The depth of sub-lithospheric diamond formation and the redistribution of carbon in the deep mantle
- 1 March 2017
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 461, 30-39
Abstract
No abstract availableFunding Information
- DFG (FR1555-9)
- ERC (227893)
This publication has 64 references indexed in Scilit:
- Experimental calibration of a garnet–clinopyroxene geobarometer for mantle eclogitesContributions to Mineralogy and Petrology, 2015
- Craton nucleation and formation of thick lithospheric rootsLithos, 2012
- A Reappraisal of Redox Melting in the Earth’s Mantle as a Function of Tectonic Setting and TimeJournal of Petrology, 2010
- Majoritic garnet: A new approach to pressure estimation of shock events in meteorites and the encapsulation of sub-lithospheric inclusions in diamondGeochimica et Cosmochimica Acta, 2010
- Oxidation state of the lithospheric mantle beneath Diavik diamond mine, central Slave craton, NWT, CanadaContributions to Mineralogy and Petrology, 2009
- Diamonds and eclogites of the Jericho kimberlite (Northern Canada)Contributions to Mineralogy and Petrology, 2009
- Evolution of the Archaean crust by delamination and shallow subductionNature, 2003
- Geochemistry of xenolithic eclogites from West Africa, part 2: origins of the high MgO eclogitesGeochimica et Cosmochimica Acta, 2002
- A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteriaMineralogical Magazine, 1987
- Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12Mg3Al2Si3O12 and Fe4Si4O12Fe3Al2Si3O12 at high pressures and temperaturesPhysics of the Earth and Planetary Interiors, 1977