Fayalite from Fe-rich paralavas of ancient coal fires in the Kuzbass,Russia |
| |
Authors: | S A Novikova |
| |
Institution: | (1) Department of Earth and Environmental Sciences, Korea University, Seoul, 136 701, Korea;(2) Sobolev Institute of Geology and Mineralogy of Siberian Branch of Russian Academy of Sciences, 630090 Novosibirsk, Russia;(3) Novosibirsk State University, Pirogova 2, 630090 Novosibirsk, Russia |
| |
Abstract: | Fayalite is a common mineral of Fe-rich paralavas related to spontaneous combustion of coal seams. Fayalite has also been
found in parabasalts from burned coal waste piles of the Chelyabinsk coal basin. Among paralavas from different combustion
metamorphic (CM) complexes of the world, fayalite is the most widespread in the fused rocks of the Kuznetsk coal basin (Kuzbass)
and the Ravat area in Tajikistan. The optimal conditions for fayalite formation as products of coal fires in the Kuzbass and
Ravat resulted from a favorable combination of the composition of fused protolith (parental rocks) composed of pelitic and
Fe-rich sediments and the redox conditions of the deep subsurface ($
f_{O_2 }
$
f_{O_2 }
is lower than the QFM buffer). In the Kuzbass, fayalite is commonly hosted in high-silica aluminous Fe-rich paralavas composed
of Fe-cordierite (sekaninaite), tridymite, hercynite-magnetite, cristobalite, aluminous clinoferrosilite, and Al-K silicic
glass. The composition of all Kuzbass fayalites is close to the Fe2SiO4 end member. Kuzbass fayalites are characterized by a negligibly low CaO content and higher MnO and P2O5 contents like fayalites from burned rocks of other CM complexes. In Kuzbass paralavas, Fe-olivine is the late phase that
crystallized after sekaninaite and tridymite, immediately before melt quenching. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|