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Buhayrat Al Asad
Van Golu
Daryacheh ye Orumiyeh
Buhayrat athTharthar
Behr al Milh
Daryacheh ye Namak
SH
AL
LO
WM
AR
I NE
CL
AS
TI C
S
Gd(B95)
Gu(B95)
Gu(B95)
Gu(B95)
Gu(S78,B95)
Gu(S78)
Gu(S78)
Gu(S78)
Gu(S78)
Gd(B95)
Gu(S78,B95)
Gu(B95)
Gu(B95)
Gu(S78)
Gu(S78)
Gu(S78)
Gu(S78)Gu(S78)
Gu(S78)Gu(S78)
Gu(S78)Gu(S78)
Gu(S78)
Gu(S78)
Gu(S78)
Gu(S78)
Gu(S78)
AIN ZALAH
QASAB
JAWANNAJMAH
QAIYARAH
RUMAILA
RACHI
ABU GHARIB
BUZURGAN
DUJAILA
BUTMAH
RATAWI
WEST QURNA
BEYKAN
KURKAN
SAHABAN
KAYAKOY
SELMOCELIKILI
SILIVANKA
WEST RAMANRAMAN
GARZANMAGRIP
KURTALAN
BAI HASSAN
EAST BAGHDAD
AHDAB
SEZGIN
GERMIK
DODAN
BARBES
KATINYENIKOY
YENIKOY EASTSARICAK
YATIR
KAYAKOY WEST
MALTEPE
MALTEPEWEST
KURKANSOUTH
ADIYAMAN
ADIYAMANSOUTH
KAHTA
PIYANKO
SOUEDIE
KARATCHOK
RISHA
HAMZA
AGHA JARI
AHWAZ
BIBI HAKIMEH
BINAK
BUSHGAN
DANAN
GACHSARAN
KABUD
KARANJ
KARUN
DARIUS-KHARG
KUH-E RIG
KUPAL
LAB-E SAFID
LALI
MALEH KUH
MANSURI
MARUN
MASJID-I SULAIMAN
PAR-E SIAH
PARIS
PAZANAN
QALEH NAR
RAG-E SAFID
SARKUN
SARVESTAN
AGHAR
DALAN
MAND
KUH-E KHAKI
KANGAN
NARVARAVI
PARS
NARGESI
RUDAK-MILATUN
SULABEDAR
CHILINGAR
GARANGAN
KILURKARIM
GULKHARI
SIAH MAKAN
DOUDROU
SHURAMSUSANGERD
AB TEYMOUR
SHADEGUN
RAMIN
HAFT KEL
NAFT SAFID
ZELOI
RAMSHIR
PAYDAR
CHESHMEH
KHUSH
DEH LURAN
SAMAND
VEYZENHAR
HALUSH
TANG-E BIJAR
KHALAFABADNAHR UMR
ZUBAIR
BURGAN
ABU HADRIYA
FATHILI
BAHRGANSAR
CYRUS
KAFJI
SAFANIYA
FEREIDOON
MARJAN
WAFRA
MINAGISH
BAHRAH
RAUDHATAIN SABRIYA
MANIFA
KHURSANIYA
BERRI
ABU SAFAH
MAGWA
AHMADI
UMM GUDAIR
FUWARIS
AL HOUT
ESFANDIAR
RIMTHAN
DIBDIBA
JURAYBIAT
RATQA
ABDALI
MEDINA
DORRA
DHARIF
ABDULIYAH
LUHAIS
ALIANE
OUDEH
LAILAK
HAMZA
DERRIK
DERRIK N.
EKHAIDER
NAFATAH
AKKAS
KHLEISIA
MILEHTHARTHAR
MAKHUL
ABU FUDHUL
BAIJA
HIBBARAH
BALAD
DIWAN
UBAID
KHIDR AL MAA
DIBDIBBA
JEBELSANAM
UMMQASR
SINDABAD
SADID
QUWAIR
QALIANADAIYAH
GUSAIR
GULLAR
MUSHORAH
JEBEL KAND
ALAN
ATSHANDEMIR DAGHAIN GHAZALTEL HAJAR
SASAN
IBRAHIM
KIRKUKKHURMALA
QARA CHAUQ
KHANUQAH
TAQ TAQ
CHEMCHEMAL
KOR MOR
PULKHANA
CHIA SURKH
QUMARGILABAT
INJANA
KHASHEMAL-AHMAR
MANSURIYA
JARIA PIKA
TELGHAZAL
NAFT KHANANAU DOMAN
ALLASHAMRIN
TIKRIT
BADRAH
MERJAN
RAFIDAIN
GARAF
NASIRIYA
RIFAEI
RAFIDAIN E.
NOOR
HALFAYAH
HUWAIZA
MAJNOON
SUBBA
TUBA
JRAISHAN
ABU KHAIMA
NAHRAWAN
AHDAB N. DHAFRIYAH
KUMAIT
AMARA
SUFAIYAH
AJEEL
KHABBAZ
KIRKUK BABA
KIRKUKAVANAH
RUMAILANORTH
K EAST
AL FAID N
ABU RABAH
CHERRIFE JIHAR
Al RASEM
ASH SHAER
PALMYRA
AL BARDE
AL HASAKAH
SALIEH
GBEIBE
GHOUNA
TISHRIN
JEBISSA
MARGADA
HAMRIN
RIQUA
MUTRIBA
TAWKE
SHAIKAN
HAWLER
JAMBUR
T h e G u lf
C a s p i a n
S e a
Qadmous
MarmaritaNasirah
Machta Helou Jweikhate
Treize
A. ShamsWadi Al-Ouyoun
DatayehKseibyeh
Joubeh
Slenfeh
Ouyoun
J. ZinnarBloudan
J. Naqnaquyeh (NE)
J. Rmah
J. Abou RahbaJ. Abtar (NE)
J. Assater
J. Mazar (NE)
J. Satih (NE)J. T. Satrah
J. Hayan
Sakakah
Hamamiyat
Al-Laqit b/h
Al-Jawf
Jabal al-Qiyl al-Kabir
At-Tawil
loc.
