a conglomerte bed as a possible lower boundary - Professor Kamal ...
a conglomerte bed as a possible lower boundary - Professor Kamal ...
a conglomerte bed as a possible lower boundary - Professor Kamal ...
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CHAPTER TWO<br />
STRATIGRAPHY AND SEDIMENTOLOGY<br />
Fig.2.8: Four limestone successions at the <strong>lower</strong> part of Qulqula Formation, west of<br />
Dostadara Village, N latitude 35 o 34 - 47.33 = and E longitude 45 o 46 - 45.63 = (P1, P2, P3<br />
and P4 are limestone successions).<br />
Fig.2.9: Geological cross section near Dostadara Village, p<strong>as</strong>sing directly by the west<br />
of Village sections.<br />
2-3.Criterion for Finding the Top and Bottom (Way Up) of the Limestone<br />
Members<br />
One of the difficulties that stand against this study is indicating whether these<br />
limestone successions are overturned or not. As the studied area is located in the<br />
Thrust Zone, the overturning is not excluded, due to imbrication and subsequent<br />
<strong>possible</strong> thrusting. To achieve these data, the field study w<strong>as</strong> conducted to indicate<br />
the top and bottom of the successions by using sedimentary structures. Most<br />
outcrops are almost devoid sedimentary structures. The useful structures are:<br />
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