摘要
宁芜型铁矿(也叫玢岩铁矿)在成因上与火山岩、次火山岩有关，广泛分布于长江中下游一带。它们的共同特点是从高温到中低温的热液围岩蚀变很发育，蚀变与成矿作用关系密切。本文参考Hclgeson等人关于水-岩石相互作用。
On the basis of the irreversibly thermodynamical principle, a thermodynamical mo-del (a set of differential equations) has been established, which can simulate the mine-ralization of Ningwu-type iron deposits. Computer-based studies have been made of the physicochemical conditions and mechanisms pertaining to the mineralization and -wall-rock alteration of these deposits.
出处
《地球化学》
CAS
1985年第2期169-181,共13页
Geochimica
