bluuebunny/crossref_metadata_2025_split huggingface dataset:
Charles Jacob, 19 fevrier 1878-13 aout 1962
Authors: Casteras Marcel , Laffitte Robert 
Published: March 2020

Abstract
From 1928 to 1950 Charles Francois Etienne Jacob was the chairman of geology of the Faculty of Sciences of the Sorbonne. His contributions to geology were chiefly to knowledge of the structural geology of France, northern Indochina and the Pyrenees, and the paleontology and stratigraphy of the middle Cretaceous of the Alps. A bibliography of his publications is given.
Etude geologique de la region de Barcis (Alpes meridionales, province d'Udine, Italie)
Authors: Saint-Marc Pierre 
Published: March 2020

Abstract
Triassic to middle Miocene rocks make up the Venetian Prealps sequence in the Barcis region (Udine province, Italy). The thick sediments belong to the eastern border of the Friuli zone. Shallow water limestones deposited from the Liassic through the Dogger were succeeded by reef limestones from the Malm to Cretaceous. The limestones are covered by Eocene flysch. ESE to WNW ripple marks and a later occurrence for the flysch on the west side of the area indicate an eastern source for the flysch deposits. Miocene sediments contain glauconite and littoral fauna. Major tectonics in the area are believed to be post-Miocene.
Les eclogites et leurs transformations au milieu des gneiss du massif de Snieznik dans les Sudetes
Authors: Smulikowski Kazimierz 
Published: March 2020

Abstract
The Snieznik eclogites of Poland are intercalated with a migmatitic gneiss and form a lithologic series differentiated by the ratio of omphacite to carinthine. They range from the common eclogites without primary amphibole to rocks rich in carinthine. The latter cannot be designated as a true eclogite for they contain no omphacite and should be placed above the sequence. Several successive stages of amphibolitization are apparent. They are the individualization of a purer common secondary hornblende and of an acidic plagioclase, ending in ordinary amphiboles. These rocks were then affected by a potassium-type metasomatism on a regional scale which was responsible for the granitization and migmatization of the surrounding gneiss and culminated the metamorphic evolution of the lithologic unit.
Le Pliocene et les accidents periglaciaires de la plage de la Mine d'Or a Penestin (Morbihan)
Authors: Riviere A. , Vernhet S. , Arbey F. , Desprairies Alain 
Published: March 2020

Abstract
Detailed study of the cliffs along the Mine d'Or coast provides results which indicate that two Pliocene stratigraphic sequences are separated by a period of emergence or semi-emergence locally evidenced by a slight unconformity and the presence of a ferruginous layer at certain points. Examination of the evidence of tectonic deformation confirms the existence of slight recent activity. Quaternary frost action, in areas where the arenaceous basement rock has been replaced by a white plastic clay, produced cryoturbation phenomena analogous to Recent pingos of the polar regions. Their morphology indicates that there were two successive glacial phases. The ferruginous crust observed at the base of and between the two Pliocene sequences is formed today in the present climate and under geologic conditions similar to those which existed during the Pliocene.
Observations nouvelles sur la stratigraphie du Jurassique de la region de Kandreho (Madagascar)
Authors: Blaison Jean 
Published: March 2020

Abstract
The cuestas along the Ikahavo coast, north of Tsilanarano, are designated as the type section for the Madagascar Jurassic. The transgressive marine Toarcian overlies the Isalo sandstone unconformably and is more extensive than previously thought. The thickness of the Aalenian is decreased due to the increased importance of the Toarcian. The Bathonian was located more to the north at Beranonorambe. Three ammonite species are described, Phymatoceras collignoni n. sp. (middle Toarcian), Sonninia (Sherbonites) aff. adicra, and Micromphalites (?) sp. (middle-upper Bathonian). Astarte baueri n. sp. is described from the Bouleiceras-Protogrammoceras zone.
Interpretation d'une succession interessant la limite oligo-miocene dans le sud du Bordelais
Authors: Caralp Michelle , Moyes Jean , Puechmaille Chantal , Vigneaux Michel 
Published: March 2020

Abstract
A core drilled at Salles, southwest of Bordeaux (France), yielded a section of strata which embraces the Oligocene-Miocene boundary. The beds are principally limestones with a predominance of carbonates in opposition to small amounts of detrital elements. On the basis of the frequency of the fauna included in the limestones three sedimentary zones are distinguished. The basal zone contains allochemical components suggesting calm sedimentation and includes nummulites and abundant melobesiids. The intermediate zone has faunal and lithologic characteristics of both the underlying and overlying zones. In the upper zone Miogypsinoides fades out and glauconite and pyrite appear. Examination of the foraminifera and ostracod microfaunas reveals three biozones which correspond to the sedimentary zones. Two tables give the distribution of the principal foraminifera and ostracod species. The type of sediments and the distribution of the microