广东省粤中断裂型碳酸盐岩地热水的水文地球化学研究——以马星-隔陂地热系统为例
The Geochemistry of Carbonate Thermal Waters Hosted by Fault Area within the Central Guangdong,China:——A Case of Maxing-gepi Geothermal System
何沛欣1
作者信息
- 1. 广东省有色金属地质局九三五队,广东 惠州 516000
- 折叠
摘要
粤中地区地热资源丰富,但人们对断裂型碳酸盐岩地热水地球化学过程的认识存在一定争议.本文以马星-隔陂地热系统为例,采用Piper图、离子比例系数、Gibbs图和主成分方法(PCA法)针对其断裂型碳酸盐岩地热水水化学特征进行综合分析.
Abstract
The central Guangdong has abundant geothermal resources.However,the geochemistry of carbonate thermal waters hosted by fault area within the area remains unclear.Based on the Piper diagram,Gibbs figure,chemical ion proportionality coefficient analysis and principal component analysis(PCA),the paper studys the geochemistry of carbonate thermal waters hosted by Gepi Fault Area.
关键词
地球化学/断裂/碳酸盐岩热储/水-岩作用/粤中Key words
geochemistry/fault/carbonate geothermal reservoir/water-rock interaction/the central Guangdong引用本文复制引用
出版年
2024
NETL
NSTL
万方数据