Van Golu Kiran MALTEPE 38°E WEST 40°ESARICAK YENIKOY EAST Budak 42°E 44°E 46°E 48°E 50°E 52°E KATIN KURKAN YATIR YENIKOY Hazro N SOUTH Hazro-1 & 2 Hezan Handof-1 Divana Silvan-1 38°N KURKAN BARBES Hazro S Kmbosdag Korudag Katin-1 SELMO 38°N CELIKILI Indet BEYKAN KAYAKOY Doondag Indet MALTEPE Tayarat Formation Indet Indet O. Sungurlu-1/A Indet Kastel-1 SILIVANKA DODAN Caspian Indet Indet Indet ADIYAMAN Indet Indet Macfadyen (1938) pointed out the presence of a fish bed, in presumably Cretaceous sandy limestones, at Indet Indet Coskunsel-2 PIYANKO E. Kahta SAHABAN KURTALAN Tabriz Tut Adiyaman-8 Karakus-10 KAYAKOY WEST GERMIK Kavikadag-1 Gur Ayarat, where abundant teeth but fewer bone fragments and vertebrae were found (n67). Durukaynak-2 Cemberlitas-14 K. Akceli-1 Bucak-1 Diyarbakir Gölbasi Indet Sinan-1 Indet Siverek-1 Alidami Siirt Diagnostic fossils and age Fossils in the Tayarat Fm include: Loftusia morgani Douville and Ompahlocyclus Karakopru-1 Alidag-2 SEZGIN MAGRIP Besni-1 GARZAN Kentalan-7 macropora (Lamarck). According to H. A. Field and K.D.Jones (unpubl. data, 1958) the Tayarat LimestoneSea contains Terbüzek ADIYAMAN KAHTA Besikli-6 Daryacheh ye Orumiyeh Indet WEST RAMAN Kentalan-2 corals, rudists (including Eoradolites?), gastropods, lamellibranchs, and algae. They maintained that generic SOUTH identification is often difficult as most of the original structures have been destroyed by recrystallisation and Sahabe-1 Kahta-2 RAMAN K. Maras Indet some by dolomitisation. In addition to the fossils recognised in the type section, the following microfossils Indet have been determined from the subsurface sections: Lepidorbitoides socialis (Leymerie), Indet Gercus-1 Orbitoides media (d’Archiac), O. apiculata, Ogivalia parisiensis d’Orbigny, Rotalia skourensis Pfender, TURKEY R. trochidiformis Lamarck, Globotruncana spp., Dictyoconus sp., Dicyclina schlumbergeri Munier-Chalmas, Rumelan-1,4,5,6 LOWER and Pseudochrysalidina sp. (n67). Map 21a Souedie-1,2,3,6,7,11,16,30 Indet GERMAV Sh (ni72) Palaeontology: Lofutsia morgani Douvillé and Omphalocyclus macropora (Lamarck). Indet Type Section Indet Argill LST Harbol Samur Dag Thin silty Kurra Chine (top) Aqra Limestone Fm. Avsar-1 Mardin Shiranish Fm. Cudi Dagh “The formation as a whole is of shallow water deposition and is often highly porous. Species of Loftusia and (sc64) Sh Mirga Mir N Flank Ora Fold (top) also at Dar-e-Tesu interbedded with Tanjero (d63) Shish Lepidorbitoides are common in the limestones, and Omphalocyclus in the shales” (on58). latest Campanian Gel-i-Senet Geli Khana Chia Zinnar Zap clastic Fm. Rasht Bakuk-1 B.Yolacan-1 DERRIK N. Kaista Village A similar fauna is present in the Tarbur Formation of Iran and the upper part of the Aruma Formation of Saudi G.Dincer-1 Yolacan-3 Chalki Nasara (top) Darari Ora Police Post Also at Gerwa Zhori, Qamish, Jebel Gara, Cilesiz-1 LAILAK Benavi Geli Khana Arabia (jw65). jalan-101 DERRIKSh(d63) Shiranish Aq Ora Cirque Zinta Gorge, (vb59) C-102 Zakho (d59)Sh Hadiena/Aq(d59) Kanun ALIANE Badran-1 KARATCHOK Banik (d59)Hadiena Village Argosh Shamu-1Camurlu-101 Qaratchok Dagh Marly Govanda Plateau HST to K180 MFS Qaratchok hi hi L Qamichlie-1 Aoda LST TAWKE (d59) Amadia (d59) (d59)Tj Oudeh-107 Dagh N. f Qaratchok-2Sh Sh Chia Gara Aq I R-6 Sh HAMZA (d63) Gel-I-Garagu/Garagu Zaita M Hadidi-1 R-7 (am79) Baluti (NW) Naz Oucharheu El Bouab & El Barde OUDEH MUSHORAH I K East-1 K East-2 Mushorah-1 Gara Village Baluti Village (SE) Aq & Tj T Ceylanpinar areas only received K-5 (am79)Sh Sufaiyah-1 (ao90) Aq Ru Kuchuk Tyron Malout Sh Dohuk (NE) (d59) Zhazhoke Tj (d59) Baflioun-1 very thin Shiranish Khurbet-1 K East-3 SOUEDIE Top-Cret in(ao90) Zibar O Shiranish Formation (68 Ma) Aafrine K EAST Sh SUFAIYAH AQRA Mirgasor Tj(d59) F Amanos Baflioun Dome Afendi-1 cover (am79) gansseri zone Dohuk (top)\ Aq & Tj Barde-2H Naur-1 (ka82b) SHAIKAN Tj(d59) Kourt Farmuz El Barde-1 A-29 Dohuk (SW) Shaikan-1 (d59) O AL BARDE Naur-101 A-16 AIN ZALAH Gund-i-Shikart MaznaTj(d59) P Passes laterally westward into the neritic Tayarat Formation (n67). Meidannki Sirrine Pm (d63) Abtakh-1 Aqra (top) El Bouab-2 Tel Brak El Barde-101 Naur-102 A-19 Abs(d59) JEBEL KAND (d59)Tj Naouren Tj (d59) H Aleppo-1 GULLAR Simrit-1 (d59) Diza Diagnostic fossils and age Fossils include: Cytherella spp., Bairdia spp., Nodosaria sp., Bassouta Kharab El Bouab-1 Sh(d63) V. thin Sh Gullar-1 Butmah-1 Rafan-1 Aq?Bekhme (top) I Echlé LST Jebel Khand-1 Diyana Tj(d59) O Globotruncana spp., Cristellaria spp., Gyroidina naranjoensis White, Anomalia sp., Map dated at 67.7Babol Ma Marly LST LST(d63) (d59) Sh B-2 B-7 Sh (oec89) Sh Jafar-1 (b99)Sh