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Evolution of magmatic and diamond-fo...

Earth (Planet)

Evolution of magmatic and diamond-forming systems of the Earth's lower mantle

Record Type:	Electronic resources : Monograph/item
Title/Author:	Evolution of magmatic and diamond-forming systems of the Earth's lower mantleby Anna V. Spivak, Yuriy A. Litvin.
Author:	Spivak, Anna V.
other author:	Litvin, Yuriy A.
Published:	Cham :Springer International Publishing :2019.
Description:	xii, 95 p. :ill., digital ;24 cm.
Contained By:	Springer eBooks
Subject:	Earth Sciences.
Subject:	Earth (Planet)Rotation.
Online resource:	http://dx.doi.org/10.1007/978-3-319-78518-9
ISBN:	9783319785189$q(electronic bk.)

Evolution of magmatic and diamond-forming systems of the Earth's lower mantle
Spivak, Anna V.

Evolution of magmatic and diamond-forming systems of the Earth's lower mantle[electronic resource] /by Anna V. Spivak, Yuriy A. Litvin. - Cham :Springer International Publishing :2019. - xii, 95 p. :ill., digital ;24 cm. - Springer geology,2197-9545. - Springer geology..

Chemical 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.

This 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.

ISBN: 9783319785189$q(electronic bk.)

Standard No.: 10.1007/978-3-319-78518-9doiSubjects--Topical Terms:

309702
Earth Sciences.
Subjects--Geographical Terms:

611612
Earth (Planet)
--Rotation.

LC Class. No.: QE509.4

Dewey Class. No.: 551.116

Evolution of magmatic and diamond-forming systems of the Earth's lower mantle
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520 $a This 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.
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