Mudrraj
Al-Aqabah
Hail
Baqah Ash Shuaibah
Al-Mayyah
Al-Ajfar
Jal As-SaqiyahQiba
Hunayzil
Lussuf
Qasr Hamman
Abu Radham
Chabd
Faid Az-Zahra
GalaibBarbak ad Diud
Salman
Aa
Aidah
Wagsa
Shabicha
S.85
Bussaya
Abu Ghar
Naft Kameh
Dalpari
Dash-i-Gul
Maidan-i-Naftun
Bardi-i-Qamcheh
Bikarz
Tut
Korudag
Hazro N
Hazro S
Yayladag
K. Maras
Glbasi
Terbzek
E. Kahta
Alidami
J. Smekai
J. Dneir
J. Abou Zounnar
J. Bardeh
J. Naqnaqiyeh (SW)J. Abtar (SW)
Abtar Est
J. Satih (SW)Soukhne
J. Al Qom
J. ThanyetAs Safra
J. Mazar (SW)
J. Shomariyeh
J. Bilaas
J. Abou DouhourJ Shaer
J Abou Roujmein
Abu Ghar
Jelta Solution Hole
Jebel Ithayna
Benavi
Injana N
Injana S
Buzurgan-1
Fuqo-1Kifl-2
Buzurgan-2
Buzurgan-3Buzurgan-4
Kumait-1
Rafedain East-1
Abu Jir-1
Hit-1
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.loc.
loc.loc.
loc.
loc.
Kharg Island
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.Binak
Hendijan
loc.
loc.
loc.
loc.
loc.
loc.
loc. loc.
loc.
Borudjerd/JTP-27
Kuh-e Safid/KRD-23
loc.
loc.
SW of crush zone area
loc.Kuh-e Pasan Kuh-e Saltan
Kuh-e Sarkanloc.
loc.loc.
Kuh-e Anaran
Kuh-e Kalak
loc.Kabir Kuh(SW flank)
Tang-e Garalfdloc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.
Isgahe Taleh Zang area Pal-e Zarreh area
General arealoc.loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
Kuh-e Badmestan
Bazan Pir & Maadn
Area
NE of roadComposite column, E area
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.loc.
loc.
loc.loc.
Lali-2
loc. loc.
loc.
loc. loc.loc.
loc.
loc.loc. loc.
loc.
loc. loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.loc.
Rag-e Safid
loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
Khaviz
loc.loc.Kuh-e Baz
loc.
loc.
loc.
Paris
loc.
loc.
loc.
loc.
loc.
NW of Deh Bid
loc.
loc.
loc.loc.
loc.
loc.
loc.
loc.loc.
loc.loc.
loc.loc.
loc.loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.loc.
loc.loc.
Kah-e Mish
loc.
loc.
loc.
loc.
loc.
Kuh-e Khami
loc.
loc.
loc.
loc.
loc.
Kuh-e Kalat
loc.
loc.
loc.
S. Shiraz
Zarqan
loc.
loc.
loc.
loc.
Kuh-e Mozzaferi
loc.
loc.
loc.
loc.loc.
loc.loc.Kuh-e Sah
loc.loc.
loc.
loc.
loc.
loc.loc.
loc.
loc.
loc.loc.
loc.
loc. loc.
loc.loc.loc.
loc.
loc.
loc.
loc.
loc.loc.
loc.
loc. loc.
loc.loc. loc.loc.
loc.
Kulah Qasi
loc.
loc.loc.
loc.
loc.
loc.
loc.
loc.
loc.
Kuh-e Dehnow/Kuh-e Gavbust
loc.
loc.
Kuh-e Gel-e Siah
Bushehr
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
loc.
Doondag
Kmbosdag
? Jebel BanuJebel Shaloradar
Jebel Bezniyan N
jebel Bezniyan SChia Surkh
Jebel Bawgaru
Karia Pika
Maqlub
Ain Safra
Bashiqua
Al Suwar-1
Berri-84Khursanyiyah-81
Abu Safah-29
Hazro-1 & 2
Harbol
B-113
loc.
B-4/7
AG-5
R-1
loc.
loc.
BabagirFardows
Gawar
MC1
MC3
MC2
MC4
Amanos
loc.loc.
loc.
J-203
MC1
Loc
West Qurna-1
Nahr Umr-7
Nahr Umr-8
Z-13
Handof-1
Turabah-1
Qumar-1
K-317
NK-35Mansuriya-1
M-2
M-3M-4
Q-55
Qasab-12
Quwair-2
Makhmur-1
BH-81K-1
Kirkuk-175
J. Aziz
BH 100/B/85
KH-5/2
T19
UB8A
JTP-21
JTP-20
JTP-7
JTP-16
RAP-3
JTP-4
JTP-6
JTP-2JTP-5
JTP-1
RAP-1
JTP-3
JTP-22
JTP-23
RFH-1
JTP-8
RFH-4
JTP-24
RFH-3 RFH-2
KRD-24KRD-27
KRD-25
KRD-26
JTP-13 JTP-25JTP-26
RAP-8
MGH-5MGH-4
MGH-1
MGH-3
RAP-5
RAP-7
RFH-6MGH-2
RAP-4
JTP-11
JTP-12
JTP-9
JTP-10
JTP-14
JTP-18
JTP-15RAP-2
RAP-6
indet.
