Fluid–Silicate Separation of an Ultrabasic Melt into High-Potassium and Low-Potassium Fractions: Evidence from Picrites of the Late Cretaceous Ultrabasic Volcanic ... View Full Text


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Article Info

DATE

2018-09

AUTHORS

Z. G. Badredinov, B. A. Markovsky, I. A. Tararin, N. I. Ekimova, V. M. Chubarov

ABSTRACT

The mineral and chemical compositions of the layered subvolcanic ultrabasic rocks formed through fluid–silicate (liquid) separation of the ultrabasic magma into high-potassium and low-potassium fractions are characterized by the example of the layered picritic sill from the Late Cretaceous ultrabasic volcanic complex of Eastern Kamchatka. It is determined that the main potassium concentrator in the picrites from the high-potassium layers is a residual volcanic glass containing up to 8–9 wt % K2O, which is unique for ultrabasic melts. More... »

PAGES

408-418

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1819714018050032

DOI

http://dx.doi.org/10.1134/s1819714018050032

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1107428818


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