Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5783989 | Lithos | 2017 | 54 Pages |
Abstract
The estimated PTt path documents the ca. 10Â Ma evolution cycle of the OSD characterized by two distinct periods: (1) 347 - >Â 342Â Ma period corresponds to nearly isothermal decompression resulting from crustal scale folding and vertical extrusion of granulites, and (2) at >Â 342-337Â Ma which corresponds to a fast, nearly isobaric cooling.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Katarzyna Walczak, Robert Anczkiewicz, Jacek SzczepaÅski, Daniela Rubatto, Jan KoÅ¡ler,