摘要
简要回顾了海底喷气成因热水沉积成矿理论发展的3个阶段,概述了海底喷气矿床分类、成矿模式、成矿规律等方面的研究现状。结合国内外新动向,提出要从整体沉积成矿盆地的岩石圈动力学成矿、地史成矿、流体动力学成矿和生物成矿等方面深入进行研究,以提高对海底喷气矿床综合预测和定量评阶的能力。
Three historical stages of the theory of exhalative hydrothermal sedimentary ore-forming process on the sea floor are briefly reviewed in this paper. The state of the art, including classification, deposit modeling, and regularity of ore-forming process, are also summarized. To advance the theory and improve forecast and quantitative evaluation of reserves, studies relating to lithosphere dynamics, historical geology, fluid dynamics and biology should be emphasized in sedimentary basin analysis.
出处
《地质科技情报》
CAS
CSCD
北大核心
1993年第2期83-86,共4页
Geological Science and Technology Information
关键词
热水
沉积
成矿理论
海底喷气
marine bottom exhalogene, hydrothermal sedimentary mineralization, exhalation deposit,sedimentary basin analysis
