Abstract
Fransa'nın Güney Alpleri'nde yer alan Suzette ve Propiac-Condorcet diyapirleri, Oligosen öncesi Pireneo-Provensal fazının yaklaşık K-G doğrultulu sıkıştırma kuvvetleri sonucu, doğrultu atımlı fay zonlannda gelişmiş "en echelon" tansiyon çatlaklarına bağlı olarak yerleşmiştir. Bunlardan Suzette diyapiri, zamanla, söz konusu fay zonlan tansiyon çatlaklarına özgü "S" şeklini kazanmıştır. Suzette diyapirini örten Oligosen, Propiac-Condorcet diyapirlerini üstleyen Miyosen yaşlı birimler, diyapire yalan kesimlerde, diyapirlerin Tersiyer sonrası yükselimi sonucu yer yer dikleşmiş ve devrilmiş konumdadır.
Keywords
References
- ARNAUD, H., 1973, Mise en évidence d'un important décalage ante-miocène, de sens senestre, le long de la faille de Presles (Vercors oriental): C.R. Acad. Sc. Paris, 276, D, 2245-2248.
- BAUDRIMONT, A.F., DUBOIS, P„ 1977, Un bassin mesogeen du domaine peri-alpin; le SE de la France: Bull. Centre Reach. Explor.-Prod.Elf-Aquitaine, France, 1,1,261-308.
- BRASSEUR, R., 1962, Etude géologique du Massif de Suzette (Vaucluse): Thfcse, Lyon, 195 s. (yayınlanmamış;).
- EMRE, T., 1977, Contribution a l'etude de quelques diapirs du SE de la France, Thèse, Grenoble, 142 s. (yayınlanmamış;).
- EMRE, T. ve TRUC, G., 1978, Mise en Evidence d'un contact discordant Oligocene-Trias dans le Massif de Suzette. Implications tectoniques et consequences sur I' origine des evaporites ludiennes du bassin de Mormoiron (Vaucluse): Gfiologie Alpine, Grenoble, 54, 17-23.
- HILLS, E.S., 1963, Elements of structural geology: Methuen and Co LTD, London, s. 172.
- ROBERT, J.P., 1976, Les decrochements, fracturations et mouvements de blocs associes. Exemples des massifs subalpins Dauphinois: These, Grenoble, 155 s. (yayınlanmamış;).
- VIALON, P., RUHLAND, M., ve GROLIER, J., 1976, Elements de tectonique analitique: Masson et Cie, Paris, s. 22.
Abstract
The Suzette and Propiac-Condorcet diapirs of the Southern Alps of France, emplaced along "en echelon" tensional fractures of strike-slip fault zones which formed by the N-S compressional forces of the Pyreneo-Provincial phase of the pre-Oligocene time. The Suzette diapir has ultimately gained "S" shape, that is a characteristic structure of subjected fault zones of tensional fractures. The Suzette diapir is overlained by the Oligocene, and the Propiac-Condorcet diapirs by the Miocene successions. Both of these younger successions later were tilted and locally overturned by the reactivation of the diapirs.
Keywords
References
- ARNAUD, H., 1973, Mise en évidence d'un important décalage ante-miocène, de sens senestre, le long de la faille de Presles (Vercors oriental): C.R. Acad. Sc. Paris, 276, D, 2245-2248.
- BAUDRIMONT, A.F., DUBOIS, P„ 1977, Un bassin mesogeen du domaine peri-alpin; le SE de la France: Bull. Centre Reach. Explor.-Prod.Elf-Aquitaine, France, 1,1,261-308.
- BRASSEUR, R., 1962, Etude géologique du Massif de Suzette (Vaucluse): Thfcse, Lyon, 195 s. (yayınlanmamış;).
- EMRE, T., 1977, Contribution a l'etude de quelques diapirs du SE de la France, Thèse, Grenoble, 142 s. (yayınlanmamış;).
- EMRE, T. ve TRUC, G., 1978, Mise en Evidence d'un contact discordant Oligocene-Trias dans le Massif de Suzette. Implications tectoniques et consequences sur I' origine des evaporites ludiennes du bassin de Mormoiron (Vaucluse): Gfiologie Alpine, Grenoble, 54, 17-23.
- HILLS, E.S., 1963, Elements of structural geology: Methuen and Co LTD, London, s. 172.
- ROBERT, J.P., 1976, Les decrochements, fracturations et mouvements de blocs associes. Exemples des massifs subalpins Dauphinois: These, Grenoble, 155 s. (yayınlanmamış;).
- VIALON, P., RUHLAND, M., ve GROLIER, J., 1976, Elements de tectonique analitique: Masson et Cie, Paris, s. 22.
Details
| Primary Language | Turkish |
|---|---|
| Subjects | Geological Sciences and Engineering (Other) |
| Journal Section | Research Article |
| Authors | |
| Publication Date | April 15, 1987 |
| Submission Date | January 1, 1987 |
| Published in Issue | Year 1987 Volume: 11 Issue: 1 |
