首页 | 本学科首页   官方微博 | 高级检索  
     检索      


North-south transfer zones and paleo-morphological reconstruction of the Xylokastro area (Corinth Gulf, Greece)
Authors:Joachim Place  Yves Graud  Marc Diraison  Laurence Warr
Institution:

aÉcole et Observatoire des Sciences de la Terre, Institut de Physique du Globe de Strasbourg, UMR 7516, 1 rue Blessig, F-67084 Strasbourg Cedex, France

bÉcole et Observatoire des Sciences de la Terre, Centre de Géochimie de la Surface, UMR 7517, 1 rue Blessig, F-67084 Strasbourg Cedex, France

Abstract:A large number of studies have documented the structural and sedimentary architecture of the Corinth Gulf, especially the major E–W trending normal faults important in accommodating the main extensional strain and associated growth of the Gilbert fan deltas. However, the role of several N–S oriented structures that crop out at the surface and are detectable at depth by seismic reflection and gravity surveys are not clearly understood. Based on new geological data, collected near Xylokastro, we describe the N–S oriented tectonic activity of this area. The mapped inland faults correspond to off-shore structures identified in re-interpreted seismic lines and appear to have acted as a major transfer zone during the opening of the Corinth Gulf. Reconstruction of the paleo-topography based on sedimentary facies and the environment of clay mineral formation suggest these transfer zones played an important role in controlling both local structural relief and depositional conditions of the Gilbert fan deltas.
Keywords:Corinth Gulf  Fault network  Tilted blocks  Transfer zone  Clay minerals  Slope deposits  Geological analogue
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号