Experimental petrology applied to natural diamond growth
RW Luth, YN Palyanov… - Reviews in Mineralogy …, 2022 - pubs.geoscienceworld.org
Perhaps the first point to address in this chapter is what role, or roles, experimental petrology
can play in understanding the formation of natural diamond. As can be seen from the other …
can play in understanding the formation of natural diamond. As can be seen from the other …
Compositions of kimberlite melts: A review of melt inclusions in kimberlite minerals
AV Golovin, VS Kamenetsky - Petrology, 2023 - Springer
The paper presents a comprehensive review of currently available data on melt inclusions
entrapped in minerals of kimberlites of different age and different provenance in ancient …
entrapped in minerals of kimberlites of different age and different provenance in ancient …
Carbonatite melt in type Ia gem diamond
AM Logvinova, A Shatskiy, R Wirth, AA Tomilenko… - Lithos, 2019 - Elsevier
Monocrystalline type Ia diamonds with octahedral growth morphology prevail among
lithospheric diamonds, including precious stones. Unlike less common 'fibrous' diamonds …
lithospheric diamonds, including precious stones. Unlike less common 'fibrous' diamonds …
Origin of K-rich diamond-forming immiscible melts and CO2 fluid via partial melting of carbonated pelites at a depth of 180–200 km
Melt inclusions in kimberlitic and metamorphic diamonds worldwide range in composition
from potassic aluminosilicate to alkali-rich carbonatitic and their low-temperature derivative …
from potassic aluminosilicate to alkali-rich carbonatitic and their low-temperature derivative …
Pyroxene-carbonate reactions in the CaMgSi2O6 ± NaAlSi2O6 + MgCO3 ± Na2CO3 ± K2CO3 system at 3–6 GPa: Implications for partial melting of …
The reactions between pyroxenes and carbonates have been studied in the CaMgSi 2 O 6+
MgCO 3 (Di+ 2Mgs), CaMgSi 2 O 6+ NaAlSi 2 O 6+ 2MgCO 3 (Di+ Jd+ 2Mgs), CaMgSi 2 O …
MgCO 3 (Di+ 2Mgs), CaMgSi 2 O 6+ NaAlSi 2 O 6+ 2MgCO 3 (Di+ Jd+ 2Mgs), CaMgSi 2 O …
Metasomatic interaction of the eutectic Na-and K-bearing carbonate melts with natural garnet lherzolite at 6 GPa and 1100–1200 C: toward carbonatite melt …
The range of carbonatite melts in equilibrium with the subcontinental lithospheric mantle
(SCLM) under geothermal conditions is limited by alkali-rich near-eutectic compositions …
(SCLM) under geothermal conditions is limited by alkali-rich near-eutectic compositions …
Towards composition of carbonatite melts in peridotitic mantle
It is generally accepted that carbonatite metasomatism in the subcontinental lithospheric
mantle (SCLM) inevitably causes wehrlitization of the primary lherzolite substrate. However …
mantle (SCLM) inevitably causes wehrlitization of the primary lherzolite substrate. However …
Carbonate melt interaction with natural eclogite at 6 GPa and 1100–1200 C: Implications for metasomatic melt composition in subcontinental lithospheric mantle
Compositional ranges of carbonate melt s stable under PT conditions corresponding to the
base of subcontinental lithospheric mantle (SCLM) are limited by alkali-rich near-eutectic …
base of subcontinental lithospheric mantle (SCLM) are limited by alkali-rich near-eutectic …
Phase relations in carbonate component of carbonatized eclogite and peridotite along subduction and continental geotherms
Phase relations in the carbonate constituent of mafic and ultramafic suites are decisive in the
deep carbon cycle and partial melting in the Earth's mantle. Here we present an …
deep carbon cycle and partial melting in the Earth's mantle. Here we present an …
Revision of the CaMgSi2O6-CO2PT phase diagram at 3–6 GPa
A Shatskiy, YG Vinogradova… - American …, 2023 - pubs.geoscienceworld.org
We reexamined the phase relationships in the system diopside-CO2 in the range of 3–6
GPa and 850–1500° C in multi-anvil experiments, including reversal ones lasting up to 169 …
GPa and 850–1500° C in multi-anvil experiments, including reversal ones lasting up to 169 …