Extensional shear zones, granitic melts, and linkage of overstepping normal faults bounding the Shuswap metamorphic core complex, British Columbia

Bradford J. Johnson

(v. 118, no. 3/4, p. 366–382, doi: 10.1130/B25800.1)

In Figures 2 and 3, some of the text labels did not appear correctly and not all were visible. The corrected figures follow.


First Page Preview

First page PDF preview
You do not currently have access to this article.