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Characteristics of heavy minerals composition and distribution in surface sediment from the Xinghua Bay of Fujian, China

机译:福建兴化湾表层沉积物中重矿物的组成与分布特征

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摘要

The composition, assemblage and distribution characteristics of heavy minerals from 63 to 125 μm grain sizes in surface sediment from the Xinghua Bay (17 stations) are studied. The matter source of silt and the relationship between heavy minerals and sedimentary environment are also discussed. The results show that there are 37 kinds of heavy minerals and the average content of them is 12.08%, which exceeds 6% compared with the Meizhou Bay (5.67%). The dominant minerals are magnetite, hornblende, epidote, ilmenite, hematite, limonite, zircon and so on. Mineral kinds reveal that the sources of silt in this bay are the fluvial input and eroded products of bedrock in circumjacent land and islands of the Xinghua Bay. However, the matter source from outside this bay is less. Four mineral assemblage zones can be divided based on heavy mineral contents and distribution characteristics in the Xinghua Bay, which are not only influenced by matter source, but also controlled by hydrodynamic condition and sedimentary environment in the Xinghua Bay.
机译:研究了兴化湾(17个站)表层沉积物中63〜125μm粒径重矿物的组成,组成和分布特征。还讨论了粉砂的物质来源以及重矿物与沉积环境之间的关系。结果表明,重矿物37种,平均含量为12.08%,比湄洲湾的5.67%高出6%。主要的矿物是磁铁矿,角闪石,附子,钛铁矿,赤铁矿,褐铁矿,锆石等。矿物种类表明,该海湾的淤泥来源是兴化湾周围陆地和岛屿的河床输入和基岩的侵蚀产物。但是,来自该海湾外部的物质来源较少。根据兴化湾的重矿物含量和分布特征,可将其划分为四个矿物组合区,既受物质来源的影响,又受兴化湾水动力条件和沉积环境的控制。

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