МОДЕЛЮВАННЯ ПРОСТОРОВОЇ МІНЛИВОСТІ ПАЛЕОТЕМПЕРАТУРНИХ УМОВ МІНЕРАЛОУТВОРЕННЯ БАРУН-ХОЛБИНСЬКОГО ЗОЛОТОРУДНОГО РОДОВИЩА (СХІДНИЙ САЯН)

Анотація

Physico-chemical conditions of the Barun-Holbins’ke gold deposit formation have
been considered. Based on the homogenization measurement data the deposit was formed
under mesothermal conditions, concordant with the mineral paragenesis and textural-
structural features of the locality.
By means of the dynamic interpretation of the physico-chemical data the spatial
temporal evolution of fluids can be followed. The spatial evolution is reflected by isoterm
maps constructed from the values of the temperature of the homogenization and the
temperature of the decrepitation. The results of comparison of paleotemporal models are
as follows: two maps provide information supporting one another.