By G. M. Bennison (auth.)
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Extra info for An Introduction to Geological Structures and Maps
O::;. ::::::- .................... . I~ •••••••• .... I .... .. . .... ...... :;.... /a-!. . . . ·d····· -: ....... o . ·~ ...... • . • . • n(j ' ......... /" " ", / ,\()if I "\ / J / / -- ( ) I ". / - <-,() / ..... -100 - __ -. --- 0/ SO" ..... Map 20 Deduce the main structural features from the outcrop patterns. Insert the fold axial traces on the map. Draw a geological section along the line X-Y. Insert on the map the sub-Permian Limestone outcrops of the coal seam, the sandstone and the fault plane.
Reproduced by permission of the Director General, British Geological Survey: NERC copyright reserved. 33 o Map 14 34 SCALE metres 500 Pre- and post-unconformity faulting After the deposition of the older set of strata earth movements causing uplift may also give rise to faulting of the strata. The unconformable series (the younger set of beds), not being laid down until a later period, are unaffected by this faulting. Earth movements subsequent to the deposition of the unconformable beds would, if they caused faulting, produce faults which affect both sets of strata.
8 Lower Cretac. ".