Tel Aswad-1 Nora-1 (cc re-interp. after Barsarin Naokelekan L Marssonella oxycona (Reuss), Gaudryina sp., Bolivina incrassata Reuss, Buliminella laevis (Beissel), AL HASAKAH ka82b data) Gusair-1 Abs B-15 BUTMAH Condensed Sareshmar I Maghlouja-1 (d59)Abs (d59) LST, marl Tj(d59) T Cibicides beaumontianus (d’Orbigny), Bolivinoides draco (Marsson), Textularia cretosa Plummer, Hasakah Kurrek Rowanduz Razan Tel El Arous Sufayah-1 to 3 GUSAIR Alan-2 Bashiqua (d59) E Gumbelina sp., and others. The formation is Maestrichtian in age (n67). Base map last amended 1/1/11 Data last amended 14/3/11 J. Aziz Abu Hadjar-1 Alan-1 Maqlub Tj(d59) Tj Tj Abba-1 Sheikh Sh(b99)Hol-1 (ka82b) Abs IRAN Suleiman-1 Mamissa SASAN Sh Zar Gelli S Aleppo (jd76) Abs(d59) Hawler-1 TANJERO Sh(d55) Sasan-1 ALAN HAWLER Tj(d59) Raqqa-1 TISHRIN Tchembe-1 Sinjar (d59) Sh Shaqlawa Kometan Endezah Syrom-2 (w74) Bara Hawler-2 Yayladag Buhayrat Al Asad Kharbaka-1 Tishrin-5 Sh Jaddala Loc Atshan-1 Abs Mosul Ain Safra (sy84)Sh FLYSCH Hamadani-1 Syrom-3 (kh97) Sh IBRAHIM Tj Shailkan © Use of this map is subject to the conditions Sh Jaddala Town Ibrahim-1 (d59) Kenan-1 Syrom-103 Syrom-1 SALIEH GHOUNA(d63) Al Hasu Umm a Dhiban (d59) 36°N Beida-1 (d59) Sh ATSHAN Balki Syrom-4 Jibisi-208 Ghouna-1 TEL HAJAR Rania Tj(d59) of the contract of purchase. For more 36°N Salhia-1 Sh(d63) AIN GHAZAL DEMIR DAGH J-203 J-2 Tel Hajar-1 ADAIYAH QALIAN Demir Dagh-1 Strike equivalents (d59, n67): Hairan-1 Gbeibi-101 (ka82b) Atshan-1 is noted as Arbil Kolosh Qalaat Jebissa-1 J-3 GBEIBE Sh (d59)Sh Qalian-1 Sh (jg06) NE Koi Sanjak The Tayarat Formation, described from the Western Desert area, information contact Jabar Makman (ka89)Abs being more eroded Adaiyah-1 (d59) V. condensed Shorish-1 is more closely comparable with the Aqra, in age, fauna and facies, Rim-1 JEBISSA Abs Koi Sanjak hi Well 151 (d63) Sheikh Sollakh-1 than Alan-1 on the (d59) Qasab-12 QUWAIR (d59) than is the Pilsener. However the Aqra and the Tayarat formations www.cambridgecarbonates.com Abs QASAB TAQ TAQ Tj SYRIAMaskane-1 Cheikh Judid-1 d63 notes absence Sh(ka82b) chronostrat (d59)Sh Mishraq-1 Quwair-1 KIRKUK are given separate names because they are palaeogeographically Qasab-2 Taq Taq-1 S Jawan-2 Quwair-2 KHURMALA Taq Taq-2 (d59) hi Khanasser-1 of lformer atest Maza-1 h (jg06) Gulneri (d59) and genetically distinct. The Aqra is limited to the tectonically- e Sh l NAJMAH Kirkuk-117 Markada-101 f Tj Tj Maastrichian in & Kirkuk-114 HARTHA FM. TAYARAT JAWAN N-2 Najmah-29 Dokan Qamchuqa top active, NE margin, and the Tayarat to the more quiescent, gently- Slenfeh Bahri-1 s Balikian WNW Rasafeh l K-317 Dokan New Bridge Jib Ganem-1 Jebissa, Ghouna o Abs(d59) Sargelu (NW) shelving, SW margin of the broad Upper Senonian basin. There Mityah-1 p Q-2 Sheikh Alas KIRKUK Mouth of Gorge Joubeh Markada-1 Toueman-1 HIBBARAH e QAIYARAH SUBMARINE Hajrawa Mawal are no comparable, linking, neritic rock-units connecting the two Tehran Jub El Abyad (b99) MARGADA (w74) HIATUS AVANAH Sargelu (SE) Azar-1 Sh Lk Hibbarah-1 Q-13 Qaiyarah-1 Absent Azkand Surdash (SE) formations across the central zone of the basin. In the subsurface Well 7 Well 201 Makhmour Avanah/Kirkuk-116 Diza 0 50 100 150 200km Dolomites (d59)Sh npc(d59) Zahis Miran E-1 sections of the Basrah area, the equivalents of the Aqra limestone, Sfiyeh1 Amara-1 Rasafa-1 Derro-1 Q-55 Ali Rash npc (d59) Derro-2 Tel Zrab-1 Enayat SHIRANISH Qarah Chauq-2 CHEMCHEMAL Pir-i-Mugurun Choarta in comparable facies, are the Tayarat and Hartha formations. The Wadi Aabeid-1 Tibni-1 Makhmur-1 Miran W-2 Well 203 Sh(b99) QARA CHAUQ BH-3 Kirkuk-14 Qal Kand Qurna Formation, which separates the Tayarat from the Hartha, is Zidan-1 Misrame-1 Habari-1 (Thin) KIRKUK BABA Miran W-1 a marly globigerinal unit which would be interpreted in northern Well 34 Hatra BAI HASSAN Bazian-1 Koni Kawa Panjwin Datayeh Well 153 Biar er Rhoûn/Jebel Bishri BH-81 Kirkuk-175 Sarchinar Kseibyeh Well K-16 Al Suwar-1 BH-13 Kirkuk-109 as a Shiranish formation tongue. Well K-5 Zemieh-2 Massoudeh-1 Qarah Chauq-1 Tourkmaniye Fort Well 33 K-1 Abs(d59) Chemchemal-2 Shahr-i-Zur Well-6 Kabbaz-4 Tj (d59) Dolaa Bishri-101 Shaafa-101 Sadid-1 Kirkuk As Sulaymaniyah Projection : Lambert Conformal Conic El Mamlaha SW Rejm Tar 400m Tabiyeh-104 KHLEISIA KHABBAZ Qal’Gah Hamah Hajjaneh SADID KHANUQAH K-3 Kirkuk-85 Qadmous Well K-25 Tabieh-101 Well-5 Ghilizardia Ellipsoid : Clarke 1866 J. Al Qom Dâbba Dafayen-3 El Khuwar-101 Khleisia-1 Khanuqah-2 Wadi Al-Ouyoun Pi(ma86) Kirkuk-49 Well-3 Jafra-107 Rasin-101 A. Shams W. Hararit Ghreta North-101 Khanuqah-1 Central Meridian : 41° 30’ 00” E Al RASEM 678m