Ghilizardia
Butmah-1
Adaiyah-1Qalian-1
Qaiyarah-1Q-2
Qasab-2
Sadid-1
Khanuqah-1
Mileh Tharthar-1
Abtakh-1
Quwair-1
Qarah Chauq-1
Rafan-1
Sufaiyah-1
Kifl-3
Diwan-1
Rafidain-1
Garaf-1
Mishraq-1
Gilabat-1Injana-5
Banik
Amadia
Ru Kuchuk
Rania
QalGah
Dalamar
Naft Kaneh-3
Kor Mor-2
Sirwan-Balambo
Taq Taq-1
Shailkan
Kirkuk-117
Kurrek
Zaita
Zibar
Argosh
Mazna
Mirgasor
Balki
Zar Gelli
Diyana
Zhazhoke
Diza
Gund-i-Shikart
Sareshmar
Naouren
Koi Sanjak
Azkand
RazanRowanduz
Derbannd-i-Sajirrma
Ali Rash
Wadi MSad
Subba-2
Luhais-2
Gullar-1
Safawi-1 Ubaid-1
Shawiya-1
Dirah-1 Liyah-1K-1
R-28
Bubaiyan-1
Bubaiyan-2
Mushtaq-1
Paydar-1
Saderabad-1,2
Abu Gharib-2Abu Gharib-12
Abu Gharib-3Abu Gharib-101
SN-1
FQ-4
FQ-7
Noor-1
Halfayah-1
H-4
Dujaila-1
Amara-1
Badrah-1
Changulah-1
Daloori-1Daloori-2
Danan-1
Kabud-1
Qalah Nar-1
Maleh Kuh-1
Sarkan-1
D. Sonoh-1
Khaneh Sorkh-1
Nan-1Darbodom-1Sankul-1
N. Shahabad-1
?M. Dashti
Emam Hasan-2Patoi-1
Vijonan
Veyzenhar-1
Anjir-1
Tang-eBijar-1
TG-1
Naft Kaneh-32 N.E. Shah
JK-1
ND-2
KA-1
Injana-4
P-5
Gilabat-3
Pulkhana-3
Pulkhana-6
Hamrin-2
Hamrin-3Hamrin-4
Jebel Hamrin-1
JD-1
Samarra-1
Hamrin-5
Hamrin-6
Qarah Chauq-2
Khanuqah-2
Demir Dagh-1
Taq Taq-2
K-3
Sasan-1
Atshan-1
Alan-2
Tel Hajar-1
Anah-2
Fallujah-1
Musaiyib-1
Afaq-1Kifl-1
Samawa-1
Ghalaisan-1
Nasiriyah-1
Ahdab-1
Deh Luran
Hu-1
Garaf-2
Dhafriyah-1
Tikrit-1
K 4/10
K 4/7
K 4/3 K 4/5
KH 8a-9
KH 6a-8
KH-6
J-1
Subba-5
Subba-4
Subba-3
Subba-1
Jerishan-1
Tuba-1T-2 T-3
R-2
Jebel Sanam-1
Siba-2
M-2
Majnoon-1
Majnoon-3 Majnoon-4
Luhais-1
Siba-1
Sindabad-1
Dibdibbah-1
Umm Qasr-1
Ri-10
Afendi-1
Maghlouja-1
Tel Aswad-1
SheikhSuleiman-1
Zakho
Sinjar
Hatra
Shaqlawa
Makhmour
Panjwin
Mawal
Khanaqin
Haditha
B7-7
Qaim
Akashat
Merjan-1
Nukhaib
B-18/7
B-2/7
Umm Al Hashim
Halfayah-2
Dujaila-2
Khider Alma-1
Ratawi-3
R. S.-72
Zubair-42
Rumaila N.-172
West Qurna-15
Rumaila N.-167Ratawi-6
Luhais-12
Ratchi
Khursaniyah-8
Berri-84
Samur Dag
Abu Khima-1
Ganmi
Bottea
Tuqaiyid w.w.
Barbak
Faida Az-Zahra
S-462
Badanah (Arar)-1
As-Sulaimaniyah (NW-44)
Kahf-1
MurayrHudayb
Suwayr
Kahf-1
Hamadani-1Kharbaka-1
Beida-1
Markada-1
Tayma-1S
Qalibah-1
Turaif-1
Traibel
Endezah
Pir-i-Mugurun
Sarchinar
EB-5
EB-80
EB-69
EB-11
EB-3
EB-1
EB-2
EB-4
EB-12
EB-6
EB-7
EB-53
EB-77
EB-10
Varavi-1
Nar-1
Kangan-1
F-2
P-5
P-3
P-4P-1P-2
Fb-1
Mand-4
Kuh-e Siah-1
Dalan-1
Aghar-1
Naura-1
Bandubast-1
Zard Kuh
Kuh-e GerehDopolan Mine
Kuh-e Manghast
Kuh-e Dinar
Roshan Kuh
Nazmabad
Estaki Mine(Abadeh)
Kuh-e Hambast
Oshtoran-Kuh
Huleyan-1
Kuh-e Bangestan-1
Lavan-1
Sabzpushan-1
Sefidar-1
Dashtak-1
Ahmadi-1 Kaneh Kat
Kabir Kuh-1
Chal-e Sheh
Kuh-e Gurpi-1
Iminoco-1
ST-8
Well-1
Well-3
Well-6
Well-5
Well-9
Well-8
Well-7
Well-10
Well-11
Hassan-1
Swab-1
El Madabe NW-101
El Hamra-101
Rasin-101
Sijan-101Omar-101
Tabieh-101
Cheikh Judid-1
Hairan-1
Raqqa-1Syrom-2
Syrom-3Syrom-103Kenan-1
Maskane-1
Shahr-i-Zur
KH-17/7
Ceylanpinar
Siverek-1Bucak-1
O. Sungurlu-1/A
Besikli-6
Kahta-2Sahabe-1
Avsar-1
K. Akceli-1
Coskunsel-2
Besni-1Karakopru-1
Durukaynak-2
Alidag-2
Cemberlitas-14Karakus-10Adiyaman-8
Bakuk-1
Gercus-1
Sfiyeh1 Derro-2
Jafar-1
Makman
Kanun
Tel El Arous
Al Hasu
J Ash Shaer-1
Kastel-1
Katin-1
Kentalan-7
Kentalan-2
Kavikadag-1Sinan-1
Silvan-1
Ahdab-2
Hajrawa
Budak
Kiran
Divana
Gel-i-SenetZap
Shish
Cudi Dagh
Hezan
Gusair-1
Gulneri
Baski ZanurDagh
Aj Dagh Derbannd-i-Khan
DizaZahis
Qal KandKoni Kawa
Dokan New BridgeMouth of Gorge
Kabbaz-4
Kirkuk-49
KM-3
KH-5/7
KH-5/5
KH-5/3
KH-5/8
BH-2
BH-5
BH-6
BH-3
KH-4/1
KH-5/4
BH-80/1
BH-48A
BH-80/1
BH-7A
KH-5/9
B-15/7
B-7/12
B-13/7
B-7/13
B 7-8
B 7-9 B 7-10
B 7-11
B -19/7
B 7-2
B 7-1
B 7-4
B7-6
B7-3
Massoudeh-1
Misrame-1Tibni-1Wadi Aabeid-1
Zemieh-2
Bishri-101
Al Hir-1
Didi-1X
Al Waha-1
Ghreta North-101
Dafayen-3
Shaafa-101
El Khuwar-101
Tabiyeh-104
Jafra-107
Qahar-103
Indet
IndetIndet
Indet
IndetIndet
Indet
Indet
Indet IndetIndet
IndetIndet Indet
IndetIndet
Indet
Indet
Indet
Indet
Indet
Az-144
Az-24
Az-274
Emam Hasan-1
Khanasser-1
Sarqala-1Shakal-1
Miran E-1
Miran W-2Miran W-1
Shaikan-1
Hawler-1
Hawler-2
Shorish-1
Bazian-1
Simrit-1
Al Jandali
Wadi Tubel
J-13
J-19 J-15
J-26J-21
J-22
J-18
J-16J-20
J-42
Jalamia
Jebel Khand-1
Atshan-1
Wadi Saggar
Ur-1
NE Koi Sanjak
Kifri
Kurdamir-1
Fahliyan
Tarbur
Tang-eGurguda
Tang-eSarvak
Tang-e Garab
Kometan
Tang-e Pabdeh
Kuh-e Amiran
Dariyan/Kuh-e Gadvan
Kabir KuhNE Flank
Ibrahim-1
Kirkuk-109
Avanah/Kirkuk-116
Kirkuk-114
Kirkuk-85
