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DYNAMICS and ACTIVE PROCESSES - International Lithosphere ...

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Minerals identification by XRD indicated that<br />

the main minerals are quartz, feldspar, mica<br />

chlorite, smectite (after the treatment of the<br />

samples) <strong>and</strong> a small quantity of serpentine.<br />

However, minor amount of feldspar is still<br />

SEM-EDS<br />

present in many of the samples (Fig.2), <strong>and</strong><br />

trace amounts of calcite <strong>and</strong> dolomite are also<br />

present in many samples(before the treatment<br />

of the samples with the acids).<br />

As a confirmation of XRD analyses even<br />

under SEM the minerals identified in thin<br />

sections are: quartz, as the main constituent,<br />

dolomite in form of cement, feldspar<br />

weathered into clay minerals (chlorite),<br />

Fig.2 XRD pattern of sample Alb_34 B/22/1 from the study area.<br />

Fig.3 Several minerals identified at thin section no.<br />

Alb_66_01. Q- Quartz; M-Muscovite; Fsp-Feldspars;<br />

Do-Dolomite; I-Ilmenite; R-Rutile; Zr-Zircon<br />

147<br />

biotite elongated like flakes, white dots of<br />

pyrite, muscovite is also present (Fig.4), in its<br />

composition has a considerable quantity of<br />

Mg <strong>and</strong> Ca, because of dolomite cement. To<br />

notice is the presence of many minerals which<br />

are accessory minerals in igneous rocks, like<br />

ilmenite, monazite, zircon (Fig.3) etc.<br />

Conclusion<br />

Fig.4 EDS spectrum for muscovite.

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