Acidic fluids in the Earth's lower crust.

ABSTRACT: Fluid flux through Earth's surface and its interior causes geochemical cycling of elements in the Earth. Quantification of such process needs accurate knowledge about the composition and properties of the fluids. Knowledge about the fluids in Earth's interior is scarce due to limitations in both experimental methods and thermodynamic modeling in high/ultrahigh pressure-temperature conditions. In this study, we present halogen (Cl, F) measurements in apatite grains from the mafic (metagabbro), and felsic (two-pyroxene granulite, charnockite, hornblende-biotite gneiss) rocks preserved in the Nilgiri Block, southern India. Previous experiments show that it is difficult to incorporate Cl in apatite compared to F at high pressure and temperature conditions. Based on regional trends in Cl and F

SUBMITTER: Samuel VO 

PROVIDER: S-EPMC8551242 | biostudies-literature | 2021 Oct

REPOSITORIES: biostudies-literature