Sheikh Alas
Wadi Fuhaimi
Bara
Umm a DhibanJaddala Town
Govanda Plateau
Kashti
Mamissa
Kolosh
Jaddala Loc
Z-3
Z-31
Balikian
Northern Highlands 1
Northern Highlands 2
Risha 2
Smeica 1
Qitar el Abd 1
Strat well on Taplin
Risha 1
Risha 11
Risha 14
Risha 15
Risha 17
Risha 23
Risha 19
Siwaqa 1
Wadi Sirhan 1
Wadi Sirhan 2
Qurayyat (Saudi)
Dahikiyeh 1
Adla 1
Azraq 1 (PP1)
Wadi Ghadaf 2
Wadi Rijal 4
Wadi Ghadaf 1
Risha 8Risha 13
Risha 12Risha 10
Fuluk 1
Heavy Oil 2(W Rajil)
Wadi Sirhan 11
Wadi Sirhan 3
Wadi Sirhan 7
Wadi Sirhan 9
Wadi Sirhan 14
Wadi Sirhan 10
Wadi Sirhan 4
Wadi Sirhan 12
Wadi Sirhan 13 Wadi Sirhan 5
Wadi Sirhan 8
Wadi Sirhan 6
Heavy Oil 1(W Rajil)Wadi Rajil 3
9
Hamzeh 411
215
Wadi Hazim 1
3 & 85Hamza 1, 10 & 12
Hamzeh 13
6
Wadi Rijal 1 & 2
7
14, 15 & 16
Well Alqin
Well HarranEl-Awanid
Well Al-Qussair
Well A15
Well A16
Mkemen SlebiWell K6
Tell Sad RushehWell K3
J SisWell 44
Al ButmiyalWell 2
Wadi Saba AbuiWell 49
Saba AbarWell 9-1
Wadi DwekhletMirrahWell 9-2
Al JuwefWell 9-3
Al Juwef(W)
Well 27
Well 24 Well K-15
Well 29
Well 26
Well 28
Well 6P-4
Well 6P-5
Well 23
Well 21
Well 19
Palmyra
Well 6P-3
Cherrife
Well 151
WNW Rasafeh
Well 201Well 7
Jub El Abyad
Well 203
Well 153Well K-5
Dolaa
Well K-16Well 34
Well 33
El Mamlaha SW
J. Sawwanet
Rejm TarHajjaneh
Well K-25
Risha 9
Risha 16
Risha 7
Risha 18
Risha 6
Risha 5
Risha 4
Risha 3
El Qaa-1
Jebel al MarahJebel Abaid
Jebel al Aasafir
Tourkmaniye Fort
Doubayat-1
Soukhne
Biar er Rhon/Jebel Bishri
Dbba
Meidannki
Bassouta
Kourt Farmuz
Aafrine
Naz Oucharheu
Baflioun DomeBaflioun-1
Tyron
Kuh-e Gadvan
Kuh-e Jahrum
Ahwaz-6
Godar Landar
Ghadir an Nijili
Rutbah
Hill 270
Al Alaif
Mulussa (W)
Mulussa (E)
Khasm Mulussa
Jebel Tayarat
Wadi Hauran at Rutbah
Wadi Hauran SW
An Nisir
Ras Semhat
Wadi Hauran/Zor Hauran
Wadi Semhat Wadi Hauran NE
An Na'aga
Qasr Amij road
Wadi Hauran tributary
Wadi Ubaid
Wadi es Souab
6 miles NE of Arkwaz
Sirwan
JebelBalambo
BaranandDagh
Sazan Police Post
Hawar-Dalamar pathPila Spi
Barsarin Naokelekan
Aqra (top)
Bekhme (top)
Dokan Qamchuqa top
Surdash (SE)
Sargelu (NW)
Sargelu (SE)
Makhul-2
Kirkuk-14BH-3
Chemchemal-2
Gara Village
Dohuk (top)\Dohuk (SW)
B-2
Dohuk (NE)
Q-13
N-2
B-7
A-16A-19
Qaratchok-2QaratchokDagh N. f
Qaratchok Dagh
Gel-I-Garagu/Garagu
Baluti Village (SE)Baluti (NW)
Chia Gara
DarariGeli Khana
N Flank Ora Fold (top)Geli KhanaChia Zinnar
Kurra Chine (top)
Chalki Nasara (top)Kaista Village
Ora Police Post
Mirga Mir
Hadiena/Hadiena Village
Shiranish Ora Cirque
Aleppo
Homs
Al Kut
Ad Diwaniyah
Alan-1
Jawan-2
Hibbarah-1
Najmah-29
Mushorah-1
Makhul-1
Anah-1
Golden Staircase
Awasil-5
Tang-e Gel-e Tursh
Tang-e Tukab
Tang-e Daneh Qumbari
Kuh-e Surmeh
Agha Jari (field centre)
Kuh-e Anaran
Tang-e Do
Nafatah-1
BH-13
Choarta
Bir Mulussa
Wads AgarMuyat/An Nisr
Nahr Umr-1,2,3
Birjisiya
Z-24
Ratawi-1
Abba-1
Beer Qdem
W. Hararit678m
Sawwanet
Jebissa-1QalaatJabar
KharabEchl
Sirrine
B-15
Sheikh Sollakh-1
Ghouna-1
KH-7/7
KH-9/7
KH-12/7
KH-3/7
J-4
Tel Aafair
KH-5/1
A-29
KH-1/7
West Kifl-1
Km160
Khleisia-1
Akkas-1
Mityah-1
KH-5/6
Aleppo-1
Rim-1
Jibisi-208Salhia-1
Tishrin-5
Syrom-1
J-2J-3
Syrom-4
El Bouab-1El Bouab-2
El Barde-1
Qamichlie-1
Gbeibi-101
Hol-1Abu Hadjar-1
Nora-1
Tchembe-1
Bahri-1
Toueman-1
Tel Zrab-1
Markada-101Maza-1
Rasafa-1Amara-1
Jib Ganem-1
Zidan-1Habari-1
Azar-1
Didi-1
Khurbet-1
Naur-1
Hadidi-1
Badran-1
Oudeh-107Shamu-1
AodaR-6
jalan-101
R-7
Kariaten-1
Tanf-1
Derro-1Enayat
El Barde-101
Barde-2H
Malout
Naur-101
Naur-102
K East-2K East-1
K East-3K-5
Tel Brak
Cilesiz-1C-102
G.Dincer-1 Yolacan-3B.Yolacan-1
Camurlu-101
S A U D I A R A B I A
I R A Q
I R AN
K U W A I T
T U R K E Y
S Y R I A
L E B A N O N
Damascus
Baghdad
Tehran
Borudjerd
Khurramabad
Bakhtaran
Esfahan
Ahvaz
Basra
Abadan
Kuwait City
Najaf
Mosul
Tabriz
Rasht
Babol
Qom
Hamadan
Karbala
Dezful
Shiraz
Kirkuk As Sulaymaniyah
Arbil
Samarra
Ar Ramadi
Nasiriyah
Hasakah
Mardin
DiyarbakirSiirt
Nukhaib
Qasr Amij
Qasr MuhaiwirBaquba
Hamah
Rutba
Akashat
Bir El Rah
38E 40E 42E 44E 46E 48E 50E
36N
34N
32N
30N
28N
38E 40E 42E 44E 46E 48E 50E
36N
38N
34N
32N
30N
28N
52E
52E
38N
500m
400m
200m
35m
30m
25m
20m 15
m
15m
Marbat Beds 15 to 50m thick; cyclic alternationsof fining-upward fluvial clastic sediments passinglaterally into deltaic sediments, mostly sandy
dolomicrites (bk92).Marbat Beds: inshore (coastal onlap) facies;
Naaja Beds overlain by Safra Beds are offshore(CC notes).
