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福建漳平石坂坑矿区水泥用灰岩矿床地质特征

范云虎

化工矿产地质2019,Vol.41Issue(3):150-157,8.
化工矿产地质2019,Vol.41Issue(3):150-157,8.

福建漳平石坂坑矿区水泥用灰岩矿床地质特征

Geological characteristics of cement limestone deposit in Shibankeng Mining, Zhangping, Fujian Province

范云虎1

作者信息

  • 1. 中化地质矿山总局福建地质勘查院,福建 福州 350013
  • 折叠

摘要

Abstract

The Shibankeng mining area in Zhangping is located in the west side of the Zhenghe-Dapu deep fault zone, the south segment of the Datian-Longyan subsag zone in the southwest Fujian depression zone, and between the Yongfu anticline and the Longzhan synclinorium. There are 4 limestone ore bodies for cement in the area, and the ore bodies are layered. The thick layers occur in the Chuanshan formation of Lower Permian and Qixia formation of Middle Permian. The occurrence of ore bodies is consistent with that of strata, and the ore quality is better. Based on the summary and analysis of the geological characteristics of the limestone ore body for cement in this area, the genetic type of the deposit is considered to be sedimentary metamorphic type. The geological characteristics of the deposit are representative in Fujian Province.

关键词

水泥用灰岩矿/矿床地质特征/漳平石坂坑

Key words

Cement limestone ore/Geological features of ore deposit/Shibankeng in Zhangping

分类

天文与地球科学

引用本文复制引用

范云虎..福建漳平石坂坑矿区水泥用灰岩矿床地质特征[J].化工矿产地质,2019,41(3):150-157,8.

化工矿产地质

1006-5296

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