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首页> 外文期刊>Geophysical Research Letters >Electromagnetic evidence for volatile-rich upwelling beneath the society hotspot, French Polynesia
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Electromagnetic evidence for volatile-rich upwelling beneath the society hotspot, French Polynesia

机译:法属波利尼西亚社会热点下富含挥发物的上升流的电磁证据

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We have conducted a seafloor magnetotelluric survey that images, for the first time, three-dimensional electrical conductivity structure in the upper mantle beneath the Society hotspot. A striking feature in our model is a high-conductivity anomaly a few hundred kilometers in diameter, which is continuous from the lowest part of the upper mantle to a depth of approximately 50km below sea level. Using theoretical and experimental results from mineral physics, we interpret the high-conductivity anomaly as evidence of the melt fraction up to 2.2vol.%, which is robust regardless of assumed temperature, and the existence of carbonated silicate melt beneath the hotspot. Our results suggest that the Society hotspot is a pathway for ascending volatiles from the deeper part of the upper mantle to the surface.
机译:我们进行了一次海底大地电磁测量,首次对协会热点下方的上地幔中的三维电导率结构进行了成像。我们模型的一个显着特征是直径为几百公里的高电导异常,该异常从上地幔的下部一直延伸到海平面以下约50公里的深度。利用矿物物理学的理论和实验结果,我们将高电导率异常解释为高达2.2vol。%的熔体分数的证据,无论假定的温度如何,该分数都是稳健的,并且热点下方存在碳酸硅酸盐熔体。我们的结果表明,该学会的热点是从上地幔的较深部分向地表上升挥发物的途径。

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