Abstract
The Guerrero terrane in southern Mexico (Figure 1) is considered a major tectonostratigraphic accretion to the Mesozoic continental crust of Mexico, and essentially lacking an old continental basement (Campa and Coney, 1993; Centeno-García et al.,1993)… in order to continue, download the full paper in PDF.
This work is licensed under a Creative Commons Attribution 4.0 International License.
Downloads
Download data is not yet available.