Back to Search Start Over

Boron coordination and B/Si ordering controls over equilibrium boron isotope fractionation among minerals, melts, and fluids.

Authors :
Li, Yin-Chuan
Wei, Hai-Zhen
Palmer, Martin R.
Jiang, Shao-Yong
Liu, Xi
Williams-Jones, Anthony E.
Ma, Jing
Lu, Jian-Jun
Lin, Yi-Bo
Dong, Ge
Source :
Chemical Geology. Feb2021, Vol. 561, pN.PAG-N.PAG. 1p.
Publication Year :
2021

Abstract

The high mobility of boron during fluid-rock interaction makes it an effective tracer for the sources of magmatic and metamorphic fluids, as recorded in minerals such as tourmaline and muscovite. Although advances have been made in quantifying the fractionation of boron isotopes among different phases, boron isotope fractionation in complex silicate melts remains poorly understood. Here, we propose appropriate models for the BO 3 and BO 4 units in silicate melts covering a wide range of chemical compositions and boron coordination structures in silicate magmas, and report the results of a theoretical investigation of boron isotope fractionation among silicate melt, minerals and fluids using a first principles theoretical approach. A comparison of measured and calculated α factors in mineral-melt and fluid-melt systems shows good agreement, suggesting the applicability of a simplified treatment of boron coordination structures in silicate melt. The results of this study show that the proportion of trigonal/tetrahedral coordinated boron and the B/Si ordering in silicate tetrahedral layers control the boron isotope fractionation among different phases, and that the effect of chemical composition is minor (less than 2‰ at 600 K). The temperature-dependent boron isotope fractionations are described as 1000lnα mica-basic fluid = 0.8–2.4 × (1000/T) - 0.8 × (1000/T)2, 1000lnα mica-acidic fluid = 7.0–14.0 × (1000/T) - 1.2 × (1000/T)2 and 1000lnα mica-tur = 1.9–5.4 × (1000/T) -3.4 × (1000/T)2 (T is temperature in Kelvins). At magmatic temperatures, ∆11B values between mineral/fluid and melt also vary with the proportion of the BO 4 unit in the melt. This study underpins the applicability of the white mica-tourmaline geothermometers and boron isotopes for fluid source identification, and also offers an explanation of boron isotope fractionation in systems that contain complex silicate melts. Unlabelled Image [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00092541
Volume :
561
Database :
Academic Search Index
Journal :
Chemical Geology
Publication Type :
Academic Journal
Accession number :
148120702
Full Text :
https://doi.org/10.1016/j.chemgeo.2020.120030