摘要
分析了塔里克铀矿点区域地质背景、矿点地质概况、含矿岩系和铀矿化特征及其成因类型,认为铀矿化成因属于层间氧化带型,"倒卷状"铀矿化为构造隆升前形成的"古矿化"。通过分析铀矿化带走向延伸特征和地貌特征,指出了找矿远景地段。
The regional geological setting, brief geological outline of the ore occurrence, ore-bearing rock series, features and genetic types of uranium mineralization of Talike uranium ore occurrence are analyzed. It is considered that the genesis of uranium mineralization belongs to the inter-layered oxidation zone type. The＇ Inverted roll-front＇ uranium mineralization is a＇ palaeo-mineralization＇ formed before the structural uplift. Prospective areas are pointed out by analyzing the strike extension of uranium mineralization zone and geomorphic features.
出处
《世界核地质科学》
CAS
2008年第3期139-142,156,共5页
World Nuclear Geoscience
关键词
塔里克铀矿点
成因
找矿方向
Talike uranium ore occurrence
genesis
prospecting direction
