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2008•Journal of Geological Hazards and Environment PreservationRequires access

GEOLOGICAL FEATURES OF GEOTHERMAL FIELD IN WEST PART OF LIAOCHENG

Kuifeng Wang

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Abstract

Geothermal heat in west part of Liaocheng locates in south of Shenxian sink in Linqing depression with the square of 1 280 km2.This article synthetically analysed geological background,hydrogeology characteristics,the earth physical and chemical characteristics.Liaocheng geothermal field is a kind of strata bounding and low temperature geothermal field.The hot reservoir is mainly composed of the lower part of Minghuazhen group and Guantao group in Neogene and Dongying group in Paleogene.Geothermal gradient in in the area is controlled mainly by structures,and the structure heat conduct is a key factor for the geothermal field formation.The geothermal water mineralization degree is less and is mainly the atmosphere precipitation source.

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What this paper is about

Geothermal heat in west part of Liaocheng locates in south of Shenxian sink in Linqing depression with the square of 1 280 km2.This article synthetically analysed geological background,hydrogeology characteristics,the earth physical and chemical characteristics.Liaocheng geothermal field is a kind of strata bounding and low temperature geothermal field.The hot reservoir is mainly composed of the lower part of Minghuazhen group and Guantao group in Neogene and Dongying group in Paleogene.Geothermal gradient in in the area is controlled mainly by structures,and the structure heat conduct is a key factor for the geothermal field formation.The geothermal water mineralization degree is less and is mainly the atmosphere precipitation source.

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Available abstract

Geothermal heat in west part of Liaocheng locates in south of Shenxian sink in Linqing depression with the square of 1 280 km2.This article synthetically analysed geological background,hydrogeology characteristics,the earth physical and chemical characteristics.Liaocheng geothermal field is a kind of strata bounding and low temperature geothermal field.The hot reservoir is mainly composed of the lower part of Minghuazhen group and Guantao group in Neogene and Dongying group in Paleogene.Geothermal gradient in in the area is controlled mainly by structures,and the structure heat conduct is a key factor for the geothermal field formation.The geothermal water mineralization degree is less and is mainly the atmosphere precipitation source.

Key concepts: Geothermal gradient, Geology, Neogene, Geothermal heating, Geothermal exploration, Geochemistry, Geothermal energy, Paleogene

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