Bulletin of the Geological Society of Denmark, Vol. 27/01-02, pp. 15-45
Bulletin of the Geological Society of Denmark, Vol. 27/01-02, pp. 15-45
Bulletin of the Geological Society of Denmark, Vol. 27/01-02, pp. 15-45
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<strong>Bulletin</strong> <strong>of</strong> <strong>the</strong> <strong>Geological</strong> <strong>Society</strong> <strong>of</strong> <strong>Denmark</strong>, vol. <strong>27</strong> 1978 <strong>27</strong><br />
Fig. 10. T-D diagrams for <strong>the</strong> pr<strong>of</strong>ile lines 1, 4, 7, 10 and 13. is not parallel with <strong>the</strong> shoreline, <strong>the</strong> pr<strong>of</strong>ile is changing and <strong>the</strong><br />
Time is abscissa and <strong>the</strong> pr<strong>of</strong>ile <strong>the</strong> ordinate, indicated by polenumbers.<br />
When an isoline is parallel with <strong>the</strong> time-axis, <strong>the</strong> loca<br />
and <strong>the</strong> x-axis.<br />
speed <strong>of</strong> this change increases by <strong>the</strong> angle between <strong>the</strong> isoline<br />
tion <strong>of</strong> <strong>the</strong> level is stable in relation to <strong>the</strong> shoreline. If <strong>the</strong> isoline
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