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OverviewThis book sheds valuable new light on the genetic mineralogy of lower-mantle diamonds and syngenetic minerals. It presents groundbreaking experimental results revealing the melting relations of ultrabasic and basic associations and a physicochemical peritectic mechanism of their evolution. The experimental investigations included here reveal the key multicomponent, multiphase oxide-silicate-carbonate-carbon parental media for lower-mantle diamonds and syngenetic minerals. Consequently, readers will find extensive information on the diamond-parental oxide-silicate-carbonate-carbon melts-solutions that supplement the general features of lower-mantle diamond genesis and the most efficient ultrabasic-basic evolution. The experimental results on physicochemical aspects, combined with analytical mineralogy data, make it possible to create a generalized composition diagram of the diamond-parental melts-solutions, there by completing the mantle-carbonatite concept for the genesis of lower-mantle diamonds and syngenetic minerals. This book addresses the needs of all researchers studying the Earth’s deepest structure, super-deep mineral formation including diamonds, and magmatic evolution. Full Product DetailsAuthor: Anna V. Spivak , Yuriy A. LitvinPublisher: Springer International Publishing AG Imprint: Springer International Publishing AG Edition: 1st ed. 2019 Weight: 1.671kg ISBN: 9783319785172ISBN 10: 3319785176 Pages: 95 Publication Date: 12 June 2018 Audience: Professional and scholarly , College/higher education , Professional & Vocational , Postgraduate, Research & Scholarly Format: Hardback Publisher's Status: Active Availability: Manufactured on demand ![]() We will order this item for you from a manufactured on demand supplier. Table of ContentsChemical and phase composition of lower mantle of the Earth: analytical and experimental data.- Experimental methods and techniques.- Evolution of the native lower mantle systems.- Evolution of the lower mantle diamond-forming system.- Diamond-forming efficiency of oxide-silicate-carbonate-carbon systems at the conditions of the Earth lower mantle.- Model of diamond formation at conditions of the Earth lower mantle.ReviewsAuthor InformationTab Content 6Author Website:Countries AvailableAll regions |