Document Type
Book Section
Publication Date
3-24-2020
Publication Title
Carbon in Earth’s Interior
Publisher
Wiley/American Geophysical Union
First page number:
11
Last page number:
23
Abstract
High‐pressure carbonaceous minerals establish a link between one of the most abundant chemical elements and processes that occur at high pressures, either in the interior of the Earth or during shock‐metamorphosis in space or on Earth. Diamonds from the Earth's mantle carry inclusions of carbides, carbonates, methane, and carbon‐dioxide. These inclusions elucidate diamond formation and the carbon recycling in the mantle. This chapter focuses on these inclusion minerals themselves, the means of detection, and the reconstruction of pressure‐temperature conditions of their formation in the mantle.
Keywords
Carbonate Inclusions; Fine‐Grained Diamond Inclusions; High‐Pressure Carbonaceous Phases; High‐Pressure Minerals; Oxides; Terrestrial Diamonds
Disciplines
Earth Sciences | Geology | Physical Sciences and Mathematics
File Format
File Size
409 KB
Language
English
Rights
IN COPYRIGHT. For more information about this rights statement, please visit http://rightsstatements.org/vocab/InC/1.0/
Creative Commons License
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
Repository Citation
Tschauner, O.
(2020).
High‐Pressure Carbonaceous Phases as Minerals.
Carbon in Earth’s Interior
11-23.
Wiley/American Geophysical Union.
http://dx.doi.org/10.1002/9781119508229.ch2