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

Camb

ridge C

arbona

tes Ltd

. Sam

ple