title: Calcite-Aragonite Equilibrium at 100{degrees}C.
abstract: The equilibrium pressure of the calcite-aragonite transition has been determined near 100 degrees C and is 4.35 kilobars. These data are in agreement with earlier work but conflict with the most recent determination by Simmons and Bell.
authors.forename: W A
authors.initials: WA
authors.lastname: Crawford
authors.forename: W S
authors.initials: WS
authors.lastname: Fyfe