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太平洋中部柱状沉积物中的自生矿物
引用本文:卢效珍.太平洋中部柱状沉积物中的自生矿物[J].海洋地质与第四纪地质,1992,12(1):67-72.
作者姓名:卢效珍
作者单位:地质矿产部海洋地质研究所
基金项目:国家自然科学基金资助项目49070263
摘    要:根据《海洋四号》861—881航次获得的岩心资料,通过对沉积物类型的观察,对其中的几种自生矿物钙十字沸石、蒙脱石、重晶石、微结核、非晶质SiO_2等矿物的成因和与沉积物类型的相关性进行了探讨。

关 键 词:沉积物  太平洋  自生矿物

AUTHIGENIC MINERALS IN A SEDIMENT COLUMN FROM THE CENTRAL PACIFIC
Lu Xiaozhen.AUTHIGENIC MINERALS IN A SEDIMENT COLUMN FROM THE CENTRAL PACIFIC[J].Marine Geology & Quaternary Geology,1992,12(1):67-72.
Authors:Lu Xiaozhen
Abstract:According to the sediment types of core obtained from Legs 861-881 of the "HY 4", the paper discussed the relationship between the formations of some authigenic minerals (phillipsite, montmorillonite, barite, micronodules, non-crystalline SiO2) and sediment types. Phillipsite and montmorillonite have been formed from volcanic materials by seawater solution, so these minerals have a close relation with palagic clay. Micronodules widely spread in the surface sediments. The author considers them as one of the authigenic ferromanganese minerals and barite as authigenic mineral. Its formation is related to siliceous bioclasts.
Keywords:Central Pacific    columnar sediment    authigenic mineral  
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