SEISMOLOGY AND GEOLOGY ›› 1997, Vol. 19 ›› Issue (3): 227-234.
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Zhou Zhenheng, Xiang Caiying
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周真恒, 向才英
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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
Zhou Zhenheng, Xiang Caiying. DISTRIBUTION OF THE LITHOSPHERIC GEOTEMPERATURE IN YUNNAN[J]. SEISMOLOGY AND GEOLOGY, 1997, 19(3): 227-234.
周真恒, 向才英. 云南岩石圈地温分布[J]. 地震地质, 1997, 19(3): 227-234.
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