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

More documents

Recommendations

Info

CHAPTER ONE INTRODUCTION 1.5. Aims of the Study 1. The purpose of the present work is to establish depositional environment and paleogeographic setting of the limestones successions of the Qulqula Formation through facies analysis and geochemistry. 2. The study of the geochemical and sedimentological variations within and between the four limestone successions in five sections with a possible interpretation of the depositional environment as another purpose of the present study. This includes distribution of the major and some trace elements in the bulk samples and their separated insoluble residues 3. This study tries to see if the four successions are repetition of single succession by imbrications and faulting (thrusting) or they are different successions which are related to different time and space. 1.6-Studied Sections. Five sections are selected for detailed study of the Lower part of the Qulqula Radilarian Formation. As previously mentioned, the studied area consists of very long belt in the Thrust Zone which includes three discontinuous parts (see section 2.1 and fig.1.2). According to these parts, the sampled sections are grouped as follows: 1-6-1. Sections of Central or Middle Part of the Studied Area (MP) Kaolos Section This section is located directly in the south of Kaolos village, in the extreme southeastern of the middle part of studied area, bout 15 Km to the north of Said Sadiq town at latitude N 35 o 29 - 13.89 = and longitude E 45 o 52 - 1.47 = (Fig. 1.2 and 1.4A). This section consists of two successions which have less thickness than others in which each is about 15m thick... Dostadara Section This section is located nearly in the middle part of this area, directly to the west of Dostadara village, about 12 Km to the northeast of Barzinja town (Fig. 1.2 and 1.4A). Located at latitude N 35 o 34 - 47.33 = and longitude E 45 o 46 - 45.63 = . This section consists of four successions, each one of average 25m thickness. 9
CHAPTER ONE INTRODUCTION Gali Section This section is located about 1Km to the east of the Chuwarta Town, at the extreme northeastern part of the middle part of studied area (Fig.1.2 and 1.4B). Located at latitude 35 o 38 - 54.08 = and longitude 45 o 41 - 13.67 = . Dostadara and Gali section consist of four successions each more than 25 thick). 1.6.2- Section of the Southeastern Part Tawella Section It is located at latitude 35 o 25 - 48 = and longitude 46 o 02 - 41 = , at the 15km northeast of Halabja town (Fig.1.1). The section is located directly to the east of Tawela town at the extreme southeastern end of the studied area. In this area only one succession is sampled because the other succession located near the border of Iran. 1.6.3- Section of the Northwestern Part Type Section (Qulqula Gorge) It is located at latitude 36 o 21 - 23 = and longitude 45 o 10 - 04 = , at the upstream of Kulkula gogre stream at the toe of Qandil mountain, 17km to the north of Qala Diza town (Fig.1.2). In this section only one succession is exposed which is about 15m thick. 1.7. Methodology 1- Reconnaissance survey of all areas of the occurrence of the formation to find the distribution of the outcrops of the formation. For this, topographic map of 1: 50000 and Google Earth Satellite image are used. The three dimension images are compared with the topographic and geologic maps. 2- Collection of available literature that concers the formation. 