CaSiO3 perovskite in diamond indicates the recycling of oceanic crust into the lower mantle

Depth of formation of CaSiO 3 -walstromite included in super-deep diamonds

(2016) C. Anzolini et al.   LITHOS

Slab melting as a barrier to deep carbon subduction

(2016) Andrew R. Thomson et al.   NATURE

Large gem diamonds from metallic liquid in Earth’s deep mantle

(2016) Evan M. Smith et al.   SCIENCE

Stable isotope evidence for crustal recycling as recorded by superdeep diamonds

(2015) A.D. Burnham et al.   EARTH AND PLANETARY SCIENCE LETTERS

Diamond thermoelastic properties and implications for determining the pressure of formation of diamond-inclusion systems

(2015) R.J. Angel et al.   Russian Geology and Geophysics

Diamond Formation: A Stable Isotope Perspective

(2014) Pierre Cartigny et al.   Annual Review of Earth and Planetary Sciences

Isotopic constraints on the nature and circulation of deep mantle C–H–O–N fluids: Carbon and nitrogen systematics within ultra-deep diamonds from Kankan (Guinea)

(2014) M. Palot et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Hydrous mantle transition zone indicated by ringwoodite included within diamond

(2014) D. G. Pearson et al.   NATURE

THE ORIGIN OF LARGE IRREGULAR GEM-QUALITY TYPE II DIAMONDS AND THE RARITY OF BLUE TYPE IIB VARIETIES

(2014) A. E. MOORE   SOUTH AFRICAN JOURNAL OF GEOLOGY

Geophysics of Chemical Heterogeneity in the Mantle

(2012) Lars Stixrude et al.   Annual Review of Earth and Planetary Sciences

Deep Mantle Cycling of Oceanic Crust: Evidence from Diamonds and Their Mineral Inclusions

(2011) M. J. Walter et al.   SCIENCE

Sources of carbon in inclusion bearing diamonds

(2009) Thomas Stachel et al.   LITHOS

Plastic deformation of lower mantle diamonds by inclusion phase transformations

(2008) Nicola J. Cayzer et al.   EUROPEAN JOURNAL OF MINERALOGY