Main Metallogenic Regularity and Metallogenic Zone Division of Permian Manganese Deposits in Northern Guizhou-Eastern Yunnan Province
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摘要:
这是一篇地球科学领域的论文。锰矿为我国十分紧缺的战略矿产之一。黔北-滇东地区是我国二叠纪锰矿最典型的分布区，在全球晚古生代也较为少见，该区锰矿资源丰富，找矿潜力巨大，称为“遵义式锰矿”。研究表明，该区锰矿产于二叠纪茅口晚期，分布严格受黔北裂谷盆地控制，锰矿在地堑盆地中心喷溢沉积成矿，在地垒区则无锰矿分布，矿体空间展布方向与盆地展布方向基本一致。其中，黔北遵义-黔西地区锰矿在空间上分布于盆地相区，并可分为中心相、过渡相、边缘相等三个锰矿相带，进一步指示了锰矿具体成矿位置，显示了锰矿受盆地中心控制非常明显的特点。在划分的遵义-宣威锰矿成矿带的基础上，详细划分出遵义-黔西锰矿成矿亚带中深溪—八里、龙坪—兴隆、团溪—尚稽、黔西4个锰矿矿集区，以及水城-宣威锰矿成矿亚带中水城—纳雍、格学2个锰矿矿集区。该研究成果对寻找黔北—滇东二叠纪隐伏锰矿床，开展成矿预测，具有重要的意义。
Abstract:This is an article in the field of earth sciences. Manganese ore is one of the strategic minerals in short supply in China. The area of Northern Guizhou-Eastern Yunnan is the most typical distribution area of manganese ore in Permian, which is also rare in the Late Paleozoic in the world. It is rich in manganese ore resources and has great prospecting potential, so it is called "Zunyi type manganese ore". The results show that the manganese ore is produced in the late Permian Maokou, and its distribution is strictly controlled by the northern Guizhou rift basin. The manganese ore is formed in the center of graben basin by exhalation deposition, but no manganese ore is distributed in the barrier area, and the ore-body spatial distribution direction is basically consistent with the basin distribution direction. Among them, manganese ore in Zunyi - western Guizhou area is spatially distributed in the basin facies area, and can be divided into three manganese ore facies belts, namely, the central phase, the transition phase and the edge, which further indicates the specific metallogenic location of manganese ore and shows that the manganese ore is controlled by the center of the basin. Based on the Zunyi-Xuanwei manganese ore belt, it can be divided into four manganese ore concentration areas in the Zunyi-Qianxi manganese ore mineralization subzone: Shenxi-Bali, Longping-Xinglong, Tuanxi-Shangji and Qianxi, and two manganese ore concentration areas in shuicheng - Xuanwei manganese ore mineralization subzone: Shuicheng - Nayong and Gexue.The research results are of great significance to search for Permian concealed manganese deposits in northern Guizhou and eastern Yunnan and to carry out metallogenic prediction.
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图 1 遵义团溪剖面中二叠统茅口组锰矿凝灰层样品（A12085）及上二叠统龙潭组底部黏土岩样品（YDX-1）锆石U-Pb定年谐和线图（A, B），与频率直方图（C, D）[36]
Figure 1.
表 1 黔北裂谷盆地原型与结构
Table 1. Prototype and structure of the Northern Guizhou Rift Basin
Ⅰ级 Ⅱ级 Ⅲ级地堑盆地与地垒 Ⅳ级地堑盆地 备注 黔北裂谷盆地 遵义—黔西次级裂谷盆地 深溪—八里地堑盆地 冯家湾—铜锣井、共青湖—转龙庙、深溪地堑盆地 黔北裂谷盆地原型恢复限于茅口晚期-龙潭 龙坪—兴隆地堑盆地 张家湾—木杠台、兴隆地堑盆地 团溪—尚稽地堑盆地 长滩—柏杨坝、和尚场地堑盆地 喇叭—南北、西坪—苟江地垒 − 黔西地堑盆地 − 水城—宣威次级裂谷盆地 格学—水城地堑盆地 营盘、徐家寨、陈家寨、坛罐窑、格学、麻窝地堑盆地 
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表 2 贵州遵义-水城锰矿成矿带结构与划分
Table 2. Structure and division of Zunyi-Shuicheng manganese ore belt in Guizhou Province
成矿带 成矿亚带 矿集区 成矿预测区 已发现矿床（点） 成矿期 遵义—宣威锰矿成矿带 遵义—黔西锰矿成矿亚带 深溪—八里锰矿集区 铜锣井—深溪锰矿预测区 铜锣井大型锰矿床、深溪大型锰矿床、永安大型锰矿床、小金沟中型锰矿床、东高寨中型锰矿床、西台小型锰矿床 茅口晚期 共青湖—转龙庙锰矿预测 冯家湾中型锰矿床、共青湖中型锰矿床、转龙庙中型锰矿床 龙坪—兴隆锰矿集区 张家湾—木杠台锰矿预测区 龙坪中型锰矿床、木杠台枪村坝中型锰矿床、毛家山小型锰矿床、高山小型锰矿床 兴隆锰矿预测区 兴隆小型锰矿床、缘竹坪小型锰矿床、大土锰矿点、天井台锰矿点 团溪—尚稽锰矿集区 长滩—白杨坝锰矿预测区 长滩锰矿点、白杨坝锰矿点 和尚场锰矿预测区 工农湾小型锰矿床、和尚场中型锰矿床、铁厂坝锰矿点、高石坎锰矿点、五龙溪锰矿点 黔西锰矿集区 刀疤水锰矿预测区太来锰矿预测区 刀疤水锰矿点、太来钴锰矿点 水城—宣威锰矿成矿亚带 水城—纳雍锰矿集区 水城锰矿预测区 徐家寨小型锰矿床、立火小型锰矿床、营盘小型锰矿床 茅口中期 纳雍锰矿预测区 / 格学锰矿集区 / 宣威格学中型锰矿床
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