3- Selection of suitable outcrop sections for sampling and description, this includes (type of lithology, vertical and lateral change), distinguishing sedimentary structures and stratigraphic relation of the formation with surrounding formations. The samples are taken in regular interval of about 1.5m, but in the monotonous intervals the sample spacing is increased 4- After removing the weathered parts, 118 fresh samples (point samples) were carefully collected from the five sections which were taken perpendicular to the strike of strat, table (1.1). The samples were broken into smaller pieces and were saved for petrographic examination under polarized and stereoscopic microscopes and small 10
Page 1 and 2: SEDIMENTLOGY AND GEOCHEMISTRY OF TH
Page 3: Supervisor Certification We certify
Page 6 and 7: Dedicated To: The Soul of my Father
Page 8 and 9: ABSTRACT The lower member of Qulqul
Page 10 and 11: LIST OF CONTENTS Chapter One: INTRO
Page 12 and 13: LIST OF FIGURES Fig. No. Title Page
Page 14 and 15: Fig. (4.1) Disribution of clay mine
Page 16 and 17: CHAPTER ONE INTRODUCTION CHAPTER ON
Page 18 and 19: CHAPTER ONE INTRODUCTION Limestone
Page 20 and 21: CHAPTER ONE INTRODUCTION Fig.1.2: T
Page 22 and 23: CHAPTER ONE INTRODUCTION Qulqula go
Page 26 and 27: CHAPTER ONE INTRODUCTION portion of
Page 28 and 29: CHAPTER ONE INTRODUCTION See Fig.1.
Page 30 and 31: CHAPTER ONE INTRODUCTION Fig.1.5: G
Page 32 and 33: CHAPTER TWO STRATIGRAPHY AND SEDIME
Page 56 and 57: CHAPTER THREE MICROFACIES ANALYSIS
Page 74 and 75:
CHAPTER THREE MICROFACIES ANALYSIS
Page 76 and 77:
Page 78 and 79:
Page 80 and 81:
CHAPTER FOUR GEOCHEMISTRY 4.2. Anal
Page 82 and 83:
CHAPTER FOUR GEOCHEMISTRY 4.3. X-Ra
Page 84 and 85:
CHAPTER FOUR GEOCHEMISTRY 4.4. Majo
Page 86 and 87:
CHAPTER FOUR GEOCHEMISTRY considera
Page 88 and 89:
CHAPTER FOUR GEOCHEMISTRY Table (4-
Page 90 and 91:
CHAPTER FOUR GEOCHEMISTRY formation
Page 92 and 93:
CHAPTER FOUR GEOCHEMISTRY Al 2 O 3
Page 94 and 95:
CHAPTER FOUR GEOCHEMISTRY Fe 2 O 3
Page 96 and 97:
CHAPTER FOUR GEOCHEMISTRY The distr
Page 98 and 99:
CHAPTER FOUR GEOCHEMISTRY reduction
Page 100 and 101:
CHAPTER FOUR GEOCHEMISTRY 4.5. Trac
Page 102 and 103:
Page 104 and 105:
CHAPTER FOUR GEOCHEMISTRY Histogram
Page 106 and 107:
CHAPTER FOUR GEOCHEMISTRY The overa
Page 108 and 109:
CHAPTER FOUR GEOCHEMISTRY The distr
Page 110 and 111:
CHAPTER FOUR GEOCHEMISTRY the frequ
Page 112 and 113:
Page 114 and 115:
CHAPTER FOUR GEOCHEMISTRY method us
Page 116 and 117:
CHAPTER FOUR GEOCHEMISTRY * * * * *
Page 118 and 119:
CHAPTER FOUR GEOCHEMISTRY According
Page 120 and 121:
CHAPTER FOUR GEOCHEMISTRY Factor (6
Page 122 and 123:
CHAPTER FOUR GEOCHEMISTRY Fig. (4.2
Page 124 and 125:
CHAPTER FOUR GEOCHEMISTRY Scale 1/1
Page 126 and 127:
CONCLUSIONS This research has concl
Page 128 and 129:
References Abdul-Hameed F. F. 1980.
Page 130 and 131:
Barnes, R. L. and Jackson, J. A., 1
Page 132 and 133:
Dunoyer De Segozac, G., 1970. The t
Page 134 and 135:
South African Journal of Geology; J
Page 136 and 137:
Nicholls, G. D. and Loring, D. H.,
Page 138 and 139:
Stanton, R. E., 1965. Rapid Methods
Page 140 and 141:
Appendixes 125
Page 142 and 143:
Table (A-2a): Major oxide, Trace El
Page 144 and 145:
Page 146 and 147:
Page 148 and 149:
Page 150 and 151:
Appendix (B): XRD patterns of some
Page 152 and 153:
Fig (B-6): XRD patterns of black li
Page 154 and 155:
Fig (B-12): XRD patterns of black l
Page 156 and 157:
Fig (B-18): XRD patterns of black l
Page 158 and 159:
@@ón‚íq @ôáŽîŠóèI@ ×a
Page 160 and 161:
@ðÝÑÜa@ö§a@À@kÔbÉn¾a@ñ§
show all

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

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?