scholarly journals Modeling of thermodynamic and chemical changes in low-temperature geothermal systems

1986 ◽  
Author(s):  
A.L. Spencer
2008 ◽  
Vol 60 (8) ◽  
pp. 821-826 ◽  
Author(s):  
Hakim Saibi ◽  
Jun Nishijima ◽  
Tomohiro Hirano ◽  
Yasuhiro Fujimitsu ◽  
Sachio Ehara

Clay Minerals ◽  
1982 ◽  
Vol 17 (2) ◽  
pp. 159-173 ◽  
Author(s):  
D. Proust

AbstractThe mineralogical and chemical changes of sheridanite were followed in different alteration horizons as weathering of its host amphibolite increased. Microscopic and microprobe analyses of phases produced in or around the chlorite allowed a classification of the different alteration stages relative to their position in the profile. In the unweathered rock, prehnite and a sericite—kaolinite assemblage appear to have formed at grain boundaries between chlorites and plagioclases. These represent low-pressure (PH2O < 2.5 ± 1 Kb) and low-temperature (320–360°C) metamorphic phases. In the saprock, where initial rock structure is still preserved, chlorites weather to a more or less regular mixed-layer chlorite-vermiculite. In the saprolite, large-grain (20 µm) vermiculite forms in the clayey zones (plasma) when rock structure is destroyed. The chemical composition of these newly-formed minerals is influenced by the original chlorites and mixed-layer minerals.


Energies ◽  
2018 ◽  
Vol 11 (6) ◽  
pp. 1591 ◽  
Author(s):  
Alessandro Sbrana ◽  
Paola Marianelli ◽  
Giuseppe Pasquini ◽  
Paolo Costantini ◽  
Francesco Palmieri ◽  
...  

2020 ◽  
Vol 1588 ◽  
pp. 012020
Author(s):  
A Ibatullina ◽  
I Krasina ◽  
M Antonova ◽  
S Ilushina ◽  
E Isayeva ◽  
...  

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