ISSN 1673-8217 CN 41-1388/TE
主管：中国石油化工集团有限公司 主办：中国石油化工股份有限公司河南油田分公司
符勇. 1997: 魏岗地区浅层地层划分及供水意义. 石油地质与工程, 11(04): 8-10+59.
引用本文: 符勇. 1997: 魏岗地区浅层地层划分及供水意义. 石油地质与工程, 11(04): 8-10+59.
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Fu Yong. 1997: Divison of Shallow Formation in Weigang District and Its Significance of Water Supply. Petroleum Geology and Engineering, 11(04): 8-10+59.
Citation: Fu Yong. 1997: Divison of Shallow Formation in Weigang District and Its Significance of Water Supply. Petroleum Geology and Engineering, 11(04): 8-10+59.
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魏岗地区浅层地层划分及供水意义

Divison of Shallow Formation in Weigang District and Its Significance of Water Supply

    摘要
  • 摘要: 利用南阳凹陷魏岗地区7口水源探井资料，对600m深度地层的颜色、化石、岩性、电性、富水性、承压水头和沉积环境几个方面进行研究，详细划分了时代，指出第四系含水层仍作为供水的主要目的层，为主要水源；上第三系含水层也能作为供水的主要目的层，为后备水源，且能提供优质矿泉水和低温热水；下第三系含水层不能作为供水的主要目的层，但能提供高温热水，可作为供热热源。

     

    Abstract: According to data of 7 water source wells, studing and deviding formation above depth of 600m of Weigang district in Nanyang basin, this paper points out that Quaternary aquifer still is the main objective formation and main water source. Neogene aquifer also is the main objective formation and reserve water source. But Eogene aquifer cannot be taken as the main objective formation.

     

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