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occurrence of Primary Sedimentary structure c loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader031vdocumentinreader031viewer20220309125b5c4d247f8b9a9c398be134html5thumbnails2jpg width=140 height=200 divdivdiv class=ts-pagebutton class=gotoPage data-page=3Page 3button div class=ts-imageimg data-url=-if-on-a-geological-map-van-parallel-to-the-bedding-contacts-a-type-of-unconformityhtmlpage=3 data-page=3 class=ts-thumb lazyload alt=Page 3: €¦ · If on a geological map van parallel to the bedding contacts A type of unconformity characterized by the occurrence of Primary Sedimentary structure c loading=lazy src=data:imagegifbase64iVBORw0KGgoAAAANSUhEUgAAAAIAAAACCAQAAADYv8WvAAAAD0lEQVR42mP8X8AwAgiABKBAv+vAXklAAAAAElFTkSuQmCC data-src=https:reader031vdocumentinreader031viewer20220309125b5c4d247f8b9a9c398be134html5thumbnails3jpg width=140 height=200 divdivdiv class=ts-pagebutton 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