Coronitic textures in the ferrogabbros of the Elet’ozero intrusive complex (Northern Karelia, Russia) as evidence for the existence of Fe-rich melt. 2. Origin of Fe-rich liquid

Volume: 55, Issue: 7, Pages: 621 - 628
Published: Jul 1, 2017
Abstract
The study of coronitic textures in ferrogabbros and data on rhythmic layering of the Elet’ozero Massif supports the existence of a specific low-temperature Fe-rich liquid in nature. This liquid was formed during solidification of intrusion owing to the local multiple accumulation of Fe and Ti contents in a parental Fe-rich Fe–Ti basaltic melt. According to obtained data, this occurred on micro- and macroscale: 1) in the interglanular...
Paper Details
Title
Coronitic textures in the ferrogabbros of the Elet’ozero intrusive complex (Northern Karelia, Russia) as evidence for the existence of Fe-rich melt. 2. Origin of Fe-rich liquid
Published Date
Jul 1, 2017
Volume
55
Issue
7
Pages
621 - 628
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