File:V. Bülow 2.jpg
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| Description |
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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I, the copyright holder of this work, hereby publish it under the following license:
This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
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- attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 07:32, 15 May 2013 | | 2,292 × 1,087 (680 KB) | Berginspektor (talk | contribs) | |
| 14:15, 14 May 2013 |  | 2,264 × 1,076 (618 KB) | Berginspektor (talk | contribs) | ||
| 14:13, 14 May 2013 |  | 2,442 × 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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