摘要
本文以东南地洼区铀矿为例，对过渡层（岩性）、构造过渡带及地洼阶段过渡期的有利配合的“三位一体”的成矿模式进行阐述，并对其找矿意义进行了初步探讨。
With uranium ore deposits in the Southeast China Diwa region as examples, this paper demonstrates an ore forming model on'trinity' of transition bed(lithology), structural transition zone and transition period of diwa stage, and primarily discusses its significance in prospecting for mineral deposits.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1999年第4期293-299,共7页
Geotectonica et Metallogenia
关键词
地洼
过渡层
过渡带
找矿意义
矿床成矿
铀矿床
Diwa
transition room
transition bed
transition zone
transition period
mineralization
ore prospecting
