摘要
华南地区热水沉积建造发育 ,在沉积建造类型、沉积作用方式、产出的大地构造背景及岩石地球化学特征等方面反映了热水沉积的多样性。该地区的热水沉积作用具有相对确定的演化特性 ,并与许多金属矿床有直接或间接的关系。
WT5BZ]Fossil sea floor hydrothermal sedimentary formations developed well in South China, such facts has attracted attention from Chinese scholars since 1980s. The hydrothermal sedimentation varied in sediment formation, model and tectonic background as well as in geochemical characteristics. It had certain evolution direction, and was to various extents in relation to the formation of many metallic ore deposits in this area.
出处
《矿物岩石地球化学通报》
CAS
CSCD
2000年第2期114-118,共5页
Bulletin of Mineralogy, Petrology and Geochemistry
基金
国家科技部攀登预选项目!( 95 预 3 9)
国家重点基础研究项目!(G19990 43 2 10 )
国家教育部骨干教师基金资助
国家自然科学基