松辽盆地北部干热岩地热资源研究

Duo Xiao, H. Wei, S. Shi, Huanlai Zhu, Senlin Gan, Xiaoxiong Wu, W. Feng
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摘要

松辽盆地拥有丰富的油气和地热资源,是中国著名的大型陆相沉积盆地。迄今为止,松辽盆地北部的地热资源研究主要集中在以低温地热资源为主的浅层。然而,对高温干热岩深层地热资源的研究仍处于空白状态。本文在松辽盆地勘探研究成果和石油探井资料的基础上,通过对高温干热岩地热资源的研究,进一步完善了松辽盆地北部地热资源勘探开发理论。干热岩分布相对集中在松辽盆地北部,主要分布在研究区中部、南部和东南部,150℃等温面深度基本小于5km,有利于干热岩发育。研究表明,松辽盆地北部两个大地热流高值区分别位于中央坳陷区南部以及中央坳陷区、东南隆起区和东北隆起区三个一级构造带的结合部,热干岩地热资源潜力较大。利用增强型地热系统开采干热岩是可行的。该研究对松辽盆地北部干热岩深层地热资源的开发利用具有一定的指导和参考意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research of Geothermal Resources on Hot Dry Rock in North Songliao Basin of China
With abundant oil and gas as well as geothermal resources, Songliao Basin is a famous large continental sedimentary basin in China. So far, the research of geothermal resources in North Songliao Basin has mainly concentrated in the shallow layers where low-temperature geothermal resource is mainly developed. However, the research of deep geothermal resource in high-temperature hot dry rock is still in a blank state. Based on the Songliao Basin exploration and research achievements as well as oil exploration well data, this paper further improves geothermal resource exploration and development theories of North Songliao Basin by researching geothermal resources in high-temperature hot dry rock. Hot dry rock distribution is relatively concentrated in the North Songliao Basin, mainly in the central, southern and southeastern part of the study area, where the depth of 150 ℃ isothermal surfaces substantially less than 5km is conducive to the development of hot dry rocks. Studies have shown that two high value areas of terrestrial heat flow in the North Songliao Basin are respectively located in the southern part of the central depression area as well as the junction of three first-order tectonic belts including central depression, southeast and northeast uplift areas, where geothermal resource potential of hot dry rock is great. By using enhanced geothermal system, mining hot dry rock is feasible. This study has some guidance and reference for the development and utilization of deep geothermal resources in hot dry rock of the North Songliao Basin.
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