Iraqi National Journal of Earth Sciences最新文献

{"title":"Effect of Water Content on Brightness Temperature and Emissivity of Soil for Passive Remote Sensing Applications","authors":"Falih A. Aziz","doi":"10.33899/earth.2014.87473","DOIUrl":"https://doi.org/10.33899/earth.2014.87473","url":null,"abstract":"","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"77 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2014-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121469806","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Hydrochemistry of Tigris River Water from its Iraqi‘s Territory Entry to Baghdad city","authors":"Hisham Yahya Dhannoun, Hazim Jumaa Mahmood","doi":"10.33899/earth.2014.87490","DOIUrl":"https://doi.org/10.33899/earth.2014.87490","url":null,"abstract":"","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"12 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2014-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121507207","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Porosity of Avanah Formation and its Stratigraphical Distribution in Selected Wells of Kirkuk Oil Field","authors":"Mohammed A. M. Sulaiman, Abdalaziz M. AL-Hamdany","doi":"10.33899/earth.2014.87488","DOIUrl":"https://doi.org/10.33899/earth.2014.87488","url":null,"abstract":"","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"85 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2014-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114774102","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Palynostratigraphy, Age determination and Paleoecology of Butmah Formation in borehole Kand-1 Northern Iraq","authors":"Yasser H. Kddo, Amer D. Nader","doi":"10.33899/earth.2014.87486","DOIUrl":"https://doi.org/10.33899/earth.2014.87486","url":null,"abstract":"Eight samples (K1-K8) from borehole Kand-1 covering (190) meters thick stratigraphic section were palynologically studied. They yield (36) species of sporomorphs belonging to (24) genera, three species were expected to be new. The miospore species recoved in this study indicate late Triassic age (Norian) and characterized by the dominance of many species of bisaccate non-striate pollen such as: Alisporites australis, A. dunrobinensis, warepanus, Falcisporites tecovasensis, Pityosporites scaurus, Protodiploxypinus acutus, P. americus, Samaropollenites speciosus. In addition to monosaccate (Vesicate sporomorphs) represented by: Patinasporites densus, Vallasporites ignacii, Enzonalasporites vigens. The dominance of monosaccate pollen grains and the presence of the acritarchs, foraminiferal lining (acid-resistant inner coat) and fresh water algae in the lower part of stratigaphic section (K1-K3) indicate deposition in lagoonal environment with relatively high salinity and little supplies of fresh water. The increase of bisaccate pollen grains in the upper part of the sections (K4-K8) indicate deposition in relatively deeper environments (Inner shelf environment). Key Word: Palynostratigraphy, Age determination, Butmah Formation, Kand-1, Iraq. ـــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ ـــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ ةمدقملا دــنق رــئب رــفح 4 قرــش لامــش عــقي يذــلا دــنق لــبج ةــقطنم يــف ي ــعبتو قا رــعلا ( ةــسا ردلا ةــقطنم د 00 مــك ) لامش ي لصوملا ةنيدم ( لا لكش 4 ) . :رئبلا تايثادحأ ضرع طخ (36o 39' 53\") لًاامش لوط طخو ) ( 43o 01' 37\" ش ًاقر ، امأ جذامنلا ( نيب ةروصحملا قامعلأا نم تناك رئبلا اذى يف ةسا ردلا ضرغل تذخأ يتلا 1640 0400 يـتلاو ا رتم ) ينيج ةرـق نيوكت لثمت (Kurrah Chine Fn.) ةمطب نيوكتو (Butmah Fn.) ادانتسا ىلإ رئب يف ةمطب نيوكتل ةميدقلا ةئيبلاو رمعلا ديدحت و ةيجولونيلابلا ةيقابطلا ...................... 