| 书目名称 | Evolution of Magmatic and Diamond-Forming Systems of the Earth‘s Lower Mantle |
| 编辑 | Anna V. Spivak,Yuriy A. Litvin |
| 视频video | |
| 概述 | Summarizes groundbreaking experimental results revealing the melting relations for lower-mantle systems and analytical data for mineral inclusions in super-deep diamonds.Explains the physicochemical p |
| 丛书名称 | Springer Geology |
| 图书封面 |  |
| 描述 | .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 evolut |
| 出版日期 | Book 2019 |
| 关键词 | The lower mantle; Composition of the lower mantle; superdeep diamonds; mineral inclusions; High pressure |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-319-78518-9 |
| isbn_softcover | 978-3-030-08719-7 |
| isbn_ebook | 978-3-319-78518-9Series ISSN 2197-9545 Series E-ISSN 2197-9553 |
| issn_series | 2197-9545 |
| copyright | Springer International Publishing AG, part of Springer Nature 2019 |
发表于 2025-3-21 17:52:33
