KINK-BANDS, CONTRACTIONAL OR REVERSE
The difference between the normal and reverse kink bands is shown in
figure accompanying this text. If the compressive stress acts parallel to
the layering, conjugate kink-bands or box folds are produced but if it
acts at an angle to the layering, a single set of kink-bands are developed
more or less at the exclusion of the other. Patterson and Weiss (1966)
produced conjugate and single kink-bands experimentally and one of their
significant conclusions has been that under large shortening, kink-bands
are converted into chevron folds. Dewey (1966) made significant
contribution towards our understanding of the nature and origin of
kink-bards and Arvid Johnson and his coworkers have presented through a
series of papers (see 1976 numbers of Tectonophysics) the origin of
kink-bands by extensive theoretical treatment of the problem of their
origin and geometry. Such kink-bands are called reverse or contractional kink-bands.
Conversely, if the orthogonal thickness within the kink-band is
systematically reduced than that in the un-deflected layering the
kink-bands are called normal or extensional kink-bands. The difference
between the normal and reverse kink bands is shown in figure. The axial plane normally bisects the angle between kinked and
unkinked sectors but this is not true if there is dilation within the
kinked zone (D ) so that the angles b1
and
b2
are not equal(see Figure below).
In this case the amount of orthogonal
thickness is increased by an amount dt.
The dilation D
or d t/t is given by : D
=[(sin b2)/(sin
b1)]-1 If b2>
b1, then there is
reduction in volume within the kink-band
and dilation will take
negative value. Positive dilation however
is more common in naturally developed rocks.
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