Geothermal Resources in the Eastern Liaocheng Geothermal Field of
详细信息
- 责任者：Wang Kuifeng (Shandong Institute and Laboratory of Geological Sciences ; Jinan 250013 ; China)
- 刊名：Geology in China
- 出版年：2009
- 卷期：36(1)
- 关键词：地热田 ; geothermal fields ; 山东 ; Shandong Province
- 页码：p.194-202
- 图表：9 illus., 2 tables，16 refs.
- 分类号：1005
- issnNo：ISSN1000-3657
- isbnNo：CN11-1167/P
摘要
Based on drilling data and recent research results, the author considers that the Liaocheng geothermal field belongs to the karst fissure layered conductive type, with the regional geological structures being mainly composed of Liaokao fault and Chiping fault, and the hot reservoir chiefly comprised of limestone strata of Ordovician Majiagou Formation. The geothermal gradient of the area is controlled mainly by structure, the structural heat conduction is a key factor for the formation of this area, the mineralization intensity of the geothermal water is low, and the geothermal water contains some useful mineral components.