Title of article
Recent syn-rift deposits in the hangingwall of the Aigion Fault (Gulf of Corinth, Greece)
Author/Authors
Lemeille، نويسنده , , Francis and Chatoupis، نويسنده , , Fanis and Foumelis، نويسنده , , Michaili and Rettenmaier، نويسنده , , Detlev and Unkel، نويسنده , , Ingmar and Micarelli، نويسنده , , Luca and Moretti، نويسنده , , Isabelle and Bourdillon، نويسنده , , Chantal and Guernet، نويسنده , , Claude and Müller، نويسنده , , Carla، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2004
Pages
10
From page
425
To page
434
Abstract
Recent deep boreholes Γ1 (205 m) and AIG 10 (1001 m), performed in the Aigion area, bring new information on syn-rift deposits. MIS1/Holocène (11.8–4.3 ka BP) and Upper Pleistocene are identified in the upper part of the boreholes. Below Holocene deposits, the borehole AIG 10 crossed successively a detrital system with fine intercalations and a thick development of clay. No specific dating was possible on this lower formation, so the age of the local basal syn-rift deposits is discussed. To cite this article: F. Lemeille et al., C. R. Geoscience 336 (2004).
Keywords
Sedimentation , subsidence , subsidence , Gulf of Corinth , Greece , Grèce , golfe de Corinthe , syn-rift deposits , depôts syn-rift , sédimentation
Journal title
Comptes Rendus Geoscience
Serial Year
2004
Journal title
Comptes Rendus Geoscience
Record number
2279770
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