首页|江西弋阳曹溪制碱用灰岩地质特征及找矿方向

江西弋阳曹溪制碱用灰岩地质特征及找矿方向

扫码查看
为支撑中国精细化高端制碱产业对矿产原料的需求,在曹溪矿区开展深部钻探和地表槽探等工作,查明矿区范围内制碱用灰岩矿体特征及空间分布,以分析矿床成因.通过分析勘查成果,发现矿床属稳定的沉积型化学碳酸盐型矿床,沉积环境处于低碱低能的浅海开阔台地环境,含矿构造为平缓向斜,矿体形态及空间展布随二叠系下统马平组地层分布,优质矿石主要为灰色巨厚层状微晶灰岩和生物碎屑灰岩.将岩石学特征作为首要的找矿要素,马平组地层作为主要的找矿标志层,为曹溪至盘岭一带找矿提供指导.
Geological Characteristics and Prospecting Direction of Caoxi Alkali-making Limestone in Yiyang County,Jiangxi Province
In order to support the demand for mineral raw materials in China's refined high-end alkali industry,deep drilling and surface trenching were carried out in Caoxi mining area to find out the character-istics and spatial distribution of limestone ore bodies for alkali production in the mining area,so as to ana-lyze the genesis of the deposit.By analyzing the exploration results,it is found that the deposit belongs to a stable sedimentary chemical carbonate deposit.The sedimentary environment is in a low-alkali and low-en-ergy shallow open platform environment.The ore-bearing structure is a gentle syncline.The shape and spa-tial distribution of the ore body are distributed with the lower Permian Maping Formation.The high-quality ore is mainly gray thick layered microcrystalline limestone and bioclastic limestone.The petrological charac-teristics are taken as the primary prospecting elements,and the Maping Formation is used as the main pros-pecting marker layer to provide guidance for the prospecting in the Caoxi-Panling area.

limestone for alkali-makingore-controlling factorsore genesisstratigraphic marker

关小强

展开 >

中国建筑材料工业地质勘查中心江西总队

制碱用灰岩 控矿因素 矿床成因 地层标志

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.(2)
  • 5