Carnets De Geologie最新文献_第10页

Revision of the Barrande's specimen "Tige d'une Cystidée indéterminée" (Cambrian, Echinodermata, Eocrinoidea) Barrande标本“未确定囊胚茎”（寒武纪、棘皮动物、Eocrinoidea）的修订

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-10-16 DOI: 10.4267/2042/62768

Martina Nohejlová, Oldřich Fatka

引用次数: 0

Atlas of Antarctic and sub-Antarctic Brachiopoda 南极和亚南极腕足纲图集

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-08-17 DOI: 10.4267/2042/62545

C. Emig

引用次数: 5

Brachiopodes actuels : historique et révision de la collection D.-P. Œhlert (Laval) ; brachiopodes des côtes françaises métropolitaines 当前腕足动物：D.-P.Œhlert收藏的历史和修订（拉瓦尔）；法国大都市海岸的腕足动物

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-07-07 DOI: 10.4267/2042/62544

F. Álvarez, C. Emig, J. Tréguier

引用次数: 4

New stratigraphic and genetic model for the dolomitic cretaceous pinda reservoirs in angola part I-the pinda of angola, an integrated lithostratigraphic approach 安哥拉白垩系品达白云岩储层的新地层学和成因模式——安哥拉品达:综合岩石地层学方法

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-06-25 DOI: 10.4267/2042/62283

B. Granier

{"title":"New stratigraphic and genetic model for the dolomitic cretaceous pinda reservoirs in angola part I-the pinda of angola, an integrated lithostratigraphic approach","authors":"B. Granier","doi":"10.4267/2042/62283","DOIUrl":"https://doi.org/10.4267/2042/62283","url":null,"abstract":"The Pinda Group of the Congo basin in the northern Angolan offshore is an overall transgressive supersequence of late Aptian - ? early Cenomanian age. Due to synsedimentary salt tectonics of the underlying Loeme Salt, the original ramp arrangement is split into discrete structures corresponding to many proven, probable and possible oil and gas plays. Where the biostratigraphic information was not destroyed by pervasive dolomitization, the little that remains is not available to the general public because it is treated as proprietary data by the Sociedade Nacional de Combustiveis de Angola Empresa Publica – Sonangol E.P. Only a limited set of data containing lithostratigraphic information (e.g., some published well logs and photomicrographs of facies) is available. The aim of this paper is to give a little more information about the Pinda stratigraphy. For instance, to be formally defined, this poorly known unit required a type section, a shortcoming that is addressed here. The wireline log signatures of some regional seismic markers are documented because they are used to correlate wells and subdivide the Group into formations. The microfacies corresponding to some key electrofacies as well as the porosity types are also condensed in a microphotograph catalog. Finally, few examples of typical LoC (i.e., Line of Correlation) diagrams are displayed and interpreted.","PeriodicalId":55273,"journal":{"name":"Carnets De Geologie","volume":"17 1","pages":"105-127"},"PeriodicalIF":1.4,"publicationDate":"2017-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46634836","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 3

Sedimentological investigation on Holocene deposits in the Mussafah channel (Abu Dhabi, United Arab Emirates) Mussafah海峡全新世沉积物的沉积学调查（阿拉伯联合酋长国阿布扎比）

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-06-25 DOI: 10.4267/2042/62267

B. Granier, R. Boichard

{"title":"Sedimentological investigation on Holocene deposits in the Mussafah channel (Abu Dhabi, United Arab Emirates)","authors":"B. Granier, R. Boichard","doi":"10.4267/2042/62267","DOIUrl":"https://doi.org/10.4267/2042/62267","url":null,"abstract":"Eight macrofacies types (5) plus subtypes (3) were identified while measuring sections along the Mussafah channel profile. These include: • aeolian sands, • microbial mat and microbial-laminated sediments, • gypsum and enterolithic anhydrite, i.e., a diagenetic variation of the previous facies, • muds with small pelecypods, and • its seagrass meadow version, • Potamid sands, and • its cemented version, i.e., the Potamid beach-rock, • washover fan coquina. A complete set of analyses, including granulometry, mineral composition, clay composition, TOC, and identification of the allochems and the microfossils, was performed on this material. The facies and their genetic setting, i.e., the sequence of facies, provide a perspective on both the environmental and stratigraphical significance of their distribution, both lateral and vertical, and an example of the application of the Walther's law. The lower microbial mat is the mark of a transgression whereas the upper microbial mat is the mark of a forced regression. In conclusion, the sequence of facies allows identification of the last Holocene transgressive-regressive cycle that includes a forced regression, which probably dates back to 6,000 years BP.","PeriodicalId":55273,"journal":{"name":"Carnets De Geologie","volume":"17 1","pages":"39-104"},"PeriodicalIF":1.4,"publicationDate":"2017-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.4267/2042/62267","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47571821","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 5

Review of the early Albian ammonites of the Montmell Formation near Marmellar (Salou-Garraf Basin, Tarragona, Catalonia, Spain) 西班牙塔拉戈纳salu - garraf盆地Marmellar附近montell组早期Albian菊石评述

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-03-24 DOI: 10.4267/2042/62038

