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MEASUREMENTS OF ELECTRICAL CONDUCTIVITY OF BASALT AT TEMPERATURES UP TO 1500℃ AND PRESSURES TO ABOUT 20 KILOBARS

机译:玄武岩电导率的测量,温度高达1500℃,压力约20公斤

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摘要

The electrical conductivity of basalt was studied by means of the AC technique at temperatures up to 1500℃ and pressures to about 20 Kb. From the sharp changes in the slope of the conductivity curve, melting temperatures were determined. As pressure increases, the melting temperatures of dry basalt increase, and the melting intervals are shorter than those determined for the same sample by differential thermal analysis and the quenching method. Complete melting of dry basalt increases the electrical conductivity by a factor of about 10 at most not only at atmospheric pressure but also at high pressures up to about 20 Kb. The pressure effect up to about 20 Kb is small compared with the effect of temperature. Water pressure increases the electrical conductivity to a much greater extent than partial melting. Therefore, structure models of electrical conductivity for western Canada will be interpreted by the difference in water content.
机译:通过交流技术研究了玄武岩的电导率,温度高达1500℃,压力高达20 Kb。从电导率曲线的斜率的急剧变化确定熔融温度。随着压力的升高,干玄武岩的熔融温度升高,并且熔融间隔比通过差热分析和淬火方法确定的相同样品短。干玄武岩的完全熔化不仅在大气压下而且在高达约20 Kb的高压下最多将电导率提高大约10倍。与温度的影响相比,高达20 Kb的压力影响很小。与部分熔化相比,水压可以更大程度地提高电导率。因此,加拿大西部的电导率结构模型将通过含水量的差异来解释。

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    WATANABE Hiroshi;

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  • 年度 1970
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  • 正文语种 en
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