Skip navigation
Skip navigation

Ordovician-Silurian rift-passive margin on the Mexican margin of the Rheic Ocean overlain by Carboniferous-Permian periarc rocks: Evidence from the eastern Acatlan Complex, Southern Mexico

Morales-Gámez, Miguel; Keppie, J. Duncan; Norman, Marc


In the Xayacatlán area of the Acatlán Complex in southern Mexico, several, N-S, fault-bounded packages of rocks occur (from west to east): (i) greenschist facies, interbedded psammites and pelites (Huerta Unit): the youngest concordant detrital zircon i

CollectionsANU Research Publications
Date published: 2008
Type: Journal article
Source: Tectonophysics
DOI: 10.1016/j.tecto.2008.01.014


File Description SizeFormat Image
01_Morales-Gámez_Ordovician-Silurian_2008.pdf2.94 MBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  19 May 2020/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator