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黔东北地区南华纪锰矿基本特征
引用本文:覃英,周琦,张遂.黔东北地区南华纪锰矿基本特征[J].贵州地质,2005,22(4):246-251.
作者姓名:覃英  周琦  张遂
作者单位:贵州省地矿局一○三地质大队,贵州,铜仁,554300
摘    要:黔东北地区“大塘坡式”锰矿,产于南华系大塘坡组底部炭质页岩中。含锰沉积盆地受北东向古断裂的控制,矿床呈北东向展布。本文总结了区内锰矿成矿地质条件、夯布特征、成矿规律、找矿标志及地质勘探工作程度,并提出了下步地质勘查工作建议。

关 键 词:锰矿  大塘坡式  成锰盆地  成矿规律  找矿标志  黔东北
文章编号:10000-594(2005)04-0246-06
收稿时间:2005-12-07
修稿时间:2005年12月7日

Elementary Properties of Manganese of Nh in the Northeastern Guizhou
QIN Ying,ZHOU Qi,ZHANG Sui.Elementary Properties of Manganese of Nh in the Northeastern Guizhou[J].Guizhou Geology,2005,22(4):246-251.
Authors:QIN Ying  ZHOU Qi  ZHANG Sui
Abstract:The Datangpo-type manganese ores in the eastern Guizhou emerge within the carbonaceous shale at the bottome of the Datangpo formation. The manganese ores which deposited into the basin are controlled by paleo-faults, the deposit spread in the north-astern direction. The geologic terms, distribution feature, metallogenic laws and marks of the prospecting are summed up, and geologic survey is put forward for next step.
Keywords:manganese  Datangpo type  manganese - forming basin  metaUogenic regular  marks of prospecting  northeastern Guizhou
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