王庆同,赵吉圆,王海根,等. 渤海海峡西南部海底沉积物重矿物组成与物源[J]. 海洋地质前沿,2023,39(6):22-31. DOI: 10.16028/j.1009-2722.2022.259
    引用本文: 王庆同,赵吉圆,王海根,等. 渤海海峡西南部海底沉积物重矿物组成与物源[J]. 海洋地质前沿,2023,39(6):22-31. DOI: 10.16028/j.1009-2722.2022.259
    WANG Qingtong, ZHAO Jiyuan, WANG Haigen, et al. Composition and provenance of heavy minerals in surface sediments in the southwestern Bohai Strait[J]. Marine Geology Frontiers, 2023, 39(6): 22-31. DOI: 10.16028/j.1009-2722.2022.259
    Citation: WANG Qingtong, ZHAO Jiyuan, WANG Haigen, et al. Composition and provenance of heavy minerals in surface sediments in the southwestern Bohai Strait[J]. Marine Geology Frontiers, 2023, 39(6): 22-31. DOI: 10.16028/j.1009-2722.2022.259

    渤海海峡西南部海底沉积物重矿物组成与物源

    Composition and provenance of heavy minerals in surface sediments in the southwestern Bohai Strait

    • 摘要: 渤海海峡是黄渤海交接地带,周边岛屿散布,地形条件复杂,沉积物类型丰富,是研究海洋动力系统的热点地区之一。通过对32个表层沉积物的重矿物分析,研究了渤海海峡西南部海域的重矿物组成、分布和物质来源。结果表明,研究区矿物组合为普通角闪石-绿帘石-黑云母-褐帘石,可将其划分成3个矿物分区。庙岛群岛矿物区(Ⅰ区)为普通角闪石-绿帘石-钛铁矿-石榴子石矿物组合,物质主要来自庙岛群岛岛屿冲刷物;中部矿物区(Ⅱ区)为普通角闪石-绿帘石-黑云母矿物组合,主要来源于黄河物质;西部矿物区(Ⅲ区)为普通角闪石-绿帘石-黑云母-褐帘石矿物组合,是黄河物质、山东半岛及庙岛群岛岛屿冲刷物的混合物。不同来源的物质在海洋动力综合作用下进行搬运、沉积,最终导致了矿物组合分区之间的物质差异。

       

      Abstract: The Bohai Strait is the channel connecting the Bohai Sea to the Yellow Sea for material and energy exchange, which has complex topographical conditions and abundant sediment types. It is one of the hotspots to study the marine dynamic systems. Thirty-two surface sediments collected in 2021 from the southwestern Bohai Strait were analyzed on the heavy minerals in terms of their composition, distribution, and provenance. Results show that the mineral assemblages were characterized by hornblende-epidote-biotite-orthite and they were from three mineral assemblages/provinces: the Miaodao Islands (I) has a hornblende-epidote-ilmenite-garnet assemblage derived mainly from the scours of the Miaodao Islands, the Central Zone (II) has a hornblende-epidote-biotite assemblage largely attributed to the Yellow River materials, and the Western Zone (III) has a hornblende-epidote-biotite-orthite assemblage that is a mixture of the Yellow River sediments and scours from the Shandong Peninsula and Miaodao Islands. Materials from different sources were transported and deposited under overall marine forces, which eventually resulted in the differences in mineral assemblages of the area.

       

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