Energy for geodynamics: Mantle decompression thermal-tsunami

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Energy for geodynamics: Mantle decompression thermal-tsunami

机译：地球动力学能量：地幔减压热海啸

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It is known through experience in deep mines and with bore-holes that temperature increases with depth in the crust. For more than half a century geophysicists have made measurements of near-surface continental and oceanic heat flow with the aim of determining the Earth’s heat loss. Pollack et al. estimate a global heat loss of 44.2 TW (1 TW = 10 12 W) based upon 24,774 observations at 20,201 sites.

机译：通过在深矿和钻孔中的经验可以知道，温度随着地壳中的深度而增加。半个多世纪以来，地球物理学家对近地表的大陆和海洋热流进行了测量，目的是确定地球的热损失。 Pollack等。根据20,201个站点的24,774个观测值，估计全球总热量损失为44.2 TW（1 TW = 10 12 W）。

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《Current Science: A Fortnightly Journal of Research》 |2006年第12期|共2页
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1. Energy for geodynamics: Mantle decompression thermal-tsunami [J] . Current Science: A Fortnightly Journal of Research . 2006,第12期

机译：地球动力学能量：地幔减压热海啸
2. Tomography of core-mantle boundary and lowermost mantle coupled by geodynamics: joint models of shear and compressional velocity [J] . Gaia Soldati, Lapo Boschi, Steve Della Mora, Annals Of Geophysics . 2014,第6期

机译：地球动力学耦合的地幔边界和最低地幔层析成像：剪切速度和压缩速度联合模型
3. Nitrogen Isotopes and Mantle Geodynamics: The Emergence of Life and the Atmosphere-Crust-Mantle Connection [J] . Pierre Cartigny, Bernard Marty Elements . 2013,第5期

机译：氮同位素和地幔地球动力学：生命的出现与大气-地壳-地幔的联系
4. Instabilities across the Scales: Simple Models for Shear Banding, Plate Subduction and Mantle Convection in Geodynamics [C] . Hans-Bernd Mühlhaus, Louis Moresi, Matt Davies, International Congress of Theoretical and Applied Mechanics . 2013

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5. Geodynamical modeling of mantle convection to investigate mantle layering and the cause of lower mantle anisotropy. [D] . McNamara, Allen Keith. 2002

机译：地幔对流的地球动力学模型，研究地幔分层和下地幔各向异性的原因。
6. Preclinical activity of 8-chloroadenosine with mantle cell lymphoma: Roles of energy depletion and inhibition of DNA and RNA synthesis [O] . Jennifer B. Dennison, Kumudha Balakrishnan, Varsha Gandhi -1

机译：8-氯腺壬籽用搭式细胞淋巴瘤的临床前活性：能量消耗和DNA和RNA合成的抑制作用
7. Joint seismic–geodynamic-mineral physical modelling of African geodynamics: A reconciliation of deep-mantle convection with surface geophysical constraints [O] . Alessandro M. Forte, Sandrine Quéré, Robert Moucha, 2010

机译：非洲地球力学的联合地震 - 地球力 - 矿物学模型：对地层对流对域的核对与表面地球物理约束

Energy for geodynamics: Mantle decompression thermal-tsunami

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