Al Hir-1 Total 305m of J-19 J-15 Derbannd-i-Sajirrma J. Sawwanet Sawwanet Shiranish Fm. est. Didi-1X 500m Rudist reefal MAKHUL J-22 J-16 SHIRANISH FM. Baski Zanur Tj Ouyoun Treize Loc Sijan-101 120m eroded (nq60) J-21 hi Central Parallel : 33° 00’ 00” N J. Abou Douhour Beer Qdem facies Makhul-1 J-20 Dagh Pila Spi (d59) Machta Helou J Abou Roujmein Omar-101 Well-8 Pi(d59) J-42 J-26 KM-3 Aj Dagh Tj Hawar-Dalamar path Jweikhate J. T. Satrah Al Waha-1 J-13 KOR MOR Derbannd-i-Khan Standard Parallel 1 : 36° 00’ 00” N Marmarita J Shaer J. Thanyet J-4 Sirwan Dalamar Qahar-103 Makhul-2 Kor Mor-2 Kashti Nasirah J. Bilaas As Safra J. Satih (NE) Well-9 Pi(d59) JAMBUR J-18 Well-1 J Ash Shaer-1 ASH SHAER Soukhne Didi-1 Well-7 Sirwan- Sazan Police Post Standard Parallel 2 : 30° 00’ 00” N Homs Hamrin-5 Sh(ja06) Kurdamir-1Baranand Gu(S78) J. Shomariyeh J. Satih (SW) Top @ 2082m Thick globigerinal open Dagh Balambo Jebel JTP-7 El Hamra-101 Balambo Jebel al Marah Soukhne Anah Graben was deep and narrow in the Late Cretaceous; it had a ‘low intensity’ of water Loftusia limestones Hamrin-6 fracture reservoir sea marls and marly Well 27 HAMRIN (ja06) Jebel Abaid J. Mazar (NE) circulation (bk92). N-S and E-W faults controlled the Tinif Trough and the Damluk Trough, (jb06f) JD-1 limestones (nq60) loc. Doubayat-1 proven by boreholes to the west and east of the Akashat Platform and on west side of the ABU FUDHUL Hamrin-4 RAP-3 Rutba-Hail Arch (trending NNE-SSW)(Karim, unpubl. in bk92). Troughs were sites of deep Pulkhana-6 Gu(S78) JTP-21 AL FAID N Well 6P-3 Hamrin-3 PULKHANA JIHAR El Madabe NW-101 oceanic sources of P-rich, cool upwelling currents throughout the phosphogenic eposides; ? Jebel Banu CHERRIFE J. Mazar (SW) Jebel Hamrin-1 Est. 145mmbo (ve04) Sample were in free connection with Tethys (bk92). Akashat (NE) and Ethna (SW) platforms represent J. Assater PALMYRA Well 6P-4 AJEEL Pulkhana-3 (? part in Cenozoic) Hamadan Cherrife Jebel al Aasafir elevated, submerged blocks that formed ‘ideal traps’ for dissolved phosphorous transported Sarqala-1 Jebel Shaloradar BASE MAP Daryacheh ye Namak Well-10 Hassan-1 by upwelling currents from the troughs into the shallower and warmer shelf environments BAIJA (nq60)Sh Shakal-1 Palmyra Hamrin-2 Thick marly LST loc. (li97) (near-shore to basin slope) to the S and E (bk92). Platforms also have non-phosphoritic (tm70) El Qaa-1 J. Hayan Sh ALLAS Tested ?1686m Kifri Jebel Bezniyan N shelfal facies. Arch crest may have occasionally been emergent, with the development of Top Shiranish P-5 Gu(S78) Qom Well 6P-5 @ 1631m Sh(sm10) Exploration well Formation J. Abou Rahba clastics and intertidal facies (bk92). East of the crest, reef and back-reef facies are represented HAMRIN Chia Surkh JTP-20 Lf by the Hartha and Tayarat formations (bk92). 27° API oil, JTP-6 ABU RABAH J. Naqnaquyeh (NE) J. Abtar (NE) Well 21 Well 24 DIGMA 2.71% sulphur (ja06) jebel Bezniyan S Well K-15 CHIA SURKH JTP-22 Abtar Est Well-11 4 TIKRIT Tikrit-1 Injana-4 Gilabat-3 Qumar-1 J. Naqnaqiyeh (SW) Well 23 200m PO MARL Injana N Jebel Bawgaru Data Source (refer to LEBANON Well 29 Beds with orbitoids; recrystallised, dolomitised, porous, 163.5 to 237m. Fossils generally INJANA Gilabat-1 QUMAR Other well J. Abtar (SW) JTP-4 (d59) J. Bardeh Well 26 Swab-1 obscured by diagenesis, particularly in upper levels where abundant orbitoids are extremely Injana S Injana-5 references database) Well 19 Wadi es Souab GILABAT JTP-23 (b93) Sh poorly preserved or washed out (ra81). Samples from 163.5 and 203.5m contain Pseudorbitoides (nq60)Sh Emam Hasan-1 Gu(S78) Qaim Anah-2 spp. (partly in fragments; 163.5m) Lepidorbitoides minor Schlumberger, Lepidorbitoides sp., loc. Kariaten-1 LST, some marls KA-1 Patoi-1 Anah-1 Anah Graben Orbitoides tissoti (Schlumberger), Orbitoides media (d’Archiac) (very rare), Planorbuilina Emam Hasan-2 cretace (Marsson), Sulcoperculina gr. dickersoni (Palmer)(163.5m), Different small rotalids, Total fm. 1036m Lk(pt04) JTP-2 JTP-1 Well located with J. Rmah Well 28 Gu(S78,B95) Bakhtaran KH-17/7 Di (d59) minute anomalinids, a few pelagic (globigerinal) foraminifera etc. (ra81). thick (nq60) Very thick (1050m) Khanaqin JTP-5 loc. ?M. Dashti Z-31 Gas field Marbat Beds 15 to 50m thick; cyclic alternations longitude &latitude Type Locality Wadi Fuhaimi KHASHEM Late Campanian - Gu(B95) JTP-3 indet. 