High-temperature hydration of ultramafic granulites from the Southern Marginal Zone of the Limpopo Belt by infiltration of CO2-rich fluid
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference28 articles.
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4. The upper stability of clinochlore at low pressure and free energy of formation of Mg-cordierite;Chernosky;Am. Mineral.,1974
5. Experimental determination of the spinel peridotite to garnet peridotite reaction in the system MgO-Al2O3-SiO2 in the range 900–1100°C and Al2O3 isopleths of enstatite in the spinel field;Danckwerth;Contrib. Mineral. Petrol.,1978
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1. Thermo-tectonic evolution of the Neoarchaean Southern Marginal Zone of the Limpopo granulite Complex (South Africa);South African Journal of Geology;2023-12-01
2. Fluid migration along deep‐crustal shear zone: A case study of the Rhenosterkoppies Greenstone Belt in the northern Kaapvaal Craton, South Africa;Geological Journal;2023-06-14
3. Genesis and mineralization style of gold occurrences of the Lower Lom Belt, Bétaré Oya district, eastern Cameroon;Ore Geology Reviews;2021-12
4. Isotope Characteristics of Carbonates from Rocks of Greenstone Belts as an Indicator of a Possible Source of Fluids in Precambrian Granulite Complexes: An Example from the Giyani Greenstone Belt and the Limpopo Granulite Complex, South Africa;Doklady Earth Sciences;2020-05
5. Carbonate-silicate inclusions in garnet as evidence for a carbonate-bearing source for fluids in leucocratic granitoids associated with granulites of the Southern Marginal Zone, Limpopo Complex, South Africa;Gondwana Research;2020-01
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