Similar(59)
Initial deformation is characterised by the development of a layer parallel fabric (S1).
Line D19 intersects both abyssal hill and trench-parallel fabrics (Figure 2).
The porosity (39 to 67%) and Darcian permeability (3.1 × 10− 15 m2 perpendicular to fabric to 3.8 × 10− 11 m2 parallel to fabric) of fine ash emitted during ash jetting indicate that the permeable zones comprised highly sheared, tube-like bubbly magma, and contrast with the low porosity (~ 17%) and nul permeability of bombs ejected to hundreds of metres from the vent in Vulcanian blasts.
And then comes a satisfying wooden thump as the warp threads fall back in parallel, the fabric now one line nearer completion.
The liz/ctl fault gouges deformed at 60, 100, 140, 160, and 170 MPa all contain narrow (10 to 50 μm), localized shear zones that occur directly adjacent to the gabbro cylinder on both sides of the gouge (referred to as B shears), which exhibit shear-zone-parallel planar fabrics defined by a preferred crystallographic orientation (Figure 7A-D).
(B) Liz/ctl gouge (P c = 140 MPa), highlighting the development of a number of anastomosing Y and B shears, showing strong evidence of the preferred crystallographic orientation of serpentine (i.e., a distinctive shear-zone-parallel planar fabric).
The material displays a preferential fabric parallel to the previous topography.
The shuttle guide was positioned behind and parallel to the fabric, and at the height of the needles.
Hold your needle parallel to the fabric so you keep your stitches small.
Cut another few on the straight grain, or parallel to the fabric edge.
Too close your bag, you can sew on a button in the inside, and cut a hole in the fabric parallel to your button.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com