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九龙江口一岩心的重矿物组合
引用本文:洪辉亮,陈峰.九龙江口一岩心的重矿物组合[J].台湾海峡,2003,22(1):65-78.
作者姓名:洪辉亮  陈峰
作者单位:国家海洋局第三海洋研究所,福建,厦门,361005
基金项目:国家海洋局科技司资助项目“福建海陆相互作用研究”(A95 5 0 2 )
摘    要:本文详细地分析了九龙江口SD0 3岩心中自生矿物的成因 ,推断河口区在约1 0ka ,B .P .中历经了河流沉积、湖泊沉积和河口海湾沉积三种沉积环境 .在沉积环境演化过程中共形成了 1 0种重矿物组合 .

关 键 词:沉积物芯  重矿物  九龙江口
文章编号:1000-8160(2003)01-0065-14
修稿时间:2002年9月3日

Characteristics of heavy minerals in a core from Jiulongjiang Estuary
HONG Hui-liang,CHEN Feng.Characteristics of heavy minerals in a core from Jiulongjiang Estuary[J].Journal of Oceanography In Taiwan Strait,2003,22(1):65-78.
Authors:HONG Hui-liang  CHEN Feng
Abstract:In the paper, the genesis of the authigenic minerals in Core SD03 from Jiulongjiang Estuary were analyzed in detail. Based on the analytical results, it was inferred that the estuarine region had experienced three kinds of sedimentary environment, that is, river deposit, lacustrine deposit and estuary-bay deposit since about 10ka,B.P..Ten assemblages of heavy minerals had been formed in the evolution process of sedimentary environment.
Keywords:sediment core  heavy minerals  Jiulongjiang Estuary
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