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Tansiyon çatlaklarında gelişen diyapirler

Diapirs Emplacement Along Tensional Fractures

Journal Name:

  • Jeoloji Mühendisliği Dergisi

Publication Year:

  • 1987
Author NameUniversity of AuthorFaculty of Author
Abstract (2. Language): 
The Suzette and Propiac-Condorcet diapirs of the Southern .Alps of France» emplaced along '"en echelon11 tensional fractures; of strike-slip fault, zones; which formed by the N-S compressional forces of the. Pyreneo-Provînctal plias« of the pre-Oligocene time., The Suzetle diapir has ultimately gained "SM sha|pes that. is. a, characteristic structure of subjected fault zones of tensional fractures., The Suzette diapir is overlained by the Oligocène» 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.
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Abstract (Original Language): 
Fransa'nın Güney Alplerftıde yer alan Suzette ve Prognac-Candarcet diyapMeıi, Oligosen öncesi Pireneo-Provensal faznnn yaklaşık K-G do-ğrultulu sıkıştııma 'kuvveden sonucu, doğrultu .alimi fay zonlannda .gelişmiş "en echelon*' tansiyon çatlaklarına bağlı olarak yerleşmiştir. Bunlardan Suzette diyapiri.,, zamanla» sözkonusu fay zonlaa tansiyon çatlaklarına, dzgp. "S" şeklini kazanmıştır.. Suzette diyapirini örten Oligosen, Propiac-Condorcet dryapuierini flsdeyen Miyosen yaşlı birimler, diyapire yata kesimlerde» diyapirlerin Tersiyer sonrası yükselimi sonucu, yer yèr «ödeşmiş ve. devrilmiş konumdadır...
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17-20
  • Turkish

REFERENCES

References: 

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