TEMPERATURE GRADIENTS IN UPPER LAYERS OF EARTHS CRUST DUE TO CONVECTIVE WATER FLOWS

被引：78

作者：

DONALDSON, IG

机构：

来源：

JOURNAL OF GEOPHYSICAL RESEARCH | 1962年 / 67卷 / 09期

关键词：

D O I：

10.1029/JZ067i009p03449

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：3449 / +

共 26 条

[11] TEMPERATURE-VARIATION IN UPPER EARTH CRUST DUE TO PERIODIC NATURE OF SOLAR INSOLATION
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[12] Asymmetric reverse transition phenomenon in internal turbulent channel flows due to temperature gradients
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[13] An experimental study of the formation of an ice crust and migration of water vapor in a comet's upper layers
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[14] Convective instabilities in liquid layers with free upper surface under the action of an inclined temperature gradient
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[15] The study of preferential water flows and convective heat transfer using the method of temperature labeling
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[16] The Study of Preferential Water Flows and Convective Heat Transfer using the Method of Temperature Labeling
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[17] COMPOSITION OF THE EARTHS CRUST AND UPPER MANTLE FROM THE DSS DATA IN THE CENTRAL TURKMENIA AND LABORATORY TESTS AT HIGH-PRESSURE AND TEMPERATURE
VOLAROVICH, MP
VOLYNETZ, LN
LEVSHIN, AL
IZVESTIYA AKADEMII NAUK SSSR FIZIKA ZEMLI, 1980, (06): : 76 - 82
[18] Influence of the Temperature and Density of the Upper Layers of the Convective Zone on the Spectrum of Gamma Quantum during Solar Flashes
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[19] Influence of the Temperature and Density of the Upper Layers of the Convective Zone on the Spectrum of Gamma Quantum during Solar Flashes
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GEOMAGNETISM AND AERONOMY, 2022, 62 (08) : 1073 - 1077
[20] MAJOR CATION GRADIENTS IN DSDP INTERSTITIAL WATERS - THE ROLE OF DIFFUSIVE EXCHANGE BETWEEN SEA-WATER AND UPPER OCEANIC-CRUST
MCDUFF, RE
GEOCHIMICA ET COSMOCHIMICA ACTA, 1981, 45 (10) : 1705 - 1713

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