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甘肃当金山二号区块水泥用大理岩矿地质特征及矿床成因

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甘肃当金山二号区块大理岩矿赋存于奥陶纪盐池湾组(Oyc)第二岩性段(Oyc2)中,矿体呈层状产出,矿石品位稳定,属I级品.总结了当金山二号区块大理岩矿床赋存层位、矿体形态及规模、矿石物质组成、结构构造、自然类型等地质特征.通过综合分析该区地质特征,确定大理岩矿属于滨-浅海陆架相沉积变质型矿床,大理岩由区域岩浆热变质作用形成,表出露的大理岩为其找矿标志.
Geological Characteristics and Genesis of Cementmarble Deposit in Dangjinshan No.2 Block,Gansu Province
Marble mine in Dangjinshan No.2 block,Gansu province,occurs in the second lithologic member(Oyc2)of Ordovician Yanchiwan Formation(Oyc).The ore body is stratified and the ore grade is stable,belonging to grade Ⅰ.This paper summarizes the geological characteristics of marble mine in Dangjinshan No.2 block,including occurrence position,ore body shape and size,ore material composition,texture andstructure,and natural type.Through comprehensive analysis of the geological characteristics of the area,it is determined that the marble deposit belongs to the shore-shallow shelf sedimentary metamorphic deposit,the marble is formed by regional magmatic thermal metamorphism,and the marble exposed on the surface is the prospecting indicator.

cementmarblegeological characteristicsgenesis of mineral depositDangjinshan

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甘肃省有色金属地质勘查局天水矿产勘查院,甘肃天水 741020

水泥用大理岩 地质特征 矿床成因 当金山

甘肃省自然资源厅地质勘查基金

甘资勘发[2020]26号:202001-Y04

2024

四川地质学报
四川省地质学会

四川地质学报

影响因子:0.314
ISSN:1006-0995
年,卷(期):2024.44(1)
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