SEISMOLOGY AND GEOLOGY ›› 1997, Vol. 19 ›› Issue (3): 227-234.

• Brief Report • Previous Articles     Next Articles

DISTRIBUTION OF THE LITHOSPHERIC GEOTEMPERATURE IN YUNNAN

Zhou Zhenheng, Xiang Caiying   

  1. Seismological Bureau of Yunnan Province, Kunming 650204
  • Received:1996-04-30 Online:1997-09-09 Published:2009-11-25

云南岩石圈地温分布

周真恒, 向才英   

  1. 云南省地震局, 昆明, 650204
  • 基金资助:
    云南省应用基础研究基金资助(93D045Q)

Abstract: According to the data of the heat flow and lithospheric structure,and the correlative formula between the heat production A and the seismic velocity VP,the distribution of the lithospheric geotemperature in Yunnan has been studied. Three geothermal types exist in whole Yunnan region: high geotemperature type with the Moho temperature >960℃ and the crustal geothermal gradient >2℃/100m,low geotemperature one with the Moho temperature <700℃ and the crustal geothermal gradient <1.5℃/100m,and middle geotmeperature one with the Moho temperature lying between the former two types and the crustal geothermal gradient 1.5~ 2.0℃/100m.

Key words: Geothermal field, Lithosphere, Yunnan

摘要: 根据大地热流和岩石圈结构资料,探讨了云南岩石圈的地温分布。研究结果表明,全区存在3种地热类型:高地温型莫霍面温度>960℃,地壳地温梯度>2℃/100m;低地温型莫霍面温度<700℃,地壳地温梯度<1.5℃/100m;中等地温型莫霍面温度介于前二者之间,地壳地温梯度为1.5~2.0℃/100m。

关键词: 地热场, 岩石圈, 云南