Anah Graben was deep and narrow in the Late Cretaceous; it had a low intensity of watercirculation (bk92). N-S and E-W faults controlled the Tinif Trough and the Damluk Trough,proven by boreholes to the west and east of the Akashat Platform and on west side of theRutba-Hail Arch (trending NNE-SSW)(Karim, unpubl. in bk92). Troughs were sites of deepoceanic sources of P-rich, cool upwelling currents throughout the phosphogenic eposides;were in free connection with Tethys (bk92). Akashat (NE) and Ethna (SW) platforms representelevated, submerged blocks that formed ideal traps for dissolved phosphorous transportedby upwelling currents from the troughs into the shallower and warmer shelf environments(near-shore to basin slope) to the S and E (bk92). Platforms also have non-phosphoriticshelfal facies. Arch crest may have occasionally been emergent, with the development of
clastics and intertidal facies (bk92). East of the crest, reef and back-reef facies are representedby the Hartha and Tayarat formations (bk92).
Transgressions contemporaneous withopening of deep troughs, grabens and
development of intrashelf basins, securingopen marine communication with the Tethyan
deep waters since the Upper Campanian,when at its concluding stages, the first
phosphogenesis appeared (bk92).
Note: Shiranish reportedalso as absent in the Abu
Jir-Awasil-Hit-MilehThartar area (du59)
d63 notes absenceof lformer atestMaastrichian in
Jebissa, GhounaSUBMARINE
HIATUSAbsent
TAYARAT
Shelf&slope
SHIRANISH
Pre c is e
orientatio n/p o s itio n
TAYARAT FM.Shelf carbonate
SHIRANISH FM.Basinal cherty
limestones, marly.Deepwater >200m
SHIRANISH FM.
Thick globigerinal opensea marls and marly
limestones (nq60)
543-580m: Wackestone with foraminifera (fragmented in part), bryozoans, echinoids, andsome very fine microfossil debris. Rich foraminiferal fauna.(ra79). Top-Cretaceous @543m:;various lithologies including wackestone, packstone, grainstone, either partly recrystallisedor partly or completely dolomitised, with no primary characteristics; some chalky and marlylimestone, gypsum in porous fossil cavities in the upper part, slightly sandy in the lowermost
part (ra79). Most palaeontology has been partially lost due to recrystallisation and/ordolomitisation (ra79)
Fauna includes Omphalocyclus macroporous (Lamarck), Simplorbites gensacicus (Leymerie),Clypeorbis mamillata (Schlumberger), Lepidorbitoides socialis (Leymerie), Lepidorbitoides
cf. minor (Schlumberger), Lepidorbitoides sp. (? cf. bisambergensis), Lepidorbitoides? -Clyporbis?, Pseudoorbitoides??, Orbitoides media (dArchiac), Orbitoides gr. tissoti,
Planorbulina cretace (Marsson), Schlumbergerina, Sulcoperculina ex. gr. dicksersoni(Palmer), Sulcoperculina sp., Gaudillaupidina sp., Rotalia sp., and other different very smallrotalids. Beside these transported benthonic foraminifera, there are sparse pelagic fossls,occasional globigerinoid forams, heterohelicids, sphaera etc., within the 544th metre, onlyone globotruncana is found: Globotruncana cf. bahijae Naggar. Finally, among the transported
fossils, some algae should be mentioned Permocalculus sp., Trinocladus sp. andSalpingoporella ubaiydhy n. sp. (type level at 578.8m). (ra79)
Lower/Middle Maastrichtian based on Globotruncana from 544m down, specificallyGlobotruncana bahijae Naggar, which does not exceed (is not younger than) Middle
Maastrichtian (ra79)
OligoceneAlbian
Beds with orbitoids; recrystallised, dolomitised, porous, 163.5 to 237m. Fossils generallyobscured by diagenesis, particularly in upper levels where abundant orbitoids are extremelypoorly preserved or washed out (ra81). Samples from 163.5 and 203.5m contain Pseudorbitoidesspp. (partly in fragments; 163.5m) Lepidorbitoides minor Schlumberger, Lepidorbitoides sp.,Orbitoides tissoti (Schlumberger), Orbitoides media (dArchiac) (very rare), Planorbuilina
cretace (Marsson), Sulcoperculina gr. dickersoni (Palmer)(163.5m), Different small rotalids,minute anomalinids, a few pelagic (globigerinal) foraminifera etc. (ra81).
Tayarat/Hartha Formations (undifferentiated; poor fossilpreservation does not allow the Maastrichtian, Campanianand possibly the Upper Santonian to be distinguished): 108to 229m depth, orbitoid beds that are highly recrystallised,dolomitised and in places possibly also silicified with fewprimary characteristics evident. Orbitoid external moulds
give this interval a distinctive appearance.
