Add to ORKGDiscusses the distribution of Fe 2+ and Fe 3+ between the brucite and talc layers. Data obtained indicate a clear-cut relationship between the peak position for Fe 2+ and the distribution between the 2 types of layer. The distribution of Fe 3+ is controlled by the size of the octathedra in the layers. -A.Hal
International audienceThe advantages and limits of empirical, semi-empirical and thermodynamic metho...
A B S T R A C T: Pore-lining chlorites are often responsible for the preservation fporosity in deepl...
International audienceIron chlorite with compositions intermediate between the two end-members daphn...
Discusses the distribution of Fe 2+ and Fe 3+ between the brucite and talc layers. Data obtained ind...
International audienceA compilation of Fe 3+-bearing chlorite analyses is used: (1) to investigate t...
Chlorite widely occurs in the alteration halo of hydrothermal deposits, it has been found in the alt...
from sandstones has been studied by analytical transmis-sion electron microscopy. Selected area (sin...
TEM/EDAX analyses suggest that he chlorites are Al-rich, Mg-chamosites with Fe/(Fe + Mg)> 0.47. O...
© SGEM2014. All Rights Reserved. This article analyzes finely dispersed matter in the deep horizons ...
International audienceChlorite is a ubiquitous product of metamorphism, alteration of magmatic rocks...
Chlorite minerals from six distinctive chlorite-quartz parageneses in central Borrowdale have been s...
Dioctahedral chlorite, collapsing on heating at 300-400°C, is reported extensively in soils. But X-r...
Two specimens or natural chromite from the Oman ophiolite were studied using Mossbauer Spectroscopy ...
Analysis of the distribution of ions in the coexisting phyllosilicate phases phengite, biotite and c...
International audienceThe advantages and limits of empirical, semi-empirical and thermodynamic metho...
A B S T R A C T: Pore-lining chlorites are often responsible for the preservation fporosity in deepl...
International audienceIron chlorite with compositions intermediate between the two end-members daphn...
Discusses the distribution of Fe 2+ and Fe 3+ between the brucite and talc layers. Data obtained ind...
International audienceA compilation of Fe 3+-bearing chlorite analyses is used: (1) to investigate t...
Chlorite widely occurs in the alteration halo of hydrothermal deposits, it has been found in the alt...
from sandstones has been studied by analytical transmis-sion electron microscopy. Selected area (sin...
TEM/EDAX analyses suggest that he chlorites are Al-rich, Mg-chamosites with Fe/(Fe + Mg)> 0.47. O...
© SGEM2014. All Rights Reserved. This article analyzes finely dispersed matter in the deep horizons ...
International audienceChlorite is a ubiquitous product of metamorphism, alteration of magmatic rocks...
Chlorite minerals from six distinctive chlorite-quartz parageneses in central Borrowdale have been s...
Dioctahedral chlorite, collapsing on heating at 300-400°C, is reported extensively in soils. But X-r...
Two specimens or natural chromite from the Oman ophiolite were studied using Mossbauer Spectroscopy ...
Analysis of the distribution of ions in the coexisting phyllosilicate phases phengite, biotite and c...
International audienceThe advantages and limits of empirical, semi-empirical and thermodynamic metho...
A B S T R A C T: Pore-lining chlorites are often responsible for the preservation fporosity in deepl...
International audienceIron chlorite with compositions intermediate between the two end-members daphn...
