摘要
用地球化学自组织作用思想讨论了鞍山式铁矿床中条带状矿化图案的微观成因机理，认为它们是一种在远离平衡态条件下的耗散结构，建立了成因理论模型．
The idea of geochemical self-organization is employed to explain the microscopical genetic mechanism of banded mineralizing pattern (BMP) developed in Anshan-type iron deposits,China. BMP is considered here as the very dissipative structure formed far from equilibrium. Theoretical models are suggested as reactive-infiltration feedback, supersaturation-nucleation-depletion cycle and competitive particle growth.
出处
《东北大学学报（自然科学版）》
EI
CAS
CSCD
1994年第5期481-484,共4页
Journal of Northeastern University(Natural Science)
基金
冶金工业部教育司资助
关键词
铁矿床
地球化学
自组织
Anshan-type iron deposits
banded mineralizing pattern
geochemical self-organization.
