Une mégaséquence d'émersion: la Lettenkohle (Trias Est de la France). Mise en évidence de marées par l'imbrication bipolaire de plaques de dessiccation-Reference-Cited by-同舟云学术

Une mégaséquence d'émersion: la Lettenkohle (Trias Est de la France). Mise en évidence de marées par l'imbrication bipolaire de plaques de dessiccation

Published:1987-06 Issue:2 Volume:76 Page:579-597
ISSN:0016-7853
Container-title:Geologische Rundschau
language:fr
Short-container-title:Geol Rundsch

Author:

Duringer Philippe

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/BF01821093.pdf

Reference90 articles.

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2. Alesi, von E. (1984): Der Trigonodus-Dolomit im Oberen Muschelkalk von SW Deutschland. - Arb. Inst. Geol. Palä ont. Univ., NF 79, 1–53, Stuttgart.

3. Aust, H. (1969): Lithologie, Geochemie und Paläontologie des Grenzbereichs Muschelkalk-Keuper in Franken. - Abh. Naturw. Ver.,10, 3–155, Würzburg.

4. Bachmann, G. H. (1979): Bioherme der MuschelPlacunopsis ostracina und ihrer Diagenese. - N. Jb. Geol. Paläont. Abh., 381–407, Stuttgart.

5. - &Gwinner, M. P. (1971): Algen-Stromatolithen von der Grenze Unterer/Mittlerer Keuper bei Schwäbisch Hall (Nordwürttemberg).- N. Jb. Geol. Paläont. Mh., 594–604, Stuttgart.

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