中国非金属矿工业导刊Issue(3)：58-62,69,6.
浙江上方山塘岭石灰岩矿地质特征及成因浅析
Analysis of Geological Characteristics and Genesis of Shantangling Limestone Mine in Zhejiang Province
宋晨阳 1郝立 1张小鹏2
作者信息
- 1. 中国建筑材料工业地质勘查中心浙江总队,浙江 杭州 330022
- 2. 浙江省龙泉市自然资源和规划局,浙江 龙泉 323700
- 折叠
摘要
Abstract
The Shantangling limestone in the upper part of Zhejiang province is mainly produced in the Carboniferous strata.The ore body is mainly controlled by the strata and is produced in a monoclinic layered manner.The strata are greatly influenced by the structure,and the ore bearing strata in the mining area are inverted.The lithological changes in the ore bearing strata are relatively small,and the ore quality is good.The industrial type of ore in the No.1 ore body of the mining area is black metallurgical flux limestone,while the industrial type of ore in the No.2 ore body is cement limestone.The average content of CaO in the deposit is over 52%,with low content of other harmful elements,making it a high-quality limestone deposit.The genetic type of the deposit is shallow marine biochemically sedimentary limestone deposit.关键词
上方山塘岭/石灰岩/地质特征/矿床成因Key words
Shangfangshan Tangling/limestone/geological characteristics/genesis of the deposit分类
天文与地球科学引用本文复制引用
宋晨阳,郝立,张小鹏..浙江上方山塘岭石灰岩矿地质特征及成因浅析[J].中国非金属矿工业导刊,2024,(3):58-62,69,6.
