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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Djibouti (1)
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Sudan (1)
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North Africa
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Algeria (2)
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Egypt (2)
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Illizi Basin (1)
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Libya (2)
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Asia
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Oman
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Qatar (7)
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Saudi Arabia (13)
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United Arab Emirates
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Abu Dhabi (5)
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Ajman (1)
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Dubai (1)
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Sharjah (1)
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Umm al-Qaiwain (1)
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Yemen (6)
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Euphrates River (1)
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Far East
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Burma (2)
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China
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Indian Peninsula
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India (3)
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Middle East
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Iran
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Iraq
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Syria (14)
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Tigris River (1)
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Turkey
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Taurus Mountains (3)
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Zagros (36)
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Canada
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Invertebrata
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Mollusca
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Cephalopoda
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Porifera
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Protista
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Textulariina
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Radiolaria (1)
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microfossils
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Plantae
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Sinjar Formation (2)
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Mesozoic
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Middle Cretaceous (2)
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Upper Cretaceous
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upper Campanian (5)
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Cenomanian (6)
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lower Maestrichtian (2)
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Senonian (8)
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Jurassic
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Middle Jurassic
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Upper Jurassic
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Kimmeridgian (1)
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Triassic
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Paleozoic
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Cambrian (2)
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Carboniferous
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Freeport Formation (1)
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Middle Pennsylvanian
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Ordovician (2)
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Silurian (1)
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ophiolite (6)
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framework silicates
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orthosilicates
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ring silicates
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sheet silicates
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clay minerals (1)
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mica group
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palygorskite (1)
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sulfates
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gypsum (2)
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Primary terms
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absolute age (6)
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Africa
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East Africa
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Djibouti (1)
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Sudan (1)
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North Africa
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Algeria (2)
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Egypt (2)
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Illizi Basin (1)
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Libya (2)
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Asia
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Arabian Peninsula
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Kuwait (8)
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Oman
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Qatar (7)
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United Arab Emirates
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Abu Dhabi (5)
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Ajman (1)
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Dubai (1)
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Sharjah (1)
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Umm al-Qaiwain (1)
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Yemen (6)
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Euphrates River (1)
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Far East
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Burma (2)
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China
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Indian Peninsula
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India (3)
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Pakistan (2)
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Middle East
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Dead Sea Rift (1)
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Iran
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Israel
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bacteria (1)
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Canada
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carbon
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organic carbon (2)
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catalogs (1)
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Cenozoic
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Bakhtiari Formation (2)
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Quaternary
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middle Holocene (1)
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upper Holocene (1)
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Tertiary
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Neogene
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middle Miocene (3)
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upper Miocene (1)
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Pliocene (3)
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Paleogene
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upper Eocene
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Priabonian (1)
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-
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Oligocene
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lower Oligocene
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Rupelian (1)
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-
upper Oligocene
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Chattian (1)
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-
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Paleocene
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lower Paleocene
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K-T boundary (1)
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Sinjar Formation (2)
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clay mineralogy (2)
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climate change (1)
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Alps
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Central Europe
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pegmatite (1)
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ultramafics
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dunite (1)
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harzburgite (1)
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-
-
volcanic rocks
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andesites (1)
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basalts
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mid-ocean ridge basalts (3)
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ocean-island basalts (1)
-
-
-
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Indian Ocean
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Arabian Sea
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Red Sea (1)
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intrusions (2)
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Invertebrata
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Echinodermata
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Crinozoa
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Echinozoa
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-
-
Mollusca
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Bivalvia
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Heterodonta
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Rudistae (3)
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Ostreoidea