02 (Bellen et al., 1959) نيوكتو ةمطب طقف ثيدحلا تاسا ردلا ىلإ ادانتسا ة اينمو تافاشكتسلاا ةكرش ةسا رد ةيطفنلا (BP and idemitsu, 1990) ،نورخآو ناسرخلا( ةيطفنلا تافاشكتسلاا ةسا ردو 4664 .) :ةمطب نيوكت ةرم لوأ نيوكتلا فصو لبق نم (Dunnigton, 1953 in Bellen et al., 1959) رئب عطقم يف ةمطب 1 برغ لامش ي لصوملا ةنيدم نم ددعب قرتخأ نكلو حطسلا ىمع فشكني لا نيوكتلا اذى نلأ لابجلا مادقأ ةقطنم يف رابلآا (Foot hill) . امأ نيوكتلا ةيراخص ييف ةسناجتم ريغ وعطقم نوكتيو ءا زجأ ةثلاث نم يجذومنلا (Jassium and Goff, 2006) :يى لفسلأا ءزجلا ( كمسب 410 فصت عم يريجلا رجحلا نم نوكتي اً رتم ) تيا ردياينلاا نم تاقبطو ةيميجس تاح . طسولأا ءزجلا ( كمسب 450 ًا رتم ) يـممر ميزـمو يتياـمولود رـجحو بذاك يئرسو يئرس يريج رجح نم نوكتيف .ليجسلا نم تاقبط عم ءا زجلأا ضعب يف وززمعلا ءزززجلا ( كمــسب نيوــكتلا نــم 100 يرــيج رــجحو بذاــك يئرــس و يئرــس يرــيج رــجح نــم فلمــتي اً رــتم ) تيامولود .تيا ردياينلإاو ليجسلا نم تلاخادت عم ي قفاوت حطس وى نيوكتمل يمفسلا سامتلا حطس نإ (Conformable) يطومب نيوكت عم مت يذلا( اغلإ ؤ نيج هرق نيوكت نم يومعلا ءزجلاو وى فيضأو اًنيوكت هرابتعاب","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"19 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2014-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123040277","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Two New Miospores Species from Triassic-Jurassic Boundary in Borehole Tel Hajar-1 South West Mosul City, Iraq","authors":"Yasser H. Kddo, Amer D. Nader","doi":"10.33899/earth.2012.64531","DOIUrl":"https://doi.org/10.33899/earth.2012.64531","url":null,"abstract":"Two new species of miospores are described from Upper TriassicLower Jurassic Butmah Formation in borehole Tel-Hajar-1northern Iraq. These are Concavisporites baăjensis sp.nov. and Concavisporites mosulensis sp. nov. ـــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ ـــــــــــــــــــــــــــ دیدج نیعون ةسارد ی افلا دحلا نم تراوبسلا نم ن يسایا رتلا نیب لص يسا روجلا لت رئب يف رجح ١ قا رعلا لامش لصوملا ةنیدم برغ بونج ردان دؤاد رماع ودق نسح رسای ضرلأا مولع مسق مولعلا ةیلك لصوملا ةعماج صخلملا فصو مت سلا نم تاحتفلا ةیثلاثلا تا روبسلا نم نیدیدج نیعون يسایا رتلا نیب لصافلا حط يسراوجلاو رجح لت رئب يف ةمطب نیوكت نم ١ امه ناعونلا ناذهو قا رعلا لامش : Concavisporites baăjensis sp. nov. and Concavisporites mosulensis sp. nov. ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ INTRODUCTION During the course of detailed palynological studies of Triassic and Jurassic strata of Butmah Formation in borehole Tel-Hajar-1 (41o 40' 20\" L , 35o 50'40\" W) south west Mosul city, Iraq. Two morphologically distinctive species of dispersed trilete spores have been encountered.Tel-Hajar-1 well was drilled on the Tel-Hajar structure which is located 30 Km. southwest of Sinjar town (Fig.1). The purpose of this paper Amer D. Nader and Yasser H. Kddo 80 is to document these species systematically and to relate their occurrence to the palynostratigraphic sequences. STRATIGRAPHY The studied samples represent part of Butmah Formation which is penetrated in borehole Tel-Hajar-1. The Butmah Formation was first described by (Dunnington 