petrology of ultramafic and related rocks along iraqi zagros thrust zone

More documents

Recommendations

Info

Fig. 2-4: Field photograph of Gimo unit of Qandiel Series occurs as a cap on the Mawat ophiolite. 25
Fig. 2-5: Geological map of the Qaladez area. 26
Page 1 and 2: PETROLOGY OF ULTRAMAFIC AND RELATED
Page 3 and 4: We certify that we read this thesis
Page 5 and 6: ABSTRACT Four main ultramafic rock
Page 7 and 8: CONTENTS Chapter 1: Background, Aim
Page 9 and 10: Chapter 7: Conclusions and Recommen
Page 11 and 12: Figure 3 - 10: Field photograph of
Page 13 and 14: albite - tremolite zone, E = albite
Page 15 and 16: Figure 6 - 19: Time-paragenesis, al
Page 17 and 18: Table 6 - 2: Representative microna
Page 19 and 20: 1 BACKGROUND 1-1 Ultramafic rocks U
Page 21 and 22: ocks of the belt. These attributes
Page 23 and 24: 1-1-3 Metamorphism of ultramafics M
Page 25 and 26: Reaction 1: Isochemical serpentiniz
Page 27 and 28: 1-2-2 Jadeitites Jadeitite is compo
Page 29 and 30: In combining the new data on the se
Page 31 and 32: 2-1 Regional geology The Iraq Zagro
Page 33 and 34: 2-1-1 Geology of Penjwin area 2-1-1
Page 35 and 36: of Luta-Rash. Volcanic rocks are ex
Page 37 and 38: and a sandstone unit of the Paleoce
Page 39: Fig. 2-1: Tectonic subdivision of I
Page 45 and 46: Chapter 3 Petrology of ultramafic r
Page 47 and 48: 3-1-2 Harzburgite Harzburgite is th
Page 49 and 50: 3-1-6 Serpentinite Two types of ser
Page 51 and 52: small amount of ilmenite. Hornblend
Page 53: In places, it is surrounded by fine
Page 62 and 63: 4 Mineralogy and mineral chemistry
Page 64 and 65: compositions with Mg-number ranging
Page 66 and 67: 4-3-4 Hydrous phases Hydrous phases
Page 68 and 69: Fig 4 -3: Compositions of chromian
Page 70 and 71: Fig 4 -6: Compositions of chromian
Page 72 and 73: Chapter 5 Discussions 55
Page 74 and 75: the tectonite region of the graph (
Page 76 and 77: involves loss and gain of CaO, SiO
Page 78 and 79: Fig. 5 - 1: Chromian spinel composi
Page 80 and 81: Fig. 5-3: Cr-number in spinel vs. F
Page 82 and 83: Chapter 6 Related rock 65
Page 84 and 85: plagioclase (Figs. 6 - 2 G,H) and z
Page 86 and 87: Plagioclase and ilmenite are the or
Page 88 and 89: 2 CaAl 2 Si 2 O 8 (anorthite) + Na
Page 90 and 91: apatite grains, characterized by bl
Page 92 and 93:
the rim. Estimated pressure - tempe
Page 94 and 95:
16 clinozoisite + H 2 O. (16) From
Page 96 and 97:
metamorphism. It was also formed du
Page 98 and 99:
Fig. 6 - 2: Photomicrographs and im
Page 100 and 101:
Fig. 6 - 4: Backscattered electron
Page 102 and 103:
Fig. 6 - 7: Line scan profile acros
Page 104 and 105:
Fig. 6 - 9: Line scan profile of pa
Page 106 and 107:
Fig. 6 - 11: (A) Backscatter electr
Page 108 and 109:
Fig. 6 - 13: Field of the approxima
Page 110 and 111:
Fig. 6 - 15: Whole rock chemical co
Page 112 and 113:
Fig. 6 - 17: Whole rock chemical co
Page 114 and 115:
Fig. 6 - 19: Time-paragenesis, albi
Page 116 and 117:
1 Conclusions 1. The Iraqi Zagros T
Page 118 and 119:
2 Recommendations for further works
Page 120 and 121:
Arai, S., 1987. An estimation of th
Page 122 and 123:
Chakhmouradian, A.R., Reguir, E.P.,
Page 124 and 125:
Evans, B.W., Frost, B.R., 1975. Chr
Page 126 and 127:
Kamenetsky, V., Crawford, A. J., an
Page 128 and 129:
Morand, V.J., 1990. High chromium a
Page 130 and 131:
Watson, E.B., Wark, D. A. and Thoma
Page 132 and 133:
Table 4 - 1: Representative microna
Page 134 and 135:
Page 136 and 137:
Page 138 and 139:
Page 140 and 141:
Page 142 and 143:
Table 4 -11: Representative microna
Page 144 and 145:
Table 4 -13: Representative microna
Page 146 and 147:
Page 148 and 149:
Page 150 and 151:
Page 152 and 153:
Page 154 and 155:
Page 156:
Research public activity Peer-revie
show all

petrology of ultramafic and related rocks along iraqi zagros thrust zone

Create successful ePaper yourself

Delete template?

Save as template?