the content and distribution of the main minerals, the research area is divided into five miHeral combination provinces. The assembled types of minerals in every province have close relationship with its hydrodynamic conditions and sedimentary environment. And the sorts of detrital minerals also show that the detrital substances in the sedimentary areas mainly originate from the drainage areas of rivers, bedrock weathering, and transformed sediment, etc.
机译:本文主要研究了南黄海表层沉积物中0.063-0.25 mm品位的碎屑矿物成分。研究结果表明,矿物质可以分为五十多种。轻矿物主要为长石,石英,云母等。重矿物主要为闪石,附子,云母,自生黄铁矿,磁铁矿,赤铁矿,石榴石,锆石等,主要分布在粉质黏土和黄土粉砂。根据主要矿物质的含量和分布,将研究区域分为五个矿物组合省份。每个省的矿物的聚集类型与其水动力条件和沉积环境密切相关。各种碎屑矿物也表明,沉积区的碎屑物质主要来源于河流流域,基岩风化和沉积物转化等。

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