1953 in Bellen et al., 1959) from borehole Butmah -2 south west Mosul city (Since Butmah Formation is not recognized in surface exposures). The formation is a heterogeneous aggregate of sediment of calcareous argillaceous and evaporitic rock suites (Fig. 2). According to (Jassium and Goff, 2006) the upper (200m.) of the Butmah Formation in the type section consist of oolitic and detrital limestone with beds of argillaceous limestone, shale and anhydrites. The middle part (180m.) is oolitic, argillaceous and dolomitic with sandstone and shale bed. The lower part (120m.) is composed of limestone with bedded anhydrite.The lithofacies and faunal assemblages indicate that Butmah Formation was deposited in shallow water lagoonal and sabkha environment. Two New Miospores Species from Triassic-Jurassic.................. 81 Fig. 2: Stratigraphic Succession, Sample Position and Range of the New Species in Borehole Tel-Hajar-1 (Kddo, 2011). Amer D. Nader and Yasser H. Kddo 82 SYSTEMATIC PALAEONTOLOGY Anteturma: PROXIMEGERMINANTES Potoniè, 1970. Turma: TRILETES Reinsch emend. Dettmann, 1963. Suprasubturma: ACAVATITRILETES Dettmann, 1963. Subturma: AZONOTRILETES Luber emend. Dettmann, 1963. Infraturma: LAEVIGATI Bennie and Kidston emend. Potoniè, 1956. Genus: Concavisporites Pflug in Thoms","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"12 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122885189","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The Preparation of an Electronic Map for the Development of Wadi AL-shour Basin Valley North Eastern Mosul City Using Geographic Information System (GIS)","authors":"Bashar M. Yahya, Basman Y. Hameed","doi":"10.33899/earth.2012.64439","DOIUrl":"https://doi.org/10.33899/earth.2012.64439","url":null,"abstract":"The study area is within Wadi AL-Shour basin north eastern mosul city. This work includes the hydrological development of the basin and the preparation of an electronic map based on remote sensing technique. The technique is considered a ىیحی رینم راشب و دیمح سنوی نامسب ٢ very active tool for the determination of the surface drainage system, analysis of the morphomatric features of the basin and the study of the hydrological balance of the basin. It has also been used for the determination of input and output flow of basin waters, the suitability of the well waters for drinking and agricultural purposes and the improvement of the productivity of the basin through the design of a harvesting method for rain waters at the study area. The collected data is processed by the use of (GIS) software and the results obtained are gathered in a main data base as a digital layers, loading to the preparation of a purpose electronic map which could be used for the monitoring and developing the study area. ــ ـــــــــــــــــــــــــــــــــــــــــــــ ةمدقملا رصحنیو لصوملا ةنیدم قرش دیدحتلابو قا رعلا نم يقرشلا يلامشلا ءزجلا يف روشلا يداو ضوح عقی ةلجد رهن يف ضوحلا بصیو ةقیشعب ةیطو ةرفصلا نیع ةیط نیب . ضرع يطخ نیب ةسا ردلا ةقطنم ددحتت ) ١٥ ̋ ١٥ ́ ٣٦ ° ، ٠٠ ̋ ٢٨ ́ ٣٦ ° ( و اقرش ) ٠٠ ̋ ٢٠ ́ ٤٣ ° ، ١٥ ̋ ٣٠ ́ ٤٣ ° ( لاامش . ةیلكلا ضوحلا ةحاسم غلبت ) ٣٠٨.٤ ( لصوم قیرط ربع هیلإ لوصولا نكمیو عبرم رتمولیك وأ ةرقع لصوم قیرط لیبرا ) لكشلا ١ .( رحبلا خانم يلاتلابو قا رعلا خانم فورظل ةسا ردلا ةقطنم خانم عضخی طسوتملا . نایبلا ىلع لوصحلا مت ماع نم ةرتفللو لصوملا ءاونأ ةطحم نم ةیخانملا تا ١٩٨٠ ماع ةیاغلو ٢٠١٠ يرطملا طقاسلا لدعم غلب ثیح ) ٣٩٧ ( ةرا رجلا تاجرد لدعمو ملم ) ٢٤ ( رخبتلا لدعمو ةیوئم ةجرد ) ٩٠.