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东太平洋多金属结核的叠层石包壳及其沉积环境意义
引用本文:韩喜球,方银霞,金翔龙,杨树锋.东太平洋多金属结核的叠层石包壳及其沉积环境意义[J].海洋学报,2000,22(5):73-81.
作者姓名:韩喜球  方银霞  金翔龙  杨树锋
作者单位:1.国家海洋局海底科学重点实验室, 杭州 310012;浙江大学地球科学系, 杭州 310027
基金项目:国家海洋局青年海洋科学基金资助项目(编号:96103).
摘    要:对东太平洋C-C区深海多金属结核的叠层石包壳、多金属结核的表面类型及其分布规律进行了详细研究和合理解释,认为叠层石的形态学特征既是建造叠层石的微生物种类差异的表现,也是环境水动力条件和溶解氧含量不同的反映,这些因素共同决定了多金属结核的表面类型,而南极底流是造成海底水体能量环境、氧化还原电位和微生物种类变化的根本原因.为多金属结核的分布规律和成矿预测提供科学依据.

关 键 词:多金属结核    分布规律    叠层石    南极底流    东太平洋
收稿时间:1999/3/12 0:00:00
修稿时间:1999-03-12

The stromatolite coats of manganese nodules from the East Pacific Ocean and their sedimentary environment significance
Han Xiqiu,Fang Yinxi,Jin Xianglong and Yang Shufeng.The stromatolite coats of manganese nodules from the East Pacific Ocean and their sedimentary environment significance[J].Acta Oceanologica Sinica (in Chinese),2000,22(5):73-81.
Authors:Han Xiqiu  Fang Yinxi  Jin Xianglong and Yang Shufeng
Institution:1.Key Lab of Submarine Geoscience of State Oceanic Administration, Hangzhou 310012;Zhejiang University, Hangzhou 3100272.Key Lab of Submarine Geoscience of State Oceanic Administration, Hangzhou 3100123.Zhejiang University, Hangzhou 310027
Abstract:The stromatolite coats, surface types and distribution rules of deep-sea manganese nodules are studied in detail and explained reasonably. It is suggested that microbes constructing stromatolite, water dynamic condition and oxygen content in water they decide the morphology characteristics of stromatolites and surface types of nodules. It is the Antarctic Bottom Water (AABW) that makes the change of energy environment of bottom water body and variety of microbes. The results provide scientific basis for manganese nodules distribution rule and metallogenic prognosis.
Keywords:Manganese nodules  distribution rule  stromatolite  Antarctic Bottom Water  Pacific Ocean
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