汾渭裂谷地热资源初探
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摘要
通过对汾渭裂谷区域地质构造、地震、裂谷形成机制以及地球物理勘察资料等的综合分析 ,探讨了汾渭裂谷地热资源分布规律与特征 ,以及地热资源与汾渭裂谷的关系。对该区域地热资源的勘探、开发和利用有一定的参考价值
In this paper,the distribution regularity and characteristic of geothermal resources in Fen wei rift, is studied by synthetic analysis in region geological condition, geological structure, earthquake, formative mechanism of the rift and the data of geophysical exploration. It will be helpful for further exploration and development of geothermal resources in Fen wei rift.
引文
[1] 王连成,乔立骐,杨军耀.第三次全国地热学术会议论文选集[C].北京:北京科学技术出版社,1991:179208.
    [2] HochsteinMP .GeothermalSystemsintheHaurakiRiftZone(NewZealand)anExampleforGeothermalSystemOveranInferredUpperMantleSwell[J].AlternativeEnergySources,1978,6:25992610.
    [3] GiggenbachWF .GraphicalTechniquesfortheEvaluationofWater/RockEquilibrationConditionsbyUseofNa,K ,MgandCaContentsofDischargeWaters[C].Proc8thNzGeothermalWorkshop,1986:3743.

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