٩ ( ملم . نإ تززع يئاملا زجعلا ةلكشم ةیمهأ يدجلا ریكفتلا ةرادإب ریوطتو ةنایصو ضاوحلأا نع ةیرهنلا رط ةیوعرلاو ةیعا رزلا ةیمنتلا تاعورشمو ةیئاملا رداصملا ةیمنت قی ) ،يروبجلا ٢٠٠٩ .( نم ةیفوجلا هایملا دعت اهتایمك ةفرعم يرورضلا نم ناف اذل ةیجولوردیهلا ةرودلا نم ءزج يهو ةعیبطلا يف هایملل ةمهملا رداصملا ولوردیهلا ةنزاوملا ةسا رد قیرط نع كلذو اهتدایز ىلع لمعلا ةیفیكو ةیج ل ضاوحلأ ةیرهنلا ) يمیعنلأ ، ٢٠٠٠ .( بسح ةسا ردلا ةقطنم يف ةیفوجلا هایملا فینصت مت ) ،لیئا ربج ١٩٧٣ ( نمض ةسا ردلا ةقطنم عقت ثیح عاطقلا ) B2 ( ةدیج اهنأب فصوت هایملا ةیعونو ةریغتم ةیجاتنإ تاذو سرافلا نیوكت وه يجولویجلا نیوكتلاو یذغتلاو لیلق نزخلا لماعمو ةئیدر ىلإ ةریغتم ة . نم نوكت ةسا ردلا ةقطنم يف ةیفوجلا هایملا ةكرح نأ املع تاقبط عافترا نم جتانلا يكیلوردیهلا طغضلا ببسب ةلجد رهن هاجتاب يأ يبرغلا بونجلا ىلإ يقرشلا لامشلا ةقیشعبو ةرفصلا نیع يف لابجلا مادقأ دنع يئاملا نیوكتلا . ل ةنزاخلاو ةلماحلا ةیئاملا تانیوكتلا فصتت ةیفوجلا هایمل اهنأب ةروصحم ریغ ةیئام تانیوكت ةلثمتملاو ب ثیح ةحتفلاو ةناجنلاا نیوكت نأ ردصملا يساسلأا ه ةیذغتل يونسلا يرطملا طقاسلا هایم امه نینیوكتلا نیذ اهنمو ةثیدحلا تابسرتلا ربع برستت يتلاو ةرفصلا نیعو ةقیشعب ةیطب ةلثمتملا تاعفترملا ىلع طقسی يذلا ةنیدم قرش لامش روشلا يداو ضوح ریوطتل ةینورتكلا ةطراخ دادعإ ................. ٣ ذفنت لإ ى كمسبو يسیئرلا نزاخلا ةناجنلاا نیوكت ربتعی ثیح ةحتفلاو ةناجنلاا ينی","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"117 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130440610","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Diagenesis of Khurmala Formation in Dokan Area, North Eastern Iraq","authors":"Safwan F. Al-Lihaibi","doi":"10.33899/earth.2012.64507","DOIUrl":"https://doi.org/10.33899/earth.2012.64507","url":null,"abstract":"Diagenesis were studied within Khurmala limestone Formation at Dokan area, Northeastern Iraq. The study recognized many diagenetic processes affected limestone within a successive sequence including micrite envelope, dolomitization, dissolution, neomorphism, cementation, mechanical and chemical compaction. The study determined four diagenetic zones. They are marine zone يبیهللا يحتف ناوفص ١٨ (micrite envelope), mixing zone (dolomitization), meteoric pheratic zone (dissolution, neomorphism, cementation) and burial zone (mechanical and chemical compaction). According to the history of diagenesis and their sequence, the study revealed that periodical fluctuation in sea level has influenced on diagenetic processes and their paragenetic sequence. ـــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ ــــــــــــــــــــــــــــــــــــ ــــــــــ ــــــــــــــــــ ةمدقملا يف ةینامیلسلا ةنیدم برغ لامش ناكود ءاضق يف ةلامروخ نیوكت اهیف فشكنی يتلا ةسا ردلا ةقطنم عقت قرش لامش ي قا رعلا ، ةـیلاعلا تاـیطلا قاـطن نمـض ) لكـشلا 1 ( ، ةـلامروخ نیوـكت فـصو دـقو ) (Khurmala Formation Paleocene-L.Eocene) ( لولأ نـلب لبق نم ةرم ) Bellen ( ماـع ) 1953 ( كوـكرك رـئب يـف _ 114 كمـسبو 185 رـتم ) Bellen et. al., 1959 .