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GOHMISSION GEOLOGIQVE - Arkisto.gsf.fi

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Suomen Geologinen Seura. N:o 12. Geologiska Sallskapet i Finland. 25<br />

the ends of the box and the whole block reduced to about l/, of its<br />

original thickness. The pressure needed was a few kg/cm2. The clay<br />

was then lifted out of the box. The sides or a section were then photographed.<br />

Plates 1 and II show the middle portion of some experiments.<br />

When the paraf<strong>fi</strong>ne layer remained in the centre it was crumpled<br />

up into folds that are identical with natural ptygmatic folds. Generally<br />

a slightly greater amount of clay flowed out of one of the apertures<br />

and the paraf<strong>fi</strong>ne layer was then bent into a looped shape (Plate<br />

II, <strong>fi</strong>g. 1). This case represents the mechanism of folding with a flat<br />

lying anticlinal axial plane. The result is similar to that of nature.<br />

Fig. 6. Set-up of experimenta on ptygmatic folding.<br />

Experimental ptygmatic folding.<br />

We <strong>fi</strong>nd flat and even drawn out limbs (D) combined with a crumpled<br />

anticlinal apex (compare <strong>fi</strong>g. 1). Inspection of Plate 1, <strong>fi</strong>g. 2, A<br />

shows that the wavelength of the folds increases with the thickness<br />

of $he sheet of paraf<strong>fi</strong>ne. By changing the consistency of this layer<br />

the wavelength can also easily be altered.<br />

In <strong>fi</strong>g. 2, Plate II the dark lines in C are the outcrop of originally<br />

plane surfaces parallel to the hard layer painted black. But the tendency<br />

of the clay to slip along horizontal shearing planes hae given<br />

. a stepped outline to the sections. In A and B the thick line shows the<br />

curve that would have ensued in perfectly plastic movement. The<br />

dying out of the contortions away from the controlling vein is well<br />

demonstrated.<br />

Another inference can be drawn from the experiments. For simplicity<br />

1 allowed only two opposing directions of escape for the clay.<br />

If the vein is placed in the plane containing the directions both of<br />

compression and elongation it is not folded. This is sirnply because<br />

it stretches together with the clay to compensate the compression. A<br />

more brittle layer, however, was not internally deformed but torn apart<br />

and the loose pieces were folded. Spurr thought the flow during gneissic

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