LITHOLOGIC, TECTONIC AND CLIMATIC FACTORS CONTROLLING THE KARSTIFICATION ON THE NORTH AQUITAINE MARGIN - EXAMPLE OF OLIGOCENE LIMESTONES

Citation
A. Klingebiel et al., LITHOLOGIC, TECTONIC AND CLIMATIC FACTORS CONTROLLING THE KARSTIFICATION ON THE NORTH AQUITAINE MARGIN - EXAMPLE OF OLIGOCENE LIMESTONES, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 317(4), 1993, pp. 523-529
Citations number
15
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
07644450
Volume
317
Issue
4
Year of publication
1993
Pages
523 - 529
Database
ISI
SICI code
0764-4450(1993)317:4<523:LTACFC>2.0.ZU;2-Z
Abstract
The ''Entre-deux-Mers'' region (Gironde), is a moving panel of the sta ble North-Aquitaine margin. It is overlain by Oligocene shallow water carbonate deposits with high porosity (grainstones, packstones, bounds tones), or low porosity (mudstones and wackestones) facies. During the Plio-Pleistocene period, a fault system, resulting from Pyreneo-Alpin e orogenesis, induced a karstic network related to tectonic fracturati ons, high porosity Oligocene facies distribution and glacio-eustatic s ea-level variations.