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DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...

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The primary purpose of this study is to<br />

determine the textural <strong>and</strong> mineralogical<br />

characteristics of this Neogene unit in respect<br />

to their genetic relationship. The second is to<br />

determine the principal minerals in the study<br />

area. The third <strong>and</strong> the most important is to<br />

identify the clay minerals, <strong>and</strong> to give a full<br />

description of them. Realizing all of this<br />

objectives, can give to us a useful <strong>and</strong> an<br />

exact information of the forming history of<br />

the sediments this area.<br />

2- METHODS of STUDY.<br />

Fig.1 Geological Map of Tirana Depression (According to the Geological<br />

Map of Albania. 1:200 000).<br />

In this study 11 clay samples were collected<br />

from the bottom to the top of the section. The<br />

mineralogical characteristics of the samples<br />

were determined through several techniques,<br />

including XRD <strong>and</strong> SEM-EDS methods. For<br />

petrographic studies <strong>and</strong> electron microscopy<br />

9 normal thin sections were prepared from the<br />

most characteristic samples. The mineralogical<br />

composition of the samples was<br />

examined using X-Ray Diffraction under<br />

CoK� radiation, with a step scanning 3 to<br />

60º2� in steps of 0.01º2� with a counting time<br />

of 1.00 s per step. First X-ray Diffraction<br />

Analyses were done from the samples in natural<br />

conditions <strong>and</strong> after this were selected the 2 most<br />

representative samples. The analyses aimed at<br />

documenting the gross mineralogy, <strong>and</strong> specially<br />

clay mineralogy of Brari Section. A clay fraction<br />

(< 2 µm) was separated out from the samples by<br />

disaggregating with different acids according to<br />

Jackson Method <strong>and</strong> dispersing the sample in<br />

distilled water <strong>and</strong> immediately washed by<br />

centrifugation. The fraction of < 2 µm was<br />

isolated by centrifugation <strong>and</strong> suspension were<br />

dried on glass slides. The clay samples in oriented<br />

mounts were run under three separate conditions:<br />

1) air dry state.<br />

2) after heating to 550º C for 2 hours <strong>and</strong><br />

3) after ethylene glycol treatment<br />

3- RESULTS <strong>and</strong> DISCUSSION. X-ray diffraction<br />

146<br />

Brari<br />

The digital data were interpreted using X-Pert<br />

Highscore Plus software, which comprises a<br />

search-match routine based on a Powder<br />

Diffraction File.

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