| 注册
首页|期刊导航|地质学报|华南陆缘火成岩区差异性地壳热结构及地热意义

华南陆缘火成岩区差异性地壳热结构及地热意义

蔺文静 王贵玲 甘浩男

地质学报2024,Vol.98Issue(2):544-557,14.
地质学报2024,Vol.98Issue(2):544-557,14.DOI:10.19762/j.cnki.dizhixuebao.2023027

华南陆缘火成岩区差异性地壳热结构及地热意义

Differential crustal thermal structure and geothermal significance in the igneous region of southeastern China

蔺文静 1王贵玲 1甘浩男1

作者信息

  • 1. 中国地质科学院水文地质环境地质研究所,河北石家庄,050061||自然资源部地热与干热岩勘查开发技术创新中心,河北石家庄,050061
  • 折叠

摘要

Abstract

High heat-producing granite is one of the important intracrustal heat sources is widely distributed in the southeastern China,which provides the possibility of superficial heat generation and accumulation in the region.Based on the distribution of granite resources in the region,this paper systematically analyzes the radiogenic heat production characteristics of the main granite bodies in the region,and makes a comparative analysis of the deep temperature distribution,geothermal heat flux and crustal heat structure in the key geothermal exploration areas with the deep drilling of geothermal exploration in the region in recent years,and proposes a heat gathering model of shallow surface geothermal resources in the study area.The analysis concluded that the southeastern China has a quadratic heat gathering pattern of"mantle source heat supply-intracrustal heat generation-fracture heat transfer-cover heat preservation",among which,the radiogenic heat production rate of granite is one of the main factors affecting the shallow geothermal field in the area.The heat production rate of the North Guangdong-South Jiangxi rock body is obviously higher than that of the granite body in Zhangzhou area,which in turn is similar to the thermal structure of lithosphere of"hot crust-cold mantle"or"warm crust-warm mantle"type but has some differences with that of"hot mantle-cold crust"type in Zhangzhou.The fracture structure and cover conditions have obvious control on subsurface heat accumulation and dissipation.The results of the study are of theoretical and guiding significance for the in-depth understanding of the genesis and heat control factors of geothermal resources in southeastern China,as well as the future exploration and development practice of geothermal resources in the region.

关键词

高产热花岗岩/大地热流/地壳热结构/热源机制/华南陆缘

Key words

high heat-producing granite/heat flow/radiogenic production rate/heat source mechanism/southeastern China

引用本文复制引用

蔺文静,王贵玲,甘浩男..华南陆缘火成岩区差异性地壳热结构及地热意义[J].地质学报,2024,98(2):544-557,14.

基金项目

本文为科技部重点研发计划课题(编号 2021YFB1507401)和国家自然科学基金项目(编号 41874100)联合资助的成果. (编号 2021YFB1507401)

地质学报

OA北大核心CSTPCD

0001-5717

访问量0
|
下载量0
段落导航相关论文