福建兴化湾表层沉积物中重矿物组分及其分布特征
The characteristics of heavy minerals composition and distribution in surface sediment from the Xinghua Bay of Fujian
-
摘要: 对兴化湾17个站位表层沉积物中63~125μm粒级重矿物组分、含量、组合及分布特征进行了分析研究,并探讨了泥沙物质来源及重矿物与沉积环境的关系.结果表明,兴化湾重矿物平均含量(质量分数)为12.08%,高出其邻近的湄州湾(5.67%)6个百分点;重矿物共计37种,以磁铁矿、角闪石、绿帘石、钛铁矿、赤铁矿、褐铁矿、锆石为主.矿物种类揭示该海湾的泥沙主要来源于湾顶河流输入和周边陆域及湾内岛屿基岩风化侵蚀产物,而湾口以外海域的输入物质较少;依据主要重矿物含量和分布特征,将兴化湾划分为4个矿物组合区,各区重矿物组合类型不仅与物质来源有关,而且受水动力条件和沉积环境制约.Abstract: The composition,assemblage and distribution characteristics of heavy minerals from 63 to 125 μm grainsizes in surface sediment from the Xinghua Bay (17 stations) are studied.And then,matter source of silt and relationship of heavy minerals with sedimentary environment are 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 silt in this bay mainly comes from fluvial input and eroded products of bedrock in circumjacent land and islands of the Xinghua Bay,however,the matter origin from outside area of this bay is less.The Xinghua Bay can be divided into 4 mineral assemblage zones based on heavy mineral contents and distribution characteristics,which are not only related to matter source,but also controlled by hydrodynamic condition and sedimentary environment in the Xinghua Bay.
-
Key words:
- heavy minerals /
- mineral assemblage /
- sedimentary environment /
- Xinghua Bay of Fujian /
-
BAYHAN E,ERGIN M,TEMEL A,et al.Sedimentology and mineralogy of surficial bottom deposits from the AegeanCanakkale-Marmara transition (Eastern Mediterranean):effects of marine and terrestrial factors [J].Marine Geology,2001,175:297-315. DIEKMANN B,KUHN G.Provenance and dispersal of glacial-marine surface sediments in the Weddell Sea and adjoining areas,Antarctica:ice-rafting versus current transport [J].Marine Geology,1999,158(1-4):209-231. SCHAFER J,DORR W.Heavy mineral analysis and typology of detrital zircons:a new approach to provenance study (Saxothuringian Flysch,Germany) [J].Journal of Sedimentary Research,1997,67(3):451-461. 石学法.海洋沉积环境研究的基本思想[J].海洋科学,1992,16(2):22-24. 陈丽蓉,栾作峰,郑铁民,等.渤海沉积物中的矿物组合及其分布特征的研究[J].海洋与湖沼,1980,11(1):46-64. 陈华胄.湄洲湾重矿物组合及分布特征[J].台湾海峡,1992,11(3):211-217. 陈华胄.台湾海峡表层沉积物中重矿物特征及其物质来源[J].台湾海峡,1993,12(2):136-143. 洪辉亮.厦门港重矿物研究[J].海洋学报,1993,15(3):49-62. 徐茂泉.九龙江口表层沉积物中碎屑矿物的研究[J].厦门大学学报(自然科学版),1994,33(5):675-680. 徐茂泉.闽江口表层沉积物中碎屑矿物的研究[J].厦门大学学报(自然科学版),1995,34(3):466-469. 徐茂泉.闽江口表层沉积物中0.125~0.250 mm粒级重矿物的分布与组合特征[J].台湾海峡,1996,15(3):229-234. 徐茂泉,沈兴兴,李超,等.海沧邻近海域表层沉积物中重矿物研究[J].海洋科学,2003,27(11):53-58. 阮金山,许翠娅,罗冬莲.福建兴化湾海水、沉积物及水产生物体内重金属的分析与评价[J].热带海洋,2002,19(1):52-57. 李孟国.兴化湾水文泥沙特征分析[J].水道港口,2001,22(4):156-159. 柯文荣.兴化湾建设大型深水航道的可行性研究[J].台湾海峡,2002,21(3):360-366. 金秉福,林振宏,季福武,等.东海外陆架Q43岩心末次冰期矿物学特征及其古环境意义[J].海洋学报,2003,25(增刊2):177-185. 杨群慧,张富元,林振宏,等.南海东北部晚更新世以来沉积环境演变的矿物-地球化学记录[J].海洋学报,2004,26(2):72-80. 李荣冠,江锦祥,蔡尔西,等.兴化湾大型底栖生物生态研究[J].海洋学报,1999,21(5):101-109. 福建省地质矿产局.福建省区域地质志[M].北京:地质出版社,1985.
计量
- 文章访问数: 714
- HTML全文浏览量: 21
- PDF下载量: 1155
- 被引次数: 0