34°N Chalk and marl with black flints, of fining-upward fluvial clastic sediments passing Samarra-1 JK-1 JARIA PIKA laterally into deltaic sediments, mostly sandy Akkas-1 Digma Marl Fm. AL-AHMAR Maastrichtian J. Abou Zounnarplentiful fish remains and a Mileh Tharthar-1 34°N dolomicrites (bk92). (aq98) Lc B-15/7 Ty (pt04) Karia Pika loc. microfauna typical Maastrichtian Marbat Beds: inshore (coastal onlap) facies; ?Di(d59) (d59) Samarra M-4 ND-2 Naft Kaneh-3 J. Smekai Na’aja Beds overlain by Safra Beds are offshore MILEH NAU DOMAN loc. loc. Well approximately located Condensate type, 10km (d63) Transgressions contemporaneous with Sh Kand-1 (CC notes). DAMLUK THARTHAR Dol(mc85) M-3 NAFT KHANA J. Zinnar AKKASopening of deep troughs, grabens and MANSURIYA NK-35 Well A16 BH-5 development of intrashelf basins, securing KH-12/7 loc. RFH-4 Saba Abar TROUGH. Mansuriya-1 Sh Vijonan Fardows Bloudan Al Butmiyal Well 9-1 open marine communication with the Tethyan Uk(ra79) Naft Kaneh-32 N. Shahabad-1 Well 2 35m N.E. Shah Babagir Well A15 J. Dneir deep waters since the Upper Campanian, Shelfal microfacies Naft Kameh JTP-8 Outcrop Oil field (Producing) BH-6 when at its concluding stages, the first with orbitoids Buhayrat ath M-2 Gu(B95) Wadi Dwekhlet DIGMA FM. phosphogenesis appeared (bk92). Mkemen Slebi Mirrah Tanf-1 30mAkashat BALAD TG-1 Borudjerd Well Al-Qussair Well K6 Well 9-2 BH-2 Tharthar Wadi Saba Abui 25m loc. RFH-1 Well 49 B-7/12 TEL Ltd.Borudjerd/ Akashat Thin (10m) LST 20m 15m Nan-1 JTP-24 Field centre point Tell Sad Rusheh BH-3 npc (ra86) GHAZAL Darbodom-1 JTP-27 Appraised field Well K3 (d63) TANG-E BIJAR Sankul-1 Well Harran An Na'aga Ghadir an Nijili B-13/7 Huleyan-1 El-Awanid Hard, with oolitic & Note: Shiranish reported Baquba Tang-e Al Juwef Al Juwef Ras Semhat JTP-16 loc. (W) Well 9-3 T19 also as absent in the Abu Bijar-1 JTP-10 chalky intervals, (d59) Abs KH-5/1 Qasr Muhaiwir Oligocene B-4/7 EB-77 RAP-6 Data point used J Sis abundant “Chara” Bir El Rah Hit-1 Jir-Awasil-Hit-Mileh EB-80 JTP-15 Kuh-e Safid/ Well 44 Wadi Semhat Al Alaif Wadi NE Wadi Hauran tributary Albian Abs(ra86) SHIRANISH FM. Discovery (d63) Mulussa (E) Thartar area (du59) RAP-2 Khaneh Sorkh-1 KRD-23 in this map Dunnington et al. (1959) state: “Passing northwards from Jebel Tayarat through Jebel Thoba, Bir Mulussa EB-69 Basinal cherty loc. JTP-14 Tang-e Garab and towards the western rim of the Ga’ara depression, the Tayarat limestone is cut out UB8A EAST BH 100/B/85 Wadi Ubaid Qasr Amij road limestones, marly. Gu(S78) Kabir Kuh Well Alqin progressively, by the erosion of its upper parts, and also perhaps by onlap convergence. Tel Aafair Qasr Amij Nafatah-1 NAFATAH JTP-11 RAP-1 In the section of Hill 270 (Lat 33°18’00”N, long 40°10’30”E) and Khasm Mulussa (lat 33°18’30”N, Mulussa (W) Deepwater >200m JTP-18 NE Flank KRD-27 ‘SHIRANISH’ Wadi Hauran SW B-7/13 Awasil-5 EB-10 Anjir-1 Khurramabad Facies boundary long. 40°07’E) the formation is absent, the Paleocene Umm Er Radhuma formation resting Wadi Hauran/ ?Pi (vb59) Fallujah-1 EB-11 6 miles NE of Arkwaz Gawar D. Sonoh-1 KRD-24 ZUBAIR Field name discordantly on eroded M’sad Formation. The convergence increases northwards, so that, KH-9/7 (d59) Pi Gu(S78) loc. Tang-e Garalfd IN TINIF Khasm Mulussa Wads Agar Zor Hauran MC4 Sh EB-53 EB-12 JTP-12 Gu(S78) loc. at Ras Semhat, the Umm er Radhuma rests directly on the Triassic Ga’ara Sandstone. The Hill 270 (ra81)Uk Ar Ramadi Kabir Kuh-1 Kuh-e Pasan SARKUN Kuh-e Saltan details of the erosional convergence from Tayarat to An Nadhara have not been studied”. TROUGH (d59) Abs Muyat/An Nisr EB-3 Abs(d59) EB-7 Gu(S78) Kabir KuhGu(S78) VEYZENHAR Kuh-e Amiran SW of crush zone area EB-4 (SW flank)(jw65) loc. G KRD-26 Na’aja Beds 2-18m thick; mostly dolomite with basal sandstones, chert nodules, KH-5/8 Abs Abu Jir-1 RAP-4 Veyzenhar-1 Sarkan-1 Erosional boundary Km160 KH-7/7 NAHRAWAN Kuh-e Sarkan thin phosphorite horizons, charophytic dolomites; top is siclicified shelly (ba00) ?Sh OLDER GEOLOGY BH-7A (d59) EB-6 JTP-9Gu(S78) Oshtoran-Kuh (pelecypod) limestone (bk92). Cycles often have hiatal surfaces (hardgrounds, (ra81)Uk EB-1 Kuh-e Anaran Gu(S78) MALEH KUH loc. RFH-2 Rutbah Gd(B95) RFH-3 toughgrounds). Mineralogy: montmorillonite-palygorskite-sepiolite, chert, MC2 KH-5/2 OUTCROP KH-5/9 BH-80/1 Baghdad (oec89)Sh Kuh-e Kalak Maleh Kuh-1 KRD-25 porcelanite, phosphorite (bk92). JTP-13 MGH-2 loc. Cherty marly Gu(S78) loc. loc. loc. JTP-25 Wadi Hauran at Rutbah Rutba BH-48A EB-2 RFH-6 Minor quantities of phosphatic material may be Wadi Saggar OPEN SHELF (oec89)LST JTP-26 RAP-5 HALUSH found in the fossiliferous and chert beds in the Wadi M’Sad with orbitoids EB-5 BADRAH loc. Chal-e Sheh Risha 2 Risha 11 area south and west of Rutbah (n67). Ty (d59) loc. BH-80/1 Badrah-1 (jw65) loc. RAP-7 Kuh-e Anaran G loc. FAULTS Northern Highlands 2 MC3 B7-7 Gu(S78) loc. MGH-5 loc. Traibel Dolomitised and recrystallised B7-6 loc. MGH-3 