现代地质2011，Vol.25Issue(2)：377-383,7.
黑龙江省敦密断裂带镜泊湖段地堑地热资源评价
Evaluation on the Geothermal Resources in Jingbo Lake Graben of the Dun-Mi Fault Zone in Heilongjiang Province
隋学文 1张俊 1石凤姣 1赵继昌2
作者信息
- 1. 黑龙江省水文地质工程地质勘察院,黑龙江哈尔滨,150030
- 2. 中国地质大学环境学院,湖北武汉,430074
- 折叠
摘要
Abstract
The research on the geothermal resources in Jingbo Lake graben of the Dun-Mi fault zone in Heilongjiang Province provides an example to acquire the formation rule of geothermal resources in the sag part of the large fracture zone. Jingbo Lake graben, the regional geological structure of which belongs to the northeast part of the Tan-Lu fault zone, expands in the form of the long strip. The graben has quite deep sedimentary rock layer which contains Neogene system and Paleogene system, the very high geothermal gradient that is 3.2 -4. 0 ℃/ hm. The temperature is 90. 8 ℃ at 2,500 m deep underground and the geothermal fluid output per unit is 54 m3/( d · m). The results show that geological conditions of geotherm is very favourable. The integrated and calculated data show that the Jingbo Lake graben can be a large-scale geothermal field. By the geothermal fluid output per unit of geothermal well and the evaluation indicators of the suitable classification of the geothermal water exploitation, this geothermal field belongs to the most suitablely exploited geothermal field that has the rich geothermal output. The discovery of geothermal field of Jingbo Lake graben has the positive guidance for seeking out the geothermal resource in the Dun-Mi fault zone, Yi-Shu fault zone and the Tan-Lu fault zone.关键词
敦密断裂/镜泊湖段地堑/地热资源/地下热水/郯庐断裂带/黑龙江省Key words
Dun-Mi fault/ Jingbo Lake graben/ geothermal resources/ geothermal water/ Tan-Lu fault zone/Heilongjiang Province分类
天文与地球科学引用本文复制引用
隋学文,张俊,石凤姣,赵继昌..黑龙江省敦密断裂带镜泊湖段地堑地热资源评价[J].现代地质,2011,25(2):377-383,7.
