The Earth's Mantle: Composition, Structure, and EvolutionThe Earth's mantle plays a crucial role in a variety of geologic processes and provides researchers with important insights into the development of our planet. Interdisciplinary in scope, The Earth's Mantle is a comprehensive overview of the composition, structure and evolution of the mantle layer. Striking a balance between established consensus and continuing controversy, the book provides researchers and graduate students with an authoritative review of this important part of our planet. Written by internationally recognized scientists from the Research School of Earth Sciences at the Australian National University, it draws on perspectives from cosmochemistry, isotope geochemistry, fluid dynamics and petrology, seismology and geodynamics, and mineral and rock physics. The hardback edition received excellent reviews. |
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المحتوى
Implications for Accretion and Core | 3 |
Trace Elements | 52 |
An Isotopic Perspective | 127 |
Consequences | 159 |
Understanding Mantle Dynamics through Mathematical Models | 191 |
Plates Plumes Mantle Convection and Mantle Evolution | 228 |
Insights from the Melting Products | 259 |
A Ringwood Concept and Its Current Expression | 311 |
From Subduction Zone to Craton | 381 |
Seismological | 405 |
Evidence from Analyses | 461 |
Insights from Laboratory Studies of Deformation | 503 |
561 | |
طبعات أخرى - عرض جميع المقتطفات
عبارات ومصطلحات مألوفة
abundances accretion amount assumed atmosphere basalts bodies boundary layer bulk calculated Chapter chemical chondrites component composition consistent constraints continental crust convection core crust dependence depleted depth derived determined dynamics early Earth Planet effects elements enriched estimate et al evidence evolution example experimental Figure flow fluid formation formed fractionation geochemical Geophys Green Griffiths groups heat higher implications important increasing indicate isotopic komatiites less Lett lherzolite lithosphere lower mantle magmas major material melting metal meteorites MORB Nature observed occur oceanic olivine origin oxidized peridotite phase plate plume possible present pressure primitive processes produced pyrolite ratio refractory region relative residual rocks samples shown siderophile significant silicate similar slab solar solidus structure studies subduction suggested surface temperature thermal transition types upper mantle values viscosity volatile volcanism volume zone