loc. Mu(a92b) Changulah-1 SAMAND Gd(B95) loc. Risha 17 limestones with orbitoid- Gu(S78) loc. MGH-4 Omphalocyclus assemblage (ra86) Isgahe Taleh Zang area Pal-e Zarreh area Risha 15 Mu (a92b) Jebel Tayarat B 7-4 loc. Normal Strike Slip Risha 1 (d59)Ty loc. KH-5/6 ?Sh MC1 KH-5/4 B 7-9 B 7-10 MGH-1 Tang-e Do Risha 7 (ba00) Tayarat/Hartha Formations (undifferentiated; poor fossil Musaiyib-1 Qalah Nar-1 loc. Risha 14 Risha 10 Risha 9 15mKH-5/5 Tayarat Formation “Ha “(ra86) loc. Gu(S78) loc. Risha 12 Risha 6 B 7-8 preservation does not allow the Maastrichtian, Campanian Esfahan Mu Risha 3 Type section on the scarp face and crest of Gu(S78) (a92b) Risha 8 and possibly the Upper SantonianBehr to be distinguished):al Milh 108 The Hartha Formation underlies the loc. Risha 5 Jebel Tayarat, 21 miles nearly due south of to 229m depth, orbitoid beds that are highly recrystallised, Daloori-2 Kabud-1 RAP-8 Risha 13 Risha 16 Shiranish Fm with a slightly disconformable loc. loc. LAB-E SAFID Thrust Inverted Risha 4 Risha 18 Rutbah, lat 32° 46’N, long 40°17’E dolomitised and in places possibly also silicified with few loc. loc. Qitar el Abd 1 Wadi Tubel contact. The overlying Tayarat Formation Daloori-1 loc. RISHA Mu (a92b) Jebel Ithayna primary characteristics evident. Orbitoid external moulds Karbala Gu(S78) KABUD loc. loc. General area (mf58) give this interval a distinctive appearance. is conformable and gradational; the contact Danan-1 QALEH NAR loc. Na’aja Beds post-second (more important/extensive) transgression (K180), to the west of the Rutba-Hail Arch. Semi- Ta Ta (mf58) DANAN B 7-11 Gu(S78,B95) Dalpari Kuh-e Gurpi-1 Northern Highlands 1 restricted inner shelf environment, passing occasionally into shoreline (bk92). Deeper facies deposited in troughs. Most is placed at the junction of dolomitic Al Kut Dhafriyah-1 DEH LURAN Deh Luran Ga’ara was emergent with fluvial (Marbat Bed) deposition, notably on the northern rim (bk92). There were between 3 and (mf38) noted the Jelta Solution Hole limestone above and globigerinal marls loc. loc. Smeica 1 formation in the Wadian 7 transgressive events, ranging from near-shore to central shelf biogenic barriers, organised in a semi-circle extending Ta (mf58) (s96) Ha Merjan-1 below. In the Kifl area, the Shiranish is loc. from N and W flanks of the Ga’ara Uplift to the S along the western side of the Rutba-Hail Arch (bk92). In the S. part, area, south of Rutbah. LAGOONAL IRAQDHAFRIYAH Tang-e Pabdeh Na’aja Beds include reef and backreef facies similar to the underlying Hartha Formation, suggesting frequent southerly PHOSPHATES:SEDIMENTS UPWELLING ON WEST PO4 OF HIGH Flowed 700 MERJAN directly overlain by the Aaliji Formation with AHDAB N. KH-5/7 An Nisir Ahdab-1 Zard Kuh change from inner shelf to reefal build-ups. In deep subsurface sections west of the investigated area (?KH-5/6 and 5/8? Abu Ghar bod (s96) unconformable contact. In southeastern Abu Gharib-2 AG-5 CHESHMEH CC Notes) inner shelf-reef facies pass into deep open marine facies towards the N and W, where outer shelf environment ?Ty(ba00) West Kifl-1 Kuwait the Shiranish Formation passes into AHDAB Ahdab-2 Dezful LALI SUBSURFACE FACIES prevailed in the both troughs (bk92). JEED FM. The Tayarat Limestone Formation is the Ta (mf58) Abu Gharib-12 loc. Shelf B -19/7 B7-3 the Bahra Formation and in Saudi Arabia ABU GHARIB Lali-2 Strat well on Taplin Risha 23 LT MAASTRICHTIAN local and only representative, in the Rutbah- KH-3/7 Shiranish Fm: Buff or ash-grey globigerinal marl, in some places dolomitic, Abu Gharib-3 facies Ga’ara area, of the sediments of the Ta/Ha (ra86) B-18/7 into the Aruma Formation (n67). loc. Mu (a92b) KH-5/3 (ra78)Uk Very recrystallised (ra86) Kifl-1 and some marly and detrital limestone beds; it is glauconitic toward the Abu Gharib-101 KHUSH loc. 32°N widespread transgression of Upper with indeterminate Ha B-2/7 KH-1/7 Afaq-1 base and contains a rich microfauna. According to (on58) the Shiranish Buzurgan-1 Godar Landar Shoal water Coarse grained Jeed Fm. is the basal phosphoritic unit of an interval on the ?Ty(ba00) (ra78) LST Indeterminate rudists (ra86) Sh (n67) SN-1 Cretaceous time. rudists @247m (ra86) Sh “Ma” (ra79) marls in the Basrah area pass in southern Kuwait into white to grey dense Buzurgan-2 loc. loc. Dash-i-Gul continental clastics 32°N southern shelf of Tethys that spans 20Ma and containing about SHOALS Limestone apparently in limestone from 205- EKHAIDER Thin chalky marly microcrystalline limestone, which in places may contain grey chert carbonates Azraq 1 (PP1) HAMZA 15 phosphorite beds; deposition coincided with block-faulting, lacking orbitoids (ra78) 206m (ra86) LST & marl (n67) nodules. This calcareous facies has not always been distinguished fromBUZURGAN ZELOI KARUN loc. Fuluk 1 opening and/or rejuvenation of grabens (bk92). Eustatic B 7-2 the adjacent formations. Similar changes have been observed west of FQ-4 transgressions and regressions, accompanied by upwelling Ubaid-1; at Safawi-1, it appears that all the Shiranish marls have passed Buzurgan-4 Fuqo-1 Paydar-1 loc. Heavy Oil 2(W Rajil) episodes; phosphorites deposited during transgressions above Nukhaib Kifl-2 SHIRANISH FM. Low energy shallow Fine grained 9 into chalky and marly limestone within the Tayarat Formation (n67). Buzurgan-3 Bardi-i-Qamcheh Wadi Rijal 4 3 & 8 Risha 19 bioturbated hardgrounds (bk92). B 7-1 Nukhaib Kifl-3 Kumait-1 FQ-7 Gu(S78) Dopolanmarine Mine carbonates continental clastics Wadi Rijal 1 & 2 5 In this general area Field & Jones Dujaila-2 MASJID-I SULAIMAN loc. loc. loc. Heavy Oil 1(W Rajil) 15 Hamza 1, 10 & 12 Dark grey silty marly limestones and calcareous shale Najaf PAYDAR Kuh-e Gereh 7 2 assigned a minimum thickness of Ad Diwaniyah Rafidain-1 NOOR loc. Wadi Hazim 1 (ra86); fauna of very rare planktonic foraminifera KUMAIT Wadi Rajil 3 6 Thickness: At the type section, at least 30m 250’ (76m) for the incomplete Saderabad-1,2 loc. Wadi Ghadaf 2 Hamzeh 4 (Gansserina gansseri Bolli); with some bulloid forms Dujaila-1 Noor-1 PAR-E SIAH Bazan Pir & Ma’adn 14, 15 & 16 11 The formation has a total thickness of some 48m in the DUJAILA Outer ramp/ Coarse shallow Hamzeh 13 Turaif-1 Tayarat-Thoba area.At the type section, rubbly porous; Tayarat in this area (n67). (ra86); implies earliest Maastrichtian age (cc) RAFIDAIN Maidan-i-Naftun loc. loc. Wadi Ghadaf 1 white, buff and pink; rather chalky, fossiliferous, slope carbonatesloc. marine clastics Dahikiyeh 1 Rafedain East-1 AMARA recrystallised, dolomitised, locally sandy limestone, KH-4/1 HUWAIZA Mushtaq-1 loc. conspicuously more massive at the base. Garaf-2 Amara-1 NAFT SAFID Jalamia K 4/5 Adla 1 K 4/3 RAFIDAIN E. loc. loc. Garaf-1 HALFAYAH Tang-e Gel-e Tursh Shallow basinal/ FineArea shallow South of the Widyan and Kifl areas, Tayarat GARAF Hu-1 RAMIN loc. In the “Lower Campanian” (first cycle), Marbat Beds were Fm was found in all deep subsurface H-4 loc. Kuh-e Badmestanintrashelf basin carbonates marine clastics deposited in a continental (fluvial) environment over and to Halfayah-2 Kuh-e Manghast Qurayyat (Saudi) The Tayarat Limestones are porous and occupy an sections and in some of the shallow Halfayah-1 loc. the north of Ga’ara. To the south, reefal to back-reefal and T General thickening of the Composite column, E area NE of road Siwaqa 1 occasionally supratidal Hartha Formation was deposited above extensive area in Al Widyan. (mf38) stated that theis area Al Jandali structural holes in the southern desert west A Shiranish Fm to the NW SHIRANISH FM. loc. loc. loc. Clastic slope Cenomanian age rocks, to the S. of Rutba and on the W. side is an almost flat-lying Eocene and Cretaceous limestone YA RIFAEI loc. loc. Tang-e Tukab Kuh-e Baz Ta (mf58) of the River (n67). R Basinal marls and limestones loc. Deep basinal carbonatesloc. of the Ga’ara uplift (bk92). Marbat Beds interpreted as equivalent terrane that has very gentler slope and drainage toward Lussuf A (n67). Gu(B95) with turbidites to the top-Hartha Formation, as seen near the Semhat outcrops T water depths >200m. All deep AHWAZ HAFT KEL DOUDROU loc. KUH-E RIG the east. The annual rainfall averages less than 10mm, Macfadyen (1938) described this area as follows: “nearly S subsurface sections in the (bk92). HE loc. loc. loc. loc. and in summer and autumn this area constitutes the most the whole of the Wadian (Al Widyan) is covered with flat- LF Basrah area and Kuwait, loc. KUPAL loc. Wadi Sirhan 2 waterless part of Iraq. A very considerable proportion of lying limestones occasionally conglomeratic. These are MA between 276 and 137m SUSANGERD loc. Supratidal/sabkha loc. the rainfall probably percolates deep underground through believed to be wholly of Eocene and Cretaceous age. RG Ahvaz loc. loc. Clastic basinal Estaki Mine Ty 105m total (n67) IN Nasiriyah-1 loc. carbonatesSHURAM & evaporites (Abadeh) solution channels in the limestone, and the ground water Since the lithology is generally similar, and recognisable Sh 168m (n67) Top res @ 1992m loc. loc. K 4/7 NASIRIYA 40m pay, loc. loc. loc. is thus beyond the reach of shallow wells; however, deep fossils mostly leached out, the Eocene-Cretaceous Shoaling up: loc. Ahwaz-6 loc. drilled wells near the underground solution channels boundary appears to (be) unmappable without a great Umm