Very recrystallisedwith indeterminate
rudists @247m (ra86) Indeterminate rudistsin limestone from 205-206m (ra86)
Dark grey silty marly limestones and calcareous shale(ra86); fauna of very rare planktonic foraminifera
(Gansserina gansseri Bolli); with some bulloid forms(ra86); implies earliest Maastrichtian age (cc)
Dolomitised and recrystallisedlimestones with orbitoid-
Omphalocyclus assemblage (ra86)
Limestone apparentlylacking orbitoids (ra78)
Rumelan-1,4,5,6Souedie-1,2,3,6,7,11,16,30
Sh (ni72)Argill LST
Naaja Beds post-second (more important/extensive) transgression (K180), to the west of the Rutba-Hail Arch. Semi-restricted inner shelf environment, passing occasionally into shoreline (bk92). Deeper facies deposited in troughs. MostGaara was emergent with fluvial (Marbat Bed) deposition, notably on the northern rim (bk92). There were between 3 and7 transgressive events, ranging from near-shore to central shelf biogenic barriers, organised in a semi-circle extending
from N and W flanks of the Gaara Uplift to the S along the western side of the Rutba-Hail Arch (bk92). In the S. part,Naaja Beds include reef and backreef facies similar to the underlying Hartha Formation, suggesting frequent southerlychange from inner shelf to reefal build-ups. In deep subsurface sections west of the investigated area (?KH-5/6 and 5/8?CC Notes) inner shelf-reef facies pass into deep open marine facies towards the N and W, where outer shelf environment
prevailed in the both troughs (bk92).
Naaja Beds 2-18m thick; mostly dolomite with basal sandstones, chert nodules,thin phosphorite horizons, charophytic dolomites; top is siclicified shelly
(pelecypod) limestone (bk92). Cycles often have hiatal surfaces (hardgrounds,toughgrounds). Mineralogy: montmorillonite-palygorskite-sepiolite, chert,
porcelanite, phosphorite (bk92).
In the Lower Campanian (first cycle), Marbat Beds weredeposited in a continental (fluvial) environment over and tothe north of Gaara. To the south, reefal to back-reefal and
occasionally supratidal Hartha Formation was deposited aboveCenomanian age rocks, to the S. of Rutba and on the W. sideof the Gaara uplift (bk92). Marbat Beds interpreted as equivalentto the top-Hartha Formation, as seen near the Semhat outcrops
(bk92).
Jeed Fm. is the basal phosphoritic unit of an interval on thesouthern shelf of Tethys that spans 20Ma and containing about15 phosphorite beds; deposition coincided with block-faulting,
opening and/or rejuvenation of grabens (bk92). Eustatictransgressions and regressions, accompanied by upwelling
episodes; phosphorites deposited during transgressions abovebioturbated hardgrounds (bk92).
Thickness: At the type section, at least 30mThe formation has a total thickness of some 48m in theTayarat-Thoba area.At the type section, rubbly porous;
white, buff and pink; rather chalky, fossiliferous,recrystallised, dolomitised, locally sandy limestone,
conspicuously more massive at the base.
Dunnington et al. (1959) state: Passing northwards from Jebel Tayarat through Jebel Thoba,and towards the western rim of the Gaara depression, the Tayarat limestone is cut out
progressively, by the erosion of its upper parts, and also perhaps by onlap convergence.In the section of Hill 270 (Lat 331800N, long 401030E) and Khasm Mulussa (lat 331830N,long. 4007E) the formation is absent, the Paleocene Umm Er Radhuma formation restingdiscordantly on eroded Msad Formation. The convergence increases northwards, so that,at Ras Semhat, the Umm er Radhuma rests directly on the Triassic Gaara Sandstone. Thedetails of the erosional convergence from Tayarat to An Nadhara have not been studied.
Minor quantities of phosphatic material may befound in the fossiliferous and chert beds in the
area south and west of Rutbah (n67).
Tayarat Fm. overliesthe Shiranish Fm. in C
& S Iraq (sa00)
Type LocalityDigma Marl Fm.
Type SectionAqra Limestone Fm.
also at Dar-e-Tesu interbedded with Tanjeroclastic Fm.
Also at Gerwa Zhori, Qamish, Jebel Gara,Zinta Gorge, (vb59)
PHO
SPH
ATE
S: U
PWEL
LIN
G P
O4
SED
IMEN
TS O
N W
EST
OF
HIG
H
SHIRANISHIN TINIFTROUGH
DAMLUKTROUGH.
DIGMAPO4 MARL
DIGMA FM.
LI M
I TO F
O P
HI O
L I TE
S
JEED FM.LT MAASTRICHTIAN
LOWERGERMAV
Anah Graben
OPEN SHELFwith orbitoids
LAGOONAL
SHOALS
Anah Graben
OLDER GEOLOGYOUTCROP
Note that much stratigraphy formerly referred to as EarlyMaastrichtian now falls into the Campanian following ICS 2004
AQRA
HARTHA FM.
TA
NJ E
RO
FL
YS
CH
TAYARAT SHELF MARGIN
SHIRANISH FM.
TAYARATFM.
Dolomitic shelf top, cyclic,with local sabkhas
Base map last amended 1/1/11 Data last amended 14/3/11
Tayarat Formation
Macfadyen (1938) pointed out the presence of a fish bed, in presumably Cretaceous sandy limestones, atGur Ayarat, where abundant teeth but fewer bone fragments and vertebrae were found (n67).
Diagnostic fossils and age Fossils in the Tayarat Fm include: Loftusia morgani Douville and Ompahlocyclusmacropora (Lamarck). According to H. A. Field and K.D.Jones (unpubl. data, 1958) the Tayarat Limestone containscorals, rudists (including Eoradolites?), gastropods, lamellibranchs, and algae. They maintained that genericidentification is often difficult as most of the original structures have been destroyed by recrystallisation andsome by dolomitisation. In addition to the fossils recognised in the type section, the following microfossilshave been determined from the subsurface sections: Lepidorbitoides socialis (Leymerie),Orbitoides media (dArchiac), O. apiculata, Ogivalia parisiensis dOrbigny, Rotalia skourensis Pfender,R. trochidiformis Lamarck, Globotruncana spp., Dictyoconus sp., Dicyclina schlumbergeri Munier-Chalmas,and Pseudochrysalidina sp. (n67).
Palaeontology: Lofutsia morgani Douvill and Omphalocyclus macropora (Lamarck).
The formation as a whole is of shallow water deposition and is often highly porous. Species of Loftusia andLepidorbitoides are common in the limestones, and Omphalocyclus in the shales (on58).
A similar fauna is present in the Tarbur Formation of Iran and the upper part of the Aruma Formation of SaudiArabia (jw65).
Shiranish Formation
Passes laterally westward into the neritic Tayarat Formation (n67).
Diagnostic fossils and age Fossils include: Cytherella spp., Bairdia spp., Nodosaria sp.,Globotruncana spp., Cristellaria spp., Gyroidina naranjoensis White, Anomalia sp.,Marssonella oxycona (Reuss), Gaudryina sp., Bolivina incrassata Reuss, Buliminella laevis (Beissel),Cibicides beaumontianus (dOrbigny), Bolivinoides draco (Marsson), Textularia cretosa Plummer,Gumbelina sp., and others. The formation is Maestrichtian in age (n67).