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Ostreidae (1)
-
-
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Cephalopoda
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Ammonoidea (1)
-
-
-
Porifera
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Stromatoporoidea (1)
-
-
Protista
-
Foraminifera
-
Fusulinina
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Fusulinidae (1)
-
-
Rotaliina
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Buliminacea
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Bolivinoides (1)
-
-
-
Globigerinacea
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Globigerinidae
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Globigerina (1)
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Globigerinoides (1)
-
-
Globotruncanidae
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Globotruncana (4)
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-
Heterohelicidae (1)
-
-
Orbitoidacea
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Lepidocyclina (1)
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Orbitoididae (1)
-
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Rotaliacea
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Nummulitidae
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Nummulites (2)
-
-
-
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Textulariina
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Lituolacea
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Orbitolinidae
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Orbitolina (1)
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Radiolaria (1)
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isostasy (1)
-
isotopes
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radioactive isotopes
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stable isotopes
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O-18/O-16 (3)
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maps (4)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (5)
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Aptian
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Shuaiba Formation (1)
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Berriasian (2)
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Thamama Group (1)
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Zubair Formation (3)
-
-
Middle Cretaceous (2)
-
Shiranish Formation (10)
-
Upper Cretaceous
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Campanian
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upper Campanian (5)
-
-
Cenomanian (6)
-
K-T boundary (1)
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Maestrichtian
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lower Maestrichtian (2)
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Senonian (8)
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Turonian (2)
-
-
-
Jurassic
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Middle Jurassic
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Bathonian (1)
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Callovian (2)
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-
Upper Jurassic
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Kimmeridgian (1)
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Oxfordian (1)
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Tithonian (1)
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-
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Triassic
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Upper Triassic
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Norian (1)
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Rhaetian (1)
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-
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metal ores
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iron ores (1)
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metals
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alkali metals
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cesium (1)
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alkaline earth metals
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chromium (1)
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rare earths (1)
-
-
metamorphic rocks
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metaigneous rocks
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serpentinite (3)
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metasomatic rocks
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rodingite (1)
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serpentinite (3)
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metamorphism (1)
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metasomatism (3)
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mineral deposits, genesis (6)
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mineral exploration (1)
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minerals (1)
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North America
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Oceania
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Melanesia
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Vanuatu (1)
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oil and gas fields (28)
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oxygen
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O-18/O-16 (3)
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Pacific Ocean (1)
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paleoclimatology (1)
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paleoecology (1)
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paleogeography (8)
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paleontology (14)
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Paleozoic
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Cambrian (2)
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Carboniferous
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Pennsylvanian
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Freeport Formation (1)
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Middle Pennsylvanian
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Allegheny Group (1)
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Ordovician (2)
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Permian
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Khuff Formation (1)
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Upper Permian (1)
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Silurian (1)
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palynology (1)
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palynomorphs
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petroleum
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natural gas (14)
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phosphate deposits (2)
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Plantae
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algae
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calcareous algae (1)
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plate tectonics (24)
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Precambrian (1)
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Iraq
Critically stressed fractures: analysis of the Shaikan Field, Kurdistan Region of Iraq
Dynamic calibration of the Shaikan Jurassic full-field fractured reservoir model through single-well DST and multi-well interference discrete fracture network simulation
The Paleogene ophiolite conundrum of the Iran–Iraq border region
Multiscale fracture length analysis in carbonate reservoir units, Kurdistan, NE Iraq
Timing of the Arabia-Eurasia continental collision—Evidence from detrital zircon U-Pb geochronology of the Red Bed Series strata of the northwest Zagros hinterland, Kurdistan region of Iraq: REPLY
Timing of the Arabia-Eurasia continental collision—Evidence from detrital zircon U-Pb geochronology of the Red Bed Series strata of the northwest Zagros hinterland, Kurdistan region of Iraq: COMMENT
Stochastic inversion by trace matching for carbonate reservoir property prediction: A Mishrif Reservoir case study
Ahdeb oil field, Mesopotamian Basin, Iraq: Reservoir architecture and oil charge history
Abstract: An integrated sedimentological and petrophysical approach was implemented to define the role of facies diversity and cyclicity on the reservoir quality of the Mishrif Formation in several oil fields in southern Iraq. The reservoir quality in most regressive cycles was enhanced upwards from deep-marine facies towards the shallower shelf-margin facies. The change in reservoir quality could be detected in the facies stacked systematically within the regressive cycles, which was also easily recognized using the porosity logs. The impact of early diagenetic overprints was quite obvious in developing both reservoir and non-reservoir rock types within the Mishrif Formation in the study area. A simple rock-typing nomenclature was proposed based on the available data in order to classify the existing reservoir (R) and non-reservoir (S) rock types. The best-recognized reservoir rock types were rudistid microfacies with grain-dominated fabrics (including both grainstone (R1) and grain-dominated packstone (R2)), which were subjected to an early diagenetic dissolution process, usually located beneath discontinuity surfaces. Such reservoir units or rock types have a regional extent within the southern Mesopotamian Basin, as they have often developed during the Mishrif shelf-margin progradation. In addition, the other important reservoir rock type was a microbialite (i.e. peloidal mud-dominated packstone (R3)), which was additionally characterized by micropores within the mud-dominated portion of the facies. However, owing to the variable intensity of the diagenetic effects and differences in the depositional texture components, the reservoir quality in this rock type could vary regionally. The regional distribution of the rudistid grainstone and grain-dominated packstone reservoir rock types (R1 and R2) was mostly related to the palaeogeographical highs that existed during deposition. However, such reservoir rock types could pinch out within the depositional sequences, showing their potential to become stratigraphic traps outside the structural crest of the field. The delineation of the reservoir rock types within a sequence-stratigraphic framework can be quite beneficial for reservoir prediction and exploration within and outside of the field.