File:V. Bülow 2.jpg

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Deutsch: "Schematisierter und ca. 40-fach überhöhter Schnitt zur Situation im Untergrund der Griesen Gegend mit Salzdiapiren, der Randsenke Lübtheen, dem Einsturztrichter über dem Diapir Conow, der Diskordanz im obersten Pliozän und der übertiefen altpleistozänen Hagenower Rinne".
Date
Source "Die jüngere Erdgeschichte des Mineraldistriktes in der Griesen Gegend SW-Mecklenburgs"; Veröffentlichungen des Arbeitskreises Bergbaufolgen, Arbeitskreis der Deutschen Gesellschaft für Geowissenschaften e.V. (DGG); Exkursionsführer und Veröffentlichungen, Berlin/Hannover, Nr. 234 (207), Seiten 29-35; hier auf Seite 31.
Author Werner von Bülow

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Date/TimeThumbnailDimensionsUserComment
current07:32, 15 May 2013Thumbnail for version as of 07:32, 15 May 20132,292 × 1,087 (680 KB)Berginspektor (talk | contribs)
14:15, 14 May 2013Thumbnail for version as of 14:15, 14 May 20132,264 × 1,076 (618 KB)Berginspektor (talk | contribs)
14:13, 14 May 2013Thumbnail for version as of 14:13, 14 May 20132,442 × 1,375 (607 KB)Berginspektor (talk | contribs){{Information |Description= "Schematisierter und ca. 40-fach überhöhter Schnitt zur Situation im Untergrund derGriesen Gegend mit Salzdiapiren, der Randsenke Lübtheen, dem Einsturztrichter über dem Diapir Conow, der Diskordanz im obersten Pliozän ...

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