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Deutsch: Oberkreidediskordanz im Geologischen Garten Bochum: Basale Schichten der Essen-Grünsand-Formation („Essener Grünsand“, Cenoman, Oberkreide) überlagern transgressiv die verkippten Sand-, Silt- und und Tonsteine der Bochum-Formation („Bochumer Schichten“, Westfal A, Oberkarbon) zwischen Flöz „Wasserfall“ und Flöz „Dünnebank“.[1]
English: Upper Cretaceous angular unconformity at Bochum Geologischer Garten: Basal beds of the Essen Greensand Formation (Cenomanian, Upper Cretaceous) transgressivley overlying tilted sand- and mudstones in between coal seams ‘Wasserfall’ and ‘Dünnebank’ of the Bochum Formation („Bochum Beds“, Westfalian A, Upper Carboniferous/Pennsylvanian).[1]
  1. a b cf. pp. 23–25 and 27/28 (figs. 18, 23, and 29) in: Till Kasielke (2015): Geologie und Reliefentwicklung im Raum Bochum [Geology and landform evolution in the area of Bochum]. Veröffentlichungen des Bochumer Botanischen Vereins. 7(3):15–36 (PDF 15 MB)
Date
Source Self-photographed
Author Hermann A. Wiese

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22 November 2006

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Date/TimeThumbnailDimensionsUserComment
current01:40, 23 September 2006Thumbnail for version as of 01:40, 23 September 20062,048 × 1,536 (1.68 MB)Arglos{{Information |Description=Gesteinsschichtung Kreide und Karbon |Source=eigenes Bild / own work |Date=Freitag, 22.11.06 |Author=Hermann A. Wiese}}

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