Al Hashim Ø = 15% AB TEYMOUR loc. Wadi Sirhan 1 Dol over LST K = 143.5mD, MAJNOON Gu(B95) PARIS Restricted circulation L L “would probably yield water”. A detailed account of this expenditure of time and labour” (n67). (ja06) 20.4° API oil loc. loc. Kuh-e Hambast Ty Samawa-1 (n67) Exa Sh(sa00) Lacustrine subject was given by (mf38, p. 127-135). Carbonates(n67) ct p Majnoon-1 In the Basrah area the Tayarat Paris basinal carbonates L loc. Sh os Marly LST (sa00) loc. Kuh-e Bangestan-1 ition conformably overlies the Qurna MARUN loc. loc. loc. Badanah (Ar’ar)-1 Qasr Hamman of m loc. Argill LST ar Majnoon-3 Majnoon-4 formation, which is a globigerinal West Qurna-1 gin J-1 loc. loc. Nasiriyah re NW of Deh Bid Dol LST qu marl and marly limestone unit, Tang-e loc. Mixed carbonate- Wadi Sirhan 11 Wadi Sirhan 7 K 4/10 Ghalaisan-1 WEST QURNA ire Kuh-e Dinar Wadi Sirhan 10 s comparable with the upper parts loc. loc. loc. Sarvak Hiatus W.T. Foran (unpubl. data, 1940) described the Ty Dol Marl & shale mo M-2 loc. Wadi Sirhan 13 543-580m: Wackestone with foraminifera (fragmented in part), bryozoans, echinoids, and (n67) re of the Shiranish Formation, of clastic lagoon loc. Wadi Sirhan 5 composite Late Cretaceous section in the Widyan Diwan-1 Ty ca SHADEGUN KARANJ loc. Wadi Sirhan 6 Wadi Sirhan 12 some very fine microfossil debris. Rich foraminiferal fauna.(ra79). Top-Cretaceous @543m:; Sh marl & shale lib which it could be considered an loc. loc. Nazmabad West Qurna-15 ra loc. Area as follows (n67): Unconformity- especially in various lithologies including wackestone, packstone, grainstone, either partly recrystallised Ty 90m total (n67) Sh t outlying tongue (n67). loc. Wadi Sirhan 4 or partly or completely dolomitised, with no primary characteristics; some chalky and marly DIWAN In the deep subsurface sections of SW io NAHR UMR Agha Jari (field centre) Wadi Sirhan 8 Wadi Tibal region. Sh 137m total (n67) TAYARAT FM. n Massive subaqueous limestone, gypsum in porous fossil cavities in the upper part, slightly sandy in the lowermost Shabicha Iraq, the Tayrat Formation is generally Shelf carbonates loc. MANSURI KHALAFABAD AGHA JARI Ophiolite Wadi Sirhan 9 Limestone, purplish grey, fossiliferous, contains part (ra79). Most palaeontology has been ‘partially lost’ due to recrystallisation and/or sulphates Wadi Sirhan 3 overlain by the Umm er Radhuma Subba-2 Nahr Umr-8 loc. loc. Khaviz loc. loc. Wadi Sirhan 14 Loftusia; yellow marls locally passing to sandstone; dolomitisation (ra79) Nahr Umr-1,2,3 Formation (n67). Ur-1 SUBBA Rumaila N.-172 Ty Gu(B95) RAMSHIR loc. grey to white granular gastropodal limestones; and Fauna includes Omphalocyclus macroporous (Lamarck), Simplorbites gensacicus (Leymerie), Subba-5 Ta (lst/dol LST) RUMAILA Nahr Umr-7 Roshan Kuh (n67) approx 183m (n67) loc. loc. loc. soft yellow limestone, 27.2’ (8.3m) Clypeorbis mamillata (Schlumberger), Lepidorbitoides socialis (Leymerie), Lepidorbitoides Sh(marly lst/LST) NORTH loc. cf. minor (Schlumberger), Lepidorbitoides sp. (? cf. bisambergensis), Lepidorbitoides? - Dol SINDABAD PAZANAN GACHSARANMassive halite Volcanics Clyporbis?, Pseudoorbitoides??, Orbitoides media (d’Archiac), Orbitoides gr. tissoti, Wagsa Shawiya-1 Tayarat Fm. overlies Subba-4 RATAWI Sindabad-1 loc. Planorbulina cretace (Marsson), “Schlumbergerina”, Sulcoperculina ex. gr. dicksersoni Argill Dol P loc. Ratawi-3 Ratawi-1 r S-462 Sl. dolomitic/ Basra e loc. loc. (Palmer), Sulcoperculina sp., Gaudillaupidina sp., Rotalia sp., and other different very small Ty the Shiranish Fm. in C c loc. As-Sulaimaniyah (NW-44) Z-31 i rotalids. Beside these transported benthonic foraminifera, there are sparse pelagic fossls, Salman (n67) anhydrite Ratawi-6 Zubair-42 s loc. Subba-3 e loc. Sh & S Iraq (sa00) Rumaila N.-167 loc. Tang-e loc. loc. occasional globigerinoid forams, heterohelicids, “sphaera” etc., within the 544th metre, only S.85 Z-13 o (lst/dol LST) TUBA r loc. Gurguda one globotruncana is found: Globotruncana cf. bahijae Naggar. Finally, among the transported LST Ty Ty i (d59) T-3 (n67) e Siba-1 Rag-e Safid loc. fossils, some algae should be mentioned Permocalculus sp., Trinocladus sp. and Barbak ad Diud Subba-1 (marly lst/LST) TyT-2 Z-3 n Kuh-e Khami Marly LST Abu Ghar Qu Qu t Salpingoporella ubaiydhy n. sp. (type level at 578.8m). (ra79) TAYARAT KH 6a-8 a Tuba-1 t Fahliyan ZUBAIR i Abadan loc. loc. loc. Marl & shale Galaib Ganmi LUHAIS Luhais-1 RUMAILA Z-24 o loc. Kah-e Mish Lower/Middle Maastrichtian based on Globotruncana from 544m down, specifically Siba-2 n “The thickness of this (the Tayarat) formation varies Golden Staircase SURFACE GEOLOGYloc. FM. Luhais-12 Ty / RAG-E SAFID loc. loc. Jabal al-Qiyãl al-Kabir Globotruncana bahijae Naggar, which does not exceed (is not younger than) Middle DIBDIBBA (n67) p loc. S R-2 o between 300 and 900’, with a probable average of 500’. loc. loc. 30°N Suwayr Maastrichtian (ra79) Birjisiya Sh s Luhais-2 TAYARAT FM. i GARANGAN Barbak t In Zubair-3 reference section it is met between 4482 and BIBI HAKIMEH loc. H RACHI Dibdibbah-1 JEBEL Shelf carbonate io 30°N n loc. Murayr A Faid Az-Zahra Rachi-1: 970’ (thickest Ri-10 R-1 SANAM 5210’(1366 & 1586m)” (on58). SIAH MAKAN CHILINGAR Kahf-1 section) (296m) ABDALI loc. loc. Hudayb L A’a Faida Az-Zahra R. S.