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Imaging of Alpine and Post-Alpine Formations Using ERT at Loutsa- Remeri Open Pit Mine, Scourta, Viotia, Greece

Manoutsoglou Emmanouil, Vafeidis Antonios, Panagopoulos Georgios, Andronikidis Nikolaos, Hamdan, Hamdan, Pyliotis Ioannis, Kikidis L., Botos N.

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URIhttp://purl.tuc.gr/dl/dias/53D672C3-C180-4A3A-96FD-D2137AD93ADA-
Αναγνωριστικόhttps://doi.org/10.3997/2214-4609.201414122-
Γλώσσαen-
ΤίτλοςImaging of Alpine and Post-Alpine Formations Using ERT at Loutsa- Remeri Open Pit Mine, Scourta, Viotia, Greeceen
ΔημιουργόςManoutsoglou Emmanouilen
ΔημιουργόςΜανουτσογλου Εμμανουηλel
ΔημιουργόςVafeidis Antoniosen
ΔημιουργόςΒαφειδης Αντωνιοςel
ΔημιουργόςPanagopoulos Georgiosen
ΔημιουργόςΠαναγοπουλος Γεωργιοςel
ΔημιουργόςAndronikidis Nikolaosen
ΔημιουργόςΑνδρονικιδης Νικολαοςel
ΔημιουργόςHamdan, Hamdanen
ΔημιουργόςPyliotis Ioannisen
ΔημιουργόςΠυλιωτης Ιωαννηςel
ΔημιουργόςKikidis L.en
ΔημιουργόςBotos N.en
ΕκδότηςBalkan Geophysical Societyen
ΠερίληψηA geophysical survey carried out at Scourta plateau in Central Greece employed the electrical tomography method in order to image the interface between Alpine and Post-Alpine formations and estimate the thickness of Terra Rossa deposits. The later are crucial for TITAN-SA cement company open pit mine. This mine provides row materials for cement production. This survey is related with future extension plan of the existing Loutsa-Remeri open pit mine. Scourta is an active polje and is filled with a thick Terra Rossa deposit which is a row material for cement industry. The geophysical survey revealed two distinct layers, the upper is characterized by lower resistivity values (less than 20 Ωm), minimum thickness to the east (25 m) and maximum thickness at least 50 m and is attributed to Terra Rossa deposits. The underlying layer exhibits higher resistivity values (more than 70 Ωm) and is attributed to karstified carbonate relief. The variation of the polje depth is accosiated with tectonokarstic processes. The E-W direction fault system delineates the karstic structure and the N-S ridge in the east part of the survey area is delineated by N-S direction faults. el
ΤύποςΠλήρης Δημοσίευση σε Συνέδριοel
ΤύποςConference Full Paperen
Άδεια Χρήσηςhttp://creativecommons.org/licenses/by/4.0/en
Ημερομηνία2015-10-29-
Ημερομηνία Δημοσίευσης2015-
Θεματική ΚατηγορίαGeology--Surveysen
Θεματική Κατηγορίαgeological surveysen
Θεματική Κατηγορίαgeology surveysen
Βιβλιογραφική ΑναφοράA. Vafidis, N. Andronikidis, H. Hamdan, I. Pyliotis, G. Panagopoulos, E. Manoutsoglou, L. Kikidis and N. Botos, " Imaging of Alpine and Post-Alpine Formations Using ERT at Loutsa- Remeri Open Pit Mine, Scourta, Viotia, Greece," in 2015 8th Cong. of the Balkan Geop. Society. doi:10.3997/2214-4609.201414122en

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