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Chapter Four Depositional Environmenment and Paleoecology Sirwan sections and later one from P.hariaensis Zone to S. triloculinoides Zone (Upper Late Maastrichtian-Lower Danian), the graphical line shows best-fit line of 45 0 which indicate similar rate of depositions. If a best-fit line can be constructed completely, the sections can be correlated, (Sirwan and Qulka) (Fig 4.10) which show the same rate of deposition in the same geologic time from Late Maastrichtian- Early Danian. This technique provides a clear graphical method which aids in the correlation or sequences. Fig (4.8): Graphic correlation shows the depositional rate of sediment between Smaquli and Qulka sections, Note: Change in the gradient in the early stage (dog-Leg) indicate highest rate of deposition in Qulka section than Smaquli section 106
Chapter Four Depositional Environmenment and Paleoecology Fig (4.9): Graphic correlation shows the depositional rate of sediment between Smaquli and Sirwan sections. Note: Change in the gradient in the early stage (dog-Leg) indicate highest rate of deposition in Sirwan section than Smaquli section Fig (4.10): Graphic correlation shows the depositional rate of sediment between Qulka and Sirwan sections. Note: NO Change in the gradient observed, a best-fit line constructed completely which indicate similar rate of deposition in Qulka and Sirwan section. 107
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BIOSTRATIGRAPHY AND PALEOECOLOGY OF
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IV Dedicated: To My Wife My Daughte
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VI Abstract The Cretaceous / Tertia
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VIII successions from the upper par
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3.2.1.4- Pseudotextularia intermedi
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XII Table No. Title Page Table (3.1
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XIV Fig (4.11): Sedimentation rate
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Chapter one Introduction such as pl
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Chapter one Introduction Fig. (1.1)
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Chapter one Introduction lithologic
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Chapter one Introduction The Shiran
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Chapter one Introduction Abdel-Kire
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Chapter one Introduction The Kolosh
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Chapter one Introduction 1.4.2.2- R
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Chapter one Introduction a- Globotr
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Chapter one Introduction Fig (1, 6)
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Chapter one Introduction 4- Kato se
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Chapter one Introduction 1.8 -The a
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Chapter Two Lithostratigraphy Fig (
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Chapter Two Lithostratigraphy 2.3-
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Chapter Two Lithostratigraphy mediu
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Chapter Two Lithostratigraphy white
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Chapter Two Lithostratigraphy The u
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Chapter Three Biostratigraphy CHAPT
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Chapter Three Biostratigraphy (1988
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Chapter Three Biostratigraphy C R E
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Chapter Three Biostratigraphy U P P
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Chapter Three Biostratigraphy 3.2.1
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Chapter Three Biostratigraphy age e
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Chapter Three Biostratigraphy Pessa
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Page 134 and 135: Chapter Five Conclusion 16- The ter
Page 136 and 137: REFERENCES Abawi, T. S. Abdel-Kiree
Page 138 and 139: Northwestern Iraq. Rafidain Journal
Page 140 and 141: Bandy, O. L., 1967. Cretaceous plan
Page 142 and 143: limestone from the accretionary pri
Page 144 and 145: Cretaceous of the south Constantine
Page 146 and 147: James, G. A. and Wynd, J. G., 1965.
Page 148 and 149: Kassab, I. I. M., 1975c. Planktonic
Page 150 and 151: Liu, C. and Olsson, R. K., 1992. Ev
Page 152 and 153: Molina, E. Arenillas, I. and Arz, J
Page 154 and 155: Petters, S. W. EL-Nakhal, H. A. and
Page 156 and 157: Sissakian, V. K., 2000. Geological
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PLATE -7 Scale bar represents magni
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PLATE -9 Scale bar represents magni
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PLATE -11 Scale bar represents magn
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PLATE -17 Figs 1- 3 Globotruncana a
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PLATE -19 Figs. 1 Gansserina wieden
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PLATE -21 Figs 1-2 Abathomphalus ma
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PLATE -23 Fig. 1 Globigerinelloides
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