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笆蕉坑组隐伏脉状钨矿床规模大、品位高,正确地认识和掌握其地质特征和成矿规律,对扩大矿区远景、寻找盲矿具有重要意义.近年来,随着坑探工程的进展,提供了更多的地质资料.一矿区(矿段)地质概述矿区位于南玲东西构造带东端与新华夏系隆起带的反接复合处.区内寒武纪变质砂,板岩系构成北东向复式背斜,背斜东陡西缓,向北东撒开.寒武系地层因受加里东
The volcanic tungsten deposit in the Bajiaokeng Formation is of large scale and high grade, and its geological characteristics and metallogenic regularities can be correctly understood and mastered. It is of great significance to expand the prospect of the mining area and find blind mines.In recent years, with the progress of the pit exploration project , Providing more geological data.General overview of a mining area (ore section) The ore area is located at the reverse junction of the eastern end of the Nanling East-West structural belt and the Neo-Cathaysian uplift belt.The composition of the Cambrian metamorphic sand and slate in the area The north-east anticline, anticlinal east-westward easterly, splayed to the northeast. The Cambrian strata were affected by Caledonian