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Article
Author(s)
BOUHLASSA Saddek, FEHDI Chemseddine and BOUBAYA Djamel
Full-Text PDF XML 1028 Views
DOI:10.17265/1934-7391/2017.05.004
Affiliation(s)
Department of Geology, Larbi Tebessi University, Tebessa 12002, Algeria
ABSTRACT
This study presents the results and the interpretation of a microgravity
survey realized in the MChentel zone near Cheria tone situated in the Northeast
Algerian. The microgravity survey, made during April and March, 2016, allowed
the obtaining of 614 measures distributed on the whole zone of study. The gravimetric data
were measured by means of a gravimeter relative GNU-KC 444 were used with
location and the height of stations with centimetric precision by pocket GPS and
an electronic theodolite type Qeo FET 420 k. The gravimetric data measured on
the ground were connected with a reference gravimetric station situated near
the zone of study. On the scale of the zone
of study, the gravimetric data show a decrease of the values of the anomaly of
Bouguer between both collapses. This trend implies probably an effect of
karstification which would explain the
decrease of the values of the anomaly of Bouguer by going to the center of the
studied zone. The interpretation of gravimetric data shows the presence
essentially of two negative zones, they present a deficit of in-depth mass
which can be 30 meters.
KEYWORDS
Microgravity survey, MChentel, Bouguer anomaly.
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