-72 In the Zubair-3 well, the Qurna Formation is overlain loc. Bussaya Jebel Sanam-1 loc. loc. Kahf-1 Sakakah L Dolomitic shelf top, cyclic, UBAID Jerishan-1RATQA by the Tayarat Formation, the contact being Hendijan Al-Laqit b/h Safawi-1 Ubaid-1 LST Ratchi Umm Qasr-1 loc. loc. O Abu Radham JRAISHAN 296m UMM conformable at the junction of dolomitic limestones loc. SULABEDAR Ty(sa96) with local sabkhas Anhy LST = thickest Tayarat Bikarz W Ty (n67) QASR above and globigerinal marls below. Reference loc. loc. Hamamiyat ST-8 approx 183m (n67) (alternations) Fm. in basin section Zubair-3, formation between 1586 to 1704m KILURKARIM loc. Dol BAHRGANSAR loc. loc. Zarqan Al-Jawf M Chabd Khider Alma-1 (118m thick). Aidah Anhy dol Ty BINAK RUDAK- Kuh-e Gadvan A (n67) loc. MILATUN Kuh-e Kalat Shiraz Basal LST Ty KHIDR AL MAA RAUDHATAIN Sh Binak Tarbur Dariyan/ loc. R (n67) SABRIYA loc. loc. Tuqaiyid w.w. Sh In the Burgan area, this formation has the loc. loc. loc. Kuh-e Gadvan I LST R-28 characteristics of a reef limestone and is loc. Dashtak-1 loc. N Tang-e Daneh Qumbari loc. Marl & shale MUTRIBA Bubaiyan-2 commonly highly porous, particularly at its loc. loc. GULKHARI loc. loc. E S. Shiraz In southwestern Iraq, with the exception of extreme Shiranish is (on58) Ba BAHRAH base, which commonly results in Kaneh Kat western region in the vicinity of Safawi-1, where thin in Rumaila Liyah-1 considerable drilling trouble due to loss of loc. loc. Ahmadi-1 C Dirah-1 NARGESI Sabzpushan-1 it is underlain by the Safawi anhydrites, this (n67) K-1 Bubaiyan-1 circulation or water flows (ingression? cc). loc. Note that much stratigraphy formerly referred to as ‘Early Kuh-e Mozzaferi loc. L (Owen and Nasr, 1958). loc. At-Tawil formation overlies the Shiranish Formation Bottea loc. Maastrichtian’ now falls into the Campanian following ICS 2004 A (formerly Qurna) conformably with lateral loc. S MEDINA loc. interdigitation (n67). KH 8a-9 T SARVESTAN loc. I KUWAIT loc. C MAGWA Kuwait City Kharg Island loc. Sefidar-1 loc. S loc. loc. loc. Ty ABU KHAIMA AHMADI RIQUA DARIUS-KHARG KH-6 (rh80) DHARIF loc. loc. Kuh-e Sah Qu Abu Khima-1 loc. loc. loc. CYRUS loc. ABDULIYAH loc. loc. BUSHGAN B-113 loc. Kulah Qasi MINAGISH DORRA loc. Bushehr In southern Iraq and in Kuwait the Tayarat is recognised as the loc. loc. loc. loc. uppermost unit of the Upper Cretaceous. In these areas according ESFANDIAR loc. loc. to (on58) the unit is: “essentially in the same facies as in the type BURGAN loc. loc. Naura-1 locality, .... it consists of brownish and dark grey granular loc. loc. Kuh-e Jahrum crystalline, dolomitic and sometimes anhydritic limestones and UMM GUDAIR loc. Dalan-1 loc. AGHAR AL HOUT loc. loc. whitish limestones interbedded with minor quantities of thin but loc. Kuh-e Siah-1 diagnostic black bituminous pyritic shales. The top of this loc. loc. loc. Aghar-1 loc. Kuh-e Surmeh SAUDI ARABIA formation has been taken at the top of the first black shale loc. FEREIDOON KUH-E KHAKI DALAN immediately below which the first Loftusia appear”. WAFRA loc. loc. loc. Qalibah-1 RIMTHAN loc. loc. loc. Cambridge (on58) mainatained that in the Basrah-Kuwait area this formation loc. KAFJI loc. loc. is thicker than the outcrop section (n67). loc. loc. loc. loc. Mand-4 Bandubast-1 The formation as a whole is of shallow-water deposition and DIBDIBA FUWARIS loc. loc. MAND is commonly highly porous (on58). The Gulf loc. loc. Tayma-1S MARJAN loc. KANGAN 28°N Turabah-1 loc. loc. loc. loc. loc. 28°N Al-Aqabah loc. loc. loc. P-5 Kuh-e Gel-e Siah SAFANIYA Kangan-1 P-1 P-4 loc. P-2 loc. Nar-1 Az-144 loc. PARS P-3 loc. loc. Baq’ah Ash Shuaibah loc. loc. loc. Az-24 Fb-1 NAR VARAVI loc. loc. Al-Mayyah MANIFA Iminoco-1 loc. Varavi-1 loc. loc. loc. Ha’il Az-274 loc. JURAYBIAT loc. loc. Al-Ajfar loc. 38°E 40°E 42°E Jal As-Saqiyah 44°E 46°E 48°E 50°E 52°E Qiba Kuh-e Dehnow/ Kuh-e Gavbust KHURSANIYA F-2 ABU HADRIYA Khursanyiyah-81 Berri-84 loc. Khursaniyah-8 BERRI Mudrraj Berri-84

Lavan-1 ABU SA’FAH Hunayzil FATHILI Abu Sa’fah-29