1. Orthogneiss mylonite and non-coaxial deformation in granites: the example of the south Armorican shear zone;Berté;J. Struct. Geol.,1979
2. The geology of the crystalline rocks near Baltimore and its bearing on the evolution of the eastern Maryland Piedmont;Crowley;Maryland Geol. Surv. Rept. of Inv.,1976
3. Gates, A. E. In press. Shear zone control on mineral deposits in the State-Line serpentinite. In: Applications to Exploration (edited by Petruk, W., Vassiliou, A. H. & Hausen, D.). Ore Geol. Rev. 3.
4. Comparison of the natural deformation of the State-Line serpentinite, U.S.A., with experimental studies;Gates;Tectonophysics,1990
5. Gates, A. E., Muller, P. D. & Valentino, D. W. In press. Terranes and tectonics of the Maryland and southeast Pennsylvania Piedmont. In: Field Trip Guide for the 1991 Northeast/Southeast Geological Society of American Meeting (edited by Schultz, A. P.). Virginia Museum Publ.