J. Moreno-Bedmar, E. Robert, R. Matamales‐Andreu, T. Bover‐Arnal

引用次数: 6

Biostratigraphy and paleoenvironmental reconstruction of the marine lower Miocene Chechiș Formation in the Transylvanian Basin based on foraminiferal assemblages 基于有孔虫组合的特兰西瓦尼亚盆地下中新世海相契奇拉组生物地层学与古环境重建

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2017-03-24 DOI: 10.4267/2042/62041

S. Székely, Raluca Bindiu-Haitonic, S. Filipescu, Răzvan-Ionuț Bercea

{"title":"Biostratigraphy and paleoenvironmental reconstruction of the marine lower Miocene Chechiș Formation in the Transylvanian Basin based on foraminiferal assemblages","authors":"S. Székely, Raluca Bindiu-Haitonic, S. Filipescu, Răzvan-Ionuț Bercea","doi":"10.4267/2042/62041","DOIUrl":"https://doi.org/10.4267/2042/62041","url":null,"abstract":"Planktonic and benthic foraminiferal assemblages were used for biostratigraphy and paleoenvironmental reconstruction of the marine lower Miocene Chechiș Formation from the Gălpâia section (Sălaj county, Romania) in the northwestern Transylvanian Basin. Planktonic foraminifera suggest an Eggenburgian (Burdigalian) age for the deposits studied and reveal episodes of high primary productivity and mostly cool surface waters. Benthic foraminiferal assemblages indicate paleoenvironmental deepening from outer shelf to upper bathyal settings. Deltaic influences may be observed at the base of the studied section in outer shelf (possibly upper bathyal) environments with oxygenated bottom water and episodic high primary productivity, as a consequence of nutrient input from the land. Changes in paleobathymetry resulted in reduction of primary productivity. The benthic assemblages from the uppermost part of the section are dominated by tubular agglutinated foraminifera and indicate an upper bathyal setting with low organic flux to the sea floor. The sediments of the studied section were deposited during the late stage of the first early Miocene relative sea-level rise in the Transylvanian Basin.","PeriodicalId":55273,"journal":{"name":"Carnets De Geologie","volume":"17 1","pages":"11-37"},"PeriodicalIF":1.4,"publicationDate":"2017-03-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.4267/2042/62041","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44355736","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 11

Early Cretaceous Toxasterid Echinoid Heteraster from the high Zagros basin, south of Iran 伊朗南部高扎格罗斯盆地早白垩世弓形类棘类异长石

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2016-12-31 DOI: 10.4267/2042/61883

M. Yavari, M. Yazdi, Hormoz Gahalavand, H. K. Shadan, M. Adabi, L. Villier

引用次数: 5

On the type species of Lingularia, and description of Eolingularia n. gen. 论舌藻属的模式种，及舌藻属的描述。

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2016-12-12 DOI: 10.4267/2042/56006

M. Bitner, C. Emig

引用次数: 3

Évolution des séries silicoclastiques miocènes en Tunisie centrale : Cas de la coupe de Khechem El Artsouma 突尼斯中部中新世硅碎屑系列的演变:以Khechem El Artsouma杯为例

IF 1.4 4区地球科学

Carnets De Geologie Pub Date : 2016-12-12 DOI: 10.4267/2042/61846

Hanen Belghithi, F. Boulvain, C. Yaich, Anne-Sophie da Silva

{"title":"Évolution des séries silicoclastiques miocènes en Tunisie centrale : Cas de la coupe de Khechem El Artsouma","authors":"Hanen Belghithi, F. Boulvain, C. Yaich, Anne-Sophie da Silva","doi":"10.4267/2042/61846","DOIUrl":"https://doi.org/10.4267/2042/61846","url":null,"abstract":"En Tunisie, au cours du Miocene, suite a la phase de plissement NE-SW (direction atlasique), les depots silicoclastiques sont mis en place dans un environnement deltaique au sud-ouest et une plate-forme marine interne au nord-est du pays. Dans cet article, nous presentons la coupe de Kechem El Artsouma, du Miocene, qui est representative des depots de Tunisie centrale. Cette zone est particulierement interessante car elle correspond a la zone de transition entre les depots de delta et marins peu profonds. Nous proposons une combinaison de techniques telles que l'analyse des facies, la susceptibilite magnetique et la mesure de la teneur en carbonate pour ameliorer l'interpretation et la reconstruction des paleo-environnements et de leur evolution au cours du Miocene. Huit facies sont identifies, situes dans un domaine fluviatile, lagunaire et un domaine de plage. Les depots de la Formation Ain Grab (Langhien) sont interpretes comme deposes en phase transgressive, suivis par les depots de la Formation de Beglia (Serravallien) en phase regressive. La Formation de Saouaf (Serravallien-Tortonien inferieur) correspond a une phase transgressive et regressive. La coupe Kechem El Artsouma permet de proposer un modele sedimentaire pour les depots du Miocene de la zone de transition en Tunisie centrale.","PeriodicalId":55273,"journal":{"name":"Carnets De Geologie","volume":"16 1","pages":"557-568"},"PeriodicalIF":1.4,"publicationDate":"2016-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.4267/2042/61846","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70514122","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 2