Map 21a latest CampanianHST to K180 MFS
(68 Ma)Map dated at 67.7 Ma
In the Burgan area, this formation has thecharacteristics of a reef limestone and iscommonly highly porous, particularly at itsbase, which commonly results inconsiderable drilling trouble due to loss ofcirculation or water flows (ingression? cc).(Owen and Nasr, 1958).
The formation as a whole is of shallow-water deposition andis commonly highly porous (on58).
The Tayarat Limestone Formation is thelocal and only representative, in the Rutbah-
Gaara area, of the sediments of thewidespread transgression of Upper
Cretaceous time.
In southern Iraq and in Kuwait the Tayarat is recognised as theuppermost unit of the Upper Cretaceous. In these areas accordingto (on58) the unit is: essentially in the same facies as in the typelocality, .... it consists of brownish and dark grey granularcrystalline, dolomitic and sometimes anhydritic limestones andwhitish limestones interbedded with minor quantities of thin butdiagnostic black bituminous pyritic shales. The top of thisformation has been taken at the top of the first black shaleimmediately below which the first Loftusia appear.
The thickness of this (the Tayarat) formation variesbetween 300 and 900, with a probable average of 500.
In Zubair-3 reference section it is met between 4482 and5210(1366 & 1586m) (on58).
In the Zubair-3 well, the Qurna Formation is overlainby the Tayarat Formation, the contact being
conformable at the junction of dolomitic limestonesabove and globigerinal marls below. Reference
section Zubair-3, formation between 1586 to 1704m(118m thick).
In the Basrah area the Tayaratconformably overlies the Qurnaformation, which is a globigerinalmarl and marly limestone unit,
comparable with the upper partsof the Shiranish Formation, of
which it could be considered anoutlying tongue (n67).
In this general area Field & Jonesassigned a minimum thickness of
250 (76m) for the incompleteTayarat in this area (n67).
Tayarat FormationType section on the scarp face and crest ofJebel Tayarat, 21 miles nearly due south ofRutbah, lat 32 46N, long 4017E
South of the Widyan and Kifl areas, TayaratFm was found in all deep subsurfacesections and in some of the shallowstructural holes in the southern desert westof the Euphrates River (n67).
(on58) mainatained that in the Basrah-Kuwait area this formationis thicker than the outcrop section (n67).
The Tayarat Limestones are porous and occupy anextensive area in Al Widyan. (mf38) stated that theis areais an almost flat-lying Eocene and Cretaceous limestoneterrane that has very gentler slope and drainage towardthe east. The annual rainfall averages less than 10mm,and in summer and autumn this area constitutes the mostwaterless part of Iraq. A very considerable proportion ofthe rainfall probably percolates deep underground throughsolution channels in the limestone, and the ground wateris thus beyond the reach of shallow wells; however, deep
drilled wells near the underground solution channelswould probably yield water. A detailed account of this
subject was given by (mf38, p. 127-135).
Strike equivalents (d59, n67):The Tayarat Formation, described from the Western Desert area,is more closely comparable with the Aqra, in age, fauna and facies,than is the Pilsener. However the Aqra and the Tayarat formationsare given separate names because they are palaeogeographicallyand genetically distinct. The Aqra is limited to the tectonically-active, NE margin, and the Tayarat to the more quiescent, gently-shelving, SW margin of the broad Upper Senonian basin. Thereare no comparable, linking, neritic rock-units connecting the twoformations across the central zone of the basin. In the subsurfacesections of the Basrah area, the equivalents of the Aqra limestone,in comparable facies, are the Tayarat and Hartha formations. TheQurna Formation, which separates the Tayarat from the Hartha, isa marly globigerinal unit which would be interpreted in northernIraq as a Shiranish formation tongue.
(mf38) noted theformation in the Wadianarea, south of Rutbah.
The Hartha Formation underlies theShiranish Fm with a slightly disconformablecontact. The overlying Tayarat Formationis conformable and gradational; the contact
is placed at the junction of dolomiticlimestone above and globigerinal marlsbelow. In the Kifl area, the Shiranish is
directly overlain by the Aaliji Formation withunconformable contact. In southeastern
Kuwait the Shiranish Formation passes intothe Bahra Formation and in Saudi Arabia
into the Aruma Formation (n67). Shiranish Fm: Buff or ash-grey globigerinal marl, in some places dolomitic,and some marly and detrital limestone beds; it is glauconitic toward thebase and contains a rich microfauna. According to (on58) the Shiranish
marls in the Basrah area pass in southern Kuwait into white to grey densemarly microcrystalline limestone, which in places may contain grey chertnodules. This calcareous facies has not always been distinguished from
the adjacent formations. Similar changes have been observed west ofUbaid-1; at Safawi-1, it appears that all the Shiranish marls have passed
into chalky and marly limestone within the Tayarat Formation (n67).
General thickening of theShiranish Fm to the NW
(n67).
Rachi-1: 970 (thickestsection) (296m)
In the deep subsurface sections of SWIraq, the Tayrat Formation is generally
overlain by the Umm er RadhumaFormation (n67).
In southwestern Iraq, with the exception of extremewestern region in the vicinity of Safawi-1, where
it is underlain by the Safawi anhydrites, thisformation overlies the Shiranish Formation(formerly Qurna) conformably with lateral
interdigitation (n67).
Macfadyen (1938) described this area as follows: nearlythe whole of the Wadian (Al Widyan) is covered with flat-lying limestones occasionally conglomeratic. These arebelieved to be wholly of Eocene and Cretaceous age.Since the lithology is generally similar, and recognisablefossils mostly leached out, the Eocene-Cretaceousboundary appears to (be) unmappable without a greatexpenditure of time and labour (n67).
