GEOLOGICAL AND MAGNETIC SUSCEPTIBILITY MAPPING OF MOUNT GIOUCHTA (CENTRAL CRETE)

 
This item is provided by the institution :

Repository :
Bulletin of the Geological Society of Greece  | ΕΚΤ eJournals
see the original item page
in the repository's web site and access all digital files if the item*
share




2010 (EN)
GEOLOGICAL AND MAGNETIC SUSCEPTIBILITY MAPPING OF MOUNT GIOUCHTA (CENTRAL CRETE) (EN)

Kamberis, E.
Kokinou, E.
Sarris, A.
Tzanaki, I.

Giouchta Mt. is located south of Heraklion city, in Crete. It is an N-S trending morphological asymmetric ridge, with steep western slope whilst the eastern slope represents a smoother relief, composed of Mesozoic limestone and Eocene- lower Oligocene flysch sediments of the Gavrovo -Tripolis zone. The present study focuses on the geological structure of Mt. Giouchta. Field mapping and tectonic analysis is performed for this purpose. The dominant structures are contractional in nature, deformed by normal faulting related to the extensional episodes initiated in Serravallian times. The strain pattern in the area is revealed from strain analysis. It is inferred that the orientation of the stress field in the area has changed several times: the N-S, stress field which was dominant during Late Serravallian times changed to NE-SW (in Late Serravallian? - Early Tortonian) and subsequently to WNW-ESE (Early to Middle Tortonian) to become NW-SE in Late Tortonian. This orientation changed also during the Quaternary times trending from NW-SE (Early Pleistocene) to ENE-WSW (Middle Pleistocene-Holocene). In addition to the above, surface soil samples were collected in the wider area of mount Giouchta and they were analyzed in order to determine the magnetic susceptibility. GIS techniques were used for mapping the spatial distribution of the geological features and the magnetic measurements on the topographic relief of the area. Statistical analysis techniques were also applied in order to investigate the relation of faulting and magnetic susceptibility. Maps representing the spatial distribution of the above measurements were created by using appropriate interpolation algorithms. (EN)

info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion

Heraklion basin (EN)
fault scarp (EN)
Southern Greece (EN)
Gavrovo-Tripolis zone (EN)

Ελληνική Γεωλογική Εταιρεία (EL)
Geological Society of Greece (EN)

Δελτίο της Ελληνικής Γεωλογικής Εταιρίας

2010-01-01


Geological Society of Greece (EN)

0438-9557
2529-1718
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Vol 43, No 1 (2010): 12th International Conference of the G.S.G.; 289-298 (EL)
Bulletin of the Geological Society of Greece; Vol 43, No 1 (2010): 12th International Conference of the G.S.G.; 289-298 (EN)

Copyright (c) 2017 E. Kokinou, E. Kamberis, A. Sarris, I. Tzanaki (EN)



*Institutions are responsible for keeping their URLs functional (digital file, item page in repository site)