摘要
以成因矿物学的理论和方法,围绕太平洋三区四地海底热液硫化物和烟囱物中黄铁矿为主线的形态标型(扫描电镜)、矿物标型(粉晶X射线衍射法)及矿物组合,揭示了黄铁矿及伴生矿物在不同热液喷发类型中的标型特征,并由此反证了不同标型特征的热液矿物与热液喷发环境相互依存的紧密关系。
In this paper, the theory and method of genetic mineralogy are used to reveal the standard type characteristics of pyrite and its associated minerals of different hydrothermal eruption types, and the hydrothermal and chimney sulfide samples were collected from three areas of the Pacific Ocean. The morphological standard types(scanning electron microscope), mineral standard types(powdered crystal X-ray diffraction method) and mineral assemblage of pyrite and associated minerals in these samples are discussed to confirm that the hydrothermal minerals with different standard type characteristics have close relations to the hydrothermal eruption environments of these minerals.
出处
《海洋科学进展》
CAS
CSCD
北大核心
2005年第1期27-34,共8页
Advances in Marine Science
基金
国家自然科学基金项目--海底热液化物中黄铁矿的标型特征及其对比研究(498760160)
关键词
太平洋
热液硫化物
黄铁矿
标型特征
Pacific Ocean
hydrothermal sulfide
pyrite
standard type characteristics