W.T. Foran (unpubl. data, 1940) described thecomposite Late Cretaceous section in the WidyanArea as follows (n67): Unconformity- especially inWadi Tibal region.Limestone, purplish grey, fossiliferous, containsLoftusia; yellow marls locally passing to sandstone;grey to white granular gastropodal limestones; andsoft yellow limestone, 27.2 (8.3m)
Chalk and marl with black flints,plentiful fish remains and a
microfauna typical Maastrichtiantype, 10km (d63)
Loftusia limestones(jb06f)
Ty Ty
Ba
(jw65) G
Ty
Ty
(sa96)
Sh(sa00)
(d59)
(lst/dol LST)(marly lst/LST)
TySh
TyQu
TySh
TySh
TyQu
TyQu
(n67)
approx 183m (n67)(n67)
296m= thickest Tayarat
Fm. in basin
(a92b)Mu
(a92b)Mu
(a92b)Mu
(a92b)Mu
(a92b)Mu
Sh
(jw65) G
?Sh
Tj
npc
Abs
Tj
Sh
Sh
Sh
?Pi
TySh
AbsAbs
Abs
Sh
Abs
Sh
Sh
Sh
Ty
TjSh
Sh
Sh
Sh
Abs Abs
Sh
ShSh
Aq Aq
(d63)Sh
(d63)
(d59)
(n67)
(n67)
(n67)
(d59)
(d59)(vb59)
(d59)
(n67)
Tj(d59)
(d59)
(d59) Tj(d59)
Tj (d59)Aq & Tj(d59)
Aq & Tj(d59)
(d59)
Tj (d59)
Tj(d59)
Tj(d59)
Tj(d59)
Tj(d59)
Tj(d59)
Tj(d59)
(d59)
Tj(d59)
Tj (d59)
Tj(d59)
Tj (d59)
Tj
(d59)
(d55)
(ka89)
(ka82b)
(d63)
(ka82b)
(cc re-interp. afterka82b data)
(d59)
(d59)
(d59)
(d59)(jd76)
(ka82b)
(ao90)
(d59)
(d59)
(d59)
(d59)(d59)
(d59)
(nq60)
(d59)
(d59)
(d59)(d59)Sh
(d59)hiShhiAq
Abs (d59)
Abs(d59)
Sh
Abs(d59)
Abs (d59)
Abs(d59)
(d59)Sh
Pi(ma86)
hiTj
(d59)hiTj
(d59)hiTj
Lc(aq98)
Di
Rudist reefalfacies
Abs (ra86)
(s96)
(ra86)(ra86)
(ra86)
(n67)
Aq
TySh
TySh
Dolmarl & shale
TaSh
TySh
Aq
Abs
Pi
Ta/HaHa
HaFlowed 700
bod (s96)
Sh
(d59)?Di
Ty 105m total (n67)Sh 168m (n67)Shoaling up:Dol over LST
(n67)
Lk (w74)Dolomites
Sh(w74)
Pm
(am79)Sh(am79)Sh
Thin (10m) LST(d63)
Hard, with oolitic &chalky intervals,
abundant Chara(d63)
Sh(b93)
Sh(li97)
Sh(d63)
Abs(d63)
Sh(d63)
Sh(b99)(Thin)
Sh(b99)
Sh(kh97)
Sh(b99)
Sh(b99)
Dol(mc85)
Sh(oec89)Cherty marly
LST(oec89)
Thin chalkyLST & marl (n67)
Sh(sc64)
Sh(jg06)
Sh (jg06)V. condensed
Sh (oec89)CondensedLST, marl
Sl. dolomitic/anhydrite
Marly LSTV. thinLST
Top-Cret ingansseri zone
(ao90)
MarlyLST
Thin siltyShiranish Fm.
(d63)
Sufayah-1 to 3(ka82b)
Sh(d63)
El Bouab & El Bardeareas only receivedvery thin Shiranish
cover (am79)
(d63) LST
Atshan-1 is noted asbeing more eroded
than Alan-1 on the (d59)chronostrat (d59)Sh
LST, some marlsTotal fm. 1036m
thick (nq60)(pt04)
Very thick (1050m)Late Campanian -
Maastrichtian(pt04)
Lk
Marly LST (sa00)
Top res @ 1992m40m pay, = 15%
K = 143.5mD,20.4 API oil(ja06)
SHIRANISH FM.Basinal marls and limestoneswater depths >200m. All deep
subsurface sections in theBasrah area and Kuwait,between 276 and 137m
TAYARAT FM.Shelf carbonates
Exact position of margin requires more c a l i b r a t i o n
Total 305m ofShiranish Fm. est.120m eroded (nq60)
Sh(nq60)Thick marly LST
Sh(ja06)Top @ 2082m
fracture reservoir(ja06)
Sh(sm10)Top Shiranish@ 1631m27 API oil,2.71% sulphur (ja06)
Tested ?1686m(tm70)
Est. 145mmbo (ve04)(? part in Cenozoic)
(rh80)
(on58)
(n67)
(n67)
(n67)
Argill LSTDol LST
Marl & shale
approx 183mDol
Argill Dol
LSTMarly LST
Marl & shale
(lst/dol LST)(marly lst/LST)
Shiranish isthin in Rumaila
(n67)
(n67)
LSTAnhy LST
(alternations)Dol
Anhy dolBasal LST
LSTMarl & shale
TySh
(ra78)Uk(ra79)Ma
Uk(ra81)
Uk(ra81)
(ra79)UkShelfal microfacieswith orbitoids
(d59)Ty
(mf58)Ta
(mf58)Ta
(mf58)Ta(mf58)Ta
(mf58)Ta
Ty 90m total (n67)Sh 137m total (n67)
Pi(d59)
Abs(d59)
npc(d59)
Pi(d59)
Sh(sy84)
npc (ra86)
(ra78) LST
(ra86)Ha
?Sh(ba00)
?Sh(ba00)
(ba00)?Ty
(ba00)?TyShelffacies
Normal Strike Slip
InvertedThrust
FAULTS
ZUBAIR
Kand-1
(d59)
Z-31
Lf
Erosional boundary
Field nameFacies boundary
Appraised field
Discovery
Gas field
Oil field (Producing)
Well approximately located
Exploration well
Field centre point
Well located withlongitude &latitude
Data point usedin this map
Other well
Outcrop
Formation
Data Source (refer toreferences database)
Condensate
SURFACE GEOLOGY
Shoal watercarbonates
Low energy shallowmarine carbonates
Outer ramp/slope carbonates
Deep basinal carbonates
Supratidal/sabkhacarbonates & evaporites
Restricted circulationbasinal carbonates
Shallow basinal/intrashelf basin carbonates
Massive subaqueoussulphates
Massive halite
LL
L
Fine shallowmarine clastics
Clastic slopewith turbidites
Clastic basinal
Lacustrine
Hiatus
Ophiolite
Volcanics
Coarse grainedcontinental clastics
Fine grainedcontinental clastics
SUBSURFACE FACIES
Mixed carbonate-clastic lagoon
Coarse shallowmarine clastics
BASE MAP
0 50 100 150 200km
Use of this map is subject to the conditionsof the contract of purchase. For more
information contactwww.cambridgecarbonates.com
Projection : Lambert Conformal ConicEllipsoid : Clarke 1866
Central Meridian : 41 30 00 ECentral Parallel : 33 00 00 N
Standard Parallel 1 : 36 00 00 NStandard Parallel 2 : 30 00 00 N
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