Striped bedding-veins are veins that lie subparallel to bedding and have an
internal layering or lineation at a small angle to the veins' long axis. T
hey form during bedding-parallel slip and can be used as shear sense indica
tors. Solid inclusion trails produce the visible internal layering or linea
tion and track the opening direction of the veins. Elongate quartz crystals
however can be oriented at an angle of up to 80 degrees to the opening dir
ection, are non-tracking, and contain almost no information on the shear se
nse. The striped bedding-veins can be separated into three types according
to the geometry of their internal segmentation. Veins of type B opened para
llel to jogs oriented at a low angle to bedding, veins of type J opened par
allel to jogs oriented at a high angle to bedding and veins of type O opene
d orthogonal to bedding and jogs. Striped bedding-veins of types B and J co
ntain crack-seal inclusion bands and displacement parallel inclusion trails
. Striped bedding-veins of type O feature only crack-seal inclusion bands.
The example of striped bedding-veins presented in this paper from the Orobi
c Alps of Italy belongs to type B. The lineation in the veins and the orien
tation of the inclusion bands and inclusion trails, as well as the orientat
ion of steps in the vein wall, can be used to determine the sense of shear
and the direction and amount of Vein opening or bedding-parallel slip. (C)
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