沉积盆地热演化波动问题初探

THERMAL UNDALATORY EVOLUTION IN SEDIMENTARY BASINS
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  • 石油大学,北京    
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  • University of Petroleum,Beijing    
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    摘要:

    本文应用波动分析的观点,探讨沉积盆地温度变化的波动性及盆地演化过程中温度和热流的 波动变化,提出沉积盆地热流变化的波动模式,并以此研究了单井的热流变化情况,从而为 沉积盆地热史研究提供了一种可能的新方法。

    Abstract:

    The geothermal regime of sedimentary basins is a concrete manifestation o f structural movement an d it evolves with the evolution of basins. Due to the undulatory characteristics of the structural movement, the geothermal evolution of a sedimentar y basin is also Based on the undulation analysis, the undulatory characteristics of the geothermal variation during the evolution of sedimentary basins ar e discussed. Moreover, the process of undulatory evolution of heat flow is stud ied and the undulation m odel of heat flow of sedimentary basins has been established. Based on this mode l, a single well heat flow variation has been carried out, which may be thought to be a new method for the study of the geothermal history of sedimentary basin .

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引用本文

邱楠生,金之钧,刘国臣,李京昌.1996.沉积盆地热演化波动问题初探[J].地质论评,42(sup):302-306,[DOI].
Qiu Nansheng, Jin Zhijun, Liu Guochen, Li Jingchang.1996. THERMAL UNDALATORY EVOLUTION IN SEDIMENTARY BASINS[J]. Geological Review,42(sup):302-306.

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