Titlebook: Genesis of Diamonds and Associated Phases; Yuriy A. Litvin Book 2017 The Editor(s) (if applicable) and The Author(s), under exclusive lice

collagenase

Nils Gunnar Wahlgren,Magnus Thorén sequential peritectic interaction: (1) the clinopyroxene-formed reaction of orthopyroxene and ultrabasic melt (orthopyroxene loss) and (2) the garnet-formed reaction of olivine with jadeite component of fractionating ultrabasic melt (olivine loss).

Adulate

Kevin R. Loughlin,Michael P. O’Learydence. This makes possible to have arrived to the construction of the generalized diagrams for compositions of diamond-producing melts under the upper mantle, transition zone and lower mantle conditions.

geometrician

978-3-319-85418-2The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl

Duodenitis

Genesis of Diamonds and Associated Phases978-3-319-54543-1Series ISSN 2366-1585 Series E-ISSN 2366-1593

TEM

生氣地

心神不寧

Physico-Chemical Features of Lower-Mantle Diamond-Parental Systems,Experimental investigations on the origin of paradoxical assemblages of Mg and Fe oxides with stishovite (Si oxide) among inclusions in the lower-mantle diamonds made it possible to reveal the physico-chemical mechanism of the effect of “stishovite paradox”.

MAZE

Yuriy A. LitvinSimplifies a complicated mantle-carbonatite model of diamond genesis using experimental and mineralogical data.Provides a physicochemical solution of the long-standing and disputable mantle-carbonatit

RADE

GILD

Nils Gunnar Wahlgren,Magnus Thorén sequential peritectic interaction: (1) the clinopyroxene-formed reaction of orthopyroxene and ultrabasic melt (orthopyroxene loss) and (2) the garnet-formed reaction of olivine with jadeite component of fractionating ultrabasic melt (olivine loss).