摘要
研究表明，断裂构造作用引起造岩组分的调整再分配导致REE迁移，且REE在贫Si富Al的构造岩（带）富集。断裂构造作用不改变REE的总体分配型式，但可引起轻、重稀土发生一定程度的分异。
Faulting could adjust the petrochemical composition of tectonites and make them redistributed at faults. The process of petrochemical-compositional redistribution might cause REE to migrate between tectonites at faults. And REE were enriched in tectonites (or tectonic zones) where the petrochemical composition Al was enriched and Si descended. Faulting was unable to change the REE distribution patterns of tectonites at faults, but couldcause differentiation occurring between LREE and HREE.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1998年第1期75-81,共7页
Geotectonica et Metallogenia
基金
中科院八.五黄金课题!"地洼构造与金矿形成及找矿方向"资助
