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a conglomerte bed as a possible lower boundary - Professor Kamal ...

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CHAPTER TWO<br />

STRATIGRAPHY AND SEDIMENTOLOGY<br />

2.4.1- Upper Boundary at the Northwestern Part of the Studied Area (NP)<br />

The northwestern part of the studied area is located 20 km to the north of Qaladiza<br />

Town. In this area, the <strong>lower</strong> <strong>boundary</strong> of the formation is not exposed while the<br />

upper <strong>boundary</strong> forms tectonic contact with the Red Bed Series. In this area Baziany,<br />

(2006) recorded and descri<strong>bed</strong> angular unconformity between the Red Bed Series<br />

and the underlying Qulqula Formation in Qulqula gorge, Qandil Mountain toe and<br />

north of B<strong>as</strong>ne Town (Figs.2.16 and 2.17). In these two are<strong>as</strong>, the Red Bed Series<br />

overlies the Qulqula Formation in angular unconformable condition. The dip angle<br />

(dip angle of the plane of angular unconformity) is equal to 17 o and 21 o respectively.<br />

Above the unconformity, the Late Cretaceous rocks are missing from stratigraphic<br />

section of Cenozoic.<br />

Fig. 2.16: Angular unconformity between Red Bed Series and Qulqula Formation at<br />

Northwest of Qaladiza Town (Baziany, 2006).<br />

Fig.2.17: Angular unconformity between Red Bed Series and Qulqula Formation at<br />

Northwest of Qaladiza Town (Baziany, 2006).<br />

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