The chemistry of carbon in aqueous fluids at crustal and upper-mantle conditions: experimental and theoretical constraints
CE Manning, EL Shock… - Reviews in Mineralogy …, 2013 - pubs.geoscienceworld.org
Carbon can be a major constituent of crustal and mantle fluids, occurring both as dissolved
ionic species (eg, carbonate ions or organic acids) and molecular species (eg, CO2, CO …
ionic species (eg, carbonate ions or organic acids) and molecular species (eg, CO2, CO …
Paleoproterozoic granulites from the Xinghe graphite mine, North China Craton: Geology, zircon U–Pb geochronology and implications for the timing of deformation …
The Xinghe graphite deposit is located in the north-central part of the North China Craton
(NCC) where Archean gray gneiss, metasedimentary rocks (khondalites) and mafic (high …
(NCC) where Archean gray gneiss, metasedimentary rocks (khondalites) and mafic (high …
Vein graphite deposits: geological settings, origin, and economic significance
FJ Luque, JM Huizenga, E Crespo-Feo, H Wada… - Mineralium …, 2014 - Springer
Graphite deposits result from the metamorphism of sedimentary rocks rich in carbonaceous
matter or from precipitation from carbon-bearing fluids (or melts). The latter process forms …
matter or from precipitation from carbon-bearing fluids (or melts). The latter process forms …
CO2 outgassing during collisional orogeny is facilitated by the generation of immiscible fluids
Orogenic degassing is emerging as a potentially relevant source of carbon dioxide (CO2)
from the continental crust. However, the processes of carbon mobilization are still poorly …
from the continental crust. However, the processes of carbon mobilization are still poorly …
Granitoid magmas preserved as melt inclusions in high-grade metamorphic rocks
This review presents a compositional database of primary anatectic granitoid magmas,
entirely based on melt inclusions (MI) in high-grade metamorphic rocks. Although MI are …
entirely based on melt inclusions (MI) in high-grade metamorphic rocks. Although MI are …
The buffering capacity of lithospheric mantle: implications for diamond formation
Current models for the formation of natural diamond involve either oxidation of a methane-
bearing fluid by reaction with oxidized mantle, or reduction of a carbonate-bearing fluid (or …
bearing fluid by reaction with oxidized mantle, or reduction of a carbonate-bearing fluid (or …
Lower crustal resistivity signature of an orogenic gold system
Orogenic gold deposits provide a significant source of the world's gold and form along faults
over a wide range of crustal depths spanning sub-greenschist to granulite grade faces, but …
over a wide range of crustal depths spanning sub-greenschist to granulite grade faces, but …
[HTML][HTML] C–O–H fluid-melt-rock interaction in graphitic granulites and problems of quantifying carbon budget in the lower continental crust
Estimates on the geological carbon cycle are subject to large uncertainties that can be
reduced by thorough observation of rocks. In this contribution, we focus specifically on C–O …
reduced by thorough observation of rocks. In this contribution, we focus specifically on C–O …
Anatexis and fluid regime of the deep continental crust: New clues from melt and fluid inclusions in metapelitic migmatites from Ivrea Zone (NW Italy)
We investigate the inclusions hosted in peritectic garnet from metapelitic migmatites of the
Kinzigite Formation (Ivrea Zone, NW Italy) to evaluate the starting composition of the …
Kinzigite Formation (Ivrea Zone, NW Italy) to evaluate the starting composition of the …
[PDF][PDF] Graphite deposit types, their origin, and economic significance
GJ Simandl, S Paradis, C Akam - … Ministry of Energy and Mines & …, 2015 - researchgate.net
Graphite is an opaque, gray-black, and soft (1-2 on Mohs hardness scale) mineral with a
metallic luster. It is characterized by a greasy feel, low density (2.09-2.23 g/cm3), high …
metallic luster. It is characterized by a greasy feel, low density (2.09-2.23 g/cm3), high …