Dry, hydrous, and CO2-bearing liquidus phase relationships in the CMAS system at 28 KB, and their bearing on the origin of alkali basalts

@inproceedings{Adam1988DryHA,
  title={Dry, hydrous, and CO2-bearing liquidus phase relationships in the CMAS system at 28 KB, and their bearing on the origin of alkali basalts},
  author={John A. Adam},
  year={1988}
}
  • John A. Adam
  • Published 1988
  • Geology
  • Dry, hydrous, and $$CO_{2}$$-bearing liquidus phase relationships were studied within the CMAS system ($$CaO-MgO-Al_{2}O_{3}-SiO_{2}$$) at 28 kb. In the dry system garnet, diopside, enstatite, and forsterite were found to coexist with a liquid of the approximate composition \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace… CONTINUE READING

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