| 锦州辖区寻找地热水资源的探讨 |
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| 引用本文： | 孙洪德,孙延征,刘士秀,姜英德,张琦.锦州辖区寻找地热水资源的探讨[J].化工矿产地质,2010,32(3):154-159. |
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| 作者姓名： | 孙洪德 孙延征 刘士秀 姜英德 张琦 |
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| 作者单位： | [1]东北煤田地质局一五五勘探队,辽宁锦州121000 [2]辽宁省第七地质大队,辽宁丹东118003 [3]辽宁省化工地质勘查院,辽宁锦州121000 |
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| 摘 要： | 通过对区内地热资源成矿机制,成矿规律的分析认为,锦州市辖区为高地温场区,地热资源主要赋存在1400m以下,深部热源是由地幔隆起地壳变薄热传导所致,区域构造体系控制了地下热水的形成和分布,凡是深度超过1400m且赋存地下水资源的地方,都能形成地下热水资源。在充分分析区内岩石的含水类型的基础上,根据它们分布和赋存深度,探讨寻找地下热水的区段及其方向,为区内地热开发提供依据。
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| 关 键 词： | 地热资源 地幔热物质 地温梯度 辽河西斜坡带 生油门限值 |
DISCUSSION ON PROSPECTING FOR GEOTHERMAL WATER RESOURCES IN JINZHOU AREA |
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| Sun Hongde,Zhang Yanzheng,Liu Shixiu,Jiang Yingde,Zhang Qi.DISCUSSION ON PROSPECTING FOR GEOTHERMAL WATER RESOURCES IN JINZHOU AREA[J].Geology of Chemical Minerals,2010,32(3):154-159. |
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| Authors: | Sun Hongde Zhang Yanzheng Liu Shixiu Jiang Yingde Zhang Qi |
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| Institution: | 1.No.155 Exporation Team of Northeast Coalfield Geological Bureau,Dandong,Liaoning,118003,China 2.No.7 Liaoning Geological Team,Jinzhou,Liaoning,121000,China 3.Liaoning Chemical and Geological Prospecting Institute,Jinzhou,Liaoning,121000,China |
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| Abstract: | According to the analysis on the ore-forming mechanism and regulation of geothermal resources in Jinzhou area,we found that the geothermal resources in the high geotemperature place were host 1400m under the earth surface,and caused by mantle bulge and the thinned out crust.The geothermal water formation and distribution was controled by regional structural system.Geothermal water will be formed at any groundwater resources hosting area which is 1400m underground.We got some foundation on developing geotherm in the area after analysing the water-containing type,distribution and the hosting depth of the rock,as well as discussing the geothermal water section and directions. |
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| Keywords: | geothermal resources mantle thermal matter geothermal gradient Liao river west inclined slope threshold of oil generation value |
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