PRESSURE GRADIENT FROM THE CONTRIBUTION OF BOTH GEOTHERMAL AND GRAVITY IN THE LITHOSPHERE

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摘要 Thepressuregradientofthelithosphereisakeytoexplainingvariousgeologicalprocesses,andvariesalsointimeandspacesimilartothegeothermalgradient.Inthispaperacorrelationformulaofgeothermalgradientsandpressuregradientswasbuiltwiththethermocomprestioncoefficients.Basedonthisformula,thearticlehasstudiedtherelationbetweenthepressuregradientsandthegeothermalgradientsinthelithosphere,andtheresultsindicatethatthepressuregradientinthelithosphereisnonlinear,anditsminimumvalueisthelithostaticgradient,andthatthepressuregradientofthelithospherewillincreaseobviouslywiththecontributionofbothgeothermalandgravity,andcouldbetwicetimesmorethanthelithostaticgradient.
机构地区 不详
出版日期 2005年02月12日(中国期刊网平台首次上网日期,不代表论文的发表时间)
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