( یو رـهظ نیوـكت ةـسا ردلا ةـقطنم يـف ةـلامروخ كمـسب غــــــــــ ـــــــــ ـــلبی ) 120 ( ًاــــــــــ ـــــــــ ـــبیرقت رــــــــــ ـــــــــ ـــتم ، نوـــــــــــ ـــــــــ ــكیو شوـــــــــــ ـــــــــ ــ لوك نیوـــــــــــ ـــــــــ ــكت ىــــــــــ ـــــــــ ـــلعا عــــــــــ ـــــــــ ـــم لاًخادــــــ ـــــــــ ـــــــتم ) Kolosh Formation ( ، ظ ددـحی ذا تاــقبط عــم بـقاعتت يــتلا بلــصلا يرــیجلا رــجحلا نـم تاــقبطب هروــه وـسلأا لـفطلا شوـلوك نیوــكتل ةدـئاعلا يداـمرلاو د ، جلا رـجحلا تاـقبط كمـس دادزـی مـث تاــقبط روـهظ لـقیو يرـی دوسلأا لفطلا ، لاو يلراملا يریجلا رجحلا روخصو تملدتملا يریجلا رجحلا روخص ىلإ بقاعتلا ریغتیو لـفط يف نوللا ينبلا نیوكتلا ىلعا ، سكرـج نیوـكت عـم يجیردـتو قـفاوتم وـهف نیوـكتلل يوـلعلا دـحلا اـما ) Gercus Formation ( ) لكـشلا 2 ( . سرد دـقلو ) Al-Qayim et. al., 1993 ( رـصعل ةدـئاعلا تاـبقاعتلا ةـیقابط ناطلــس ةــبیه ةــقطنم يــف نیجویلاــبلا _ قا رــعلا قرــش لامــش ، يـــه ةــیتانوبراكلا تاــبقاعتلا كــلت نا اوــنیبو تاذ ةــــــــــ ـینوكلا ةـــــــــــعیبط راجنـــــــــــس نیوـــــــــــكت ىــــــــــ ـلا سیـــــــ ــــلو ةـــــــــــ لامروخ نیوـــــــــــكت ىــــــــــ ـلا ةدــــ ـــــــئاع يــــــ ـــــهو ةـــــــــــ یدم ) Sinjar ormation ( . سرد اــمك ) Al-Qayim, 1995 ( ةــلامروخ نیوــكتل ةیبوــسرلا تانحــسلا لامــش يــف ةراــتخم عطاــقم يــف قا رعلا ، دجوو اذه نا نیینحـس نیما زـح نمض بسرت نیوكتلا ، ـینوكلالا تانحـسلا ما زـح وـه لولاا وـه يناـثلاو ة دملا تاحطسم تانحس ما زح . سرد دقو ) نورخاو يدیمحلا ، (2011 اوزـیمو ناكود ةقطنم يف ةلامروخ نیوكت ةقیقد ةیسیئر تانحس ةسمخ يهو : ينیطلا يریجلا رجحلا ةنحس و يكاولا يریجلا رجحلا ةنحس و رجحلا ةنحس صوــصرملا يرــیجلا و جلا رــجحلا ةنحــس ـــ ـ يــبیبحلا يری و رــجحلا ةنحــس ــیجلا طبا رــتملا ير نیوــكتلا نا اوجتنتــساو و ةـیئیب هقطنا ةثلاث يف","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"4 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115728862","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Foraminiferal Biostratigraphy of Bekhme Formation (Late Campanian) in Dohuk Area/ Northern Iraq","authors":"Layla Y. Al-Haidary, Majid M. Al-Mutwali","doi":"10.33899/earth.2012.64525","DOIUrl":"https://doi.org/10.33899/earth.2012.64525","url":null,"abstract":"","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"39 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127462612","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Transversopontis omarians sp.nov. Calcareous Nannofossils from Jaddala Formation (Eocene) in Dh.1 well, central Iraq","authors":"Mohammad H. Al-Ubaidi, Omar A. Al-Badrani","doi":"10.33899/earth.2012.64530","DOIUrl":"https://doi.org/10.33899/earth.2012.64530","url":null,"abstract":"ABSITRACT Transversopontis omarians sp.nov. is described from Jaddala Formation (Eocene) in Dh.1well, central Iraq. This species is recognized by having elliptical muroliths with transverse bar lacking two openings in the ends of the central area, it is reaching about 10 microns in length. ــــــــــــــــــــــــــــــــــــ ـ ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ عونلا Transversopontis omarians sp.nov. نم نم ةیسلكلا ونانلا تا رجحتم ةلادج نیوكت ) نیسویلاا ( ةیرفظ رئب يف ١ قا رعلا طسو","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"86 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114453673","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Systematic Studies on some Middle Eocene Calcareous Nannofossils / Northern Iraq","authors":"Ali H. Elewi","doi":"10.33899/earth.2012.64519","DOIUrl":"https://doi.org/10.33899/earth.2012.64519","url":null,"abstract":"","PeriodicalId":371191,"journal":{"name":"Iraqi National Journal of Earth Sciences","volume":"42 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134088473","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}