GEOTHERMAL GEOLOGICAL CHARACTERISTICS OF FIVE TECTONIC UNITS IN THE SEDIMENTARY BASINS OF HENAN PROVINCE

HUANG Guang-shou; GUO Li-li; HUANG Kai

2020 Vol. 29, No. 2

Article Contents

Article navigation > Geology and Resources > 2020 > 29(2): 172-179

Next Article Previous Article

HUANG Guang-shou, GUO Li-li, HUANG Kai. GEOTHERMAL GEOLOGICAL CHARACTERISTICS OF FIVE TECTONIC UNITS IN THE SEDIMENTARY BASINS OF HENAN PROVINCE[J]. Geology and Resources, 2020, 29(2): 172-179.

Citation:

HUANG Guang-shou, GUO Li-li, HUANG Kai. GEOTHERMAL GEOLOGICAL CHARACTERISTICS OF FIVE TECTONIC UNITS IN THE SEDIMENTARY BASINS OF HENAN PROVINCE[J]. Geology and Resources, 2020, 29(2): 172-179.

GEOTHERMAL GEOLOGICAL CHARACTERISTICS OF FIVE TECTONIC UNITS IN THE SEDIMENTARY BASINS OF HENAN PROVINCE

1.
Henan Institute of Geological Survey, Zhengzhou 450001, China
2.
Strategic Alliance for Technological Innovation of Underground Clean Energy Exploration and Development Industry, Zhengzhou 450001, China
3.
No.5 Institute of Geological Exploration, Henan Bureau of Geology and Mineral Resources, Zhengzhou 450001, China

Received Date: 15 July 2019

Revised Date: 20 August 2019

Publish Date: 28 April 2020

Abstract

Abstract

The sedimentary basins inside five tectonic units in Henan Province, involving 11 cities and more than 60 counties, is the main areas where geothermal resources occur. Analysis of 524 geothermal wells in the five tectonic units shows that the geothermal wells are unevenly distributed in different units, and the depths of water taking layers in the wells vary greatly. The average water taking depths of the five tectonic units provide a basis for the designing of geothermal wells in these areas. The distribution statistics of geothermal wells in the five tectonic units show that the distribution density in three units is less than 0.9 wells per 100 km², with great potential for exploration.
- Tangyin fault depression /
- Neihuang uplift /
- Jiyuan-Kaifeng depression /
- Tongxu uplift /
- Zhoukou depression /
- geothermal geology /
- Henan Province

FullText(HTML)

References

[1]	王现国, 张慧, 张娟娟.开封凹陷区地热水水化学特征及同位素分析[J].安全与环境工程, 2012, 19(6):88-92. Google Scholar
[2]	李海林.郑州市郑东新区深部地热资源研究[J].地下水, 2011, 33(4):7-10. Google Scholar
[3]	王继华.河南沉降盆地地热资源评价[J].长江大学学报(自然科学版), 2010, 7(2):178-180. Google Scholar
[4]	王心义, 黄丹.河南省地热资源开发利用现状评价[J].地下水, 2010, 32(1):54-55, 70. Google Scholar
[5]	王肖凤, 符勇, 康彩艳.南阳盆地地热特征与开发利用前景[J].平顶山学院学报, 2010, 25(2):122-125. Google Scholar
[6]	商真平, 姚兰兰.商丘市城区可采地热资源量计算分析[J].人民黄河, 2009, 31(5):62, 64. Google Scholar
[7]	张心勇, 马传明.开封凹陷区地温场特征分析[J].工程勘察, 2009, 37(10):44-49. Google Scholar
[8]	齐玉峰.河南省开封凹陷区地热田地热资源分析[J].西南科技大学学报, 2009, 24(3):75-78. Google Scholar
[9]	刘传权, 郭克剑.郑州市城区深部基岩层热储特征分析[J].华南地质与矿产, 2008(2):58-61. Google Scholar
[10]	黄光寿, 郭丽丽, 黄凯.河南省十大温泉地热地质特征[J].地质与资源, 2020, 29(1):91-100. Google Scholar
[11]	张满波, 武秀江, 吴双红.河南省地热资源形势及开发利用潜力分析[J].地下水, 2008, 30(4):45, 70. Google Scholar
[12]	齐玉峰, 王现国, 王关杰, 等.开封凹陷区地热资源开发利用与保护[J].地下水, 2007, 29(4):77-79. Google Scholar
[13]	郭山峰, 王春晖, 吴祖成.周口市地热资源浅析及水文地质参数计算[J].地下水, 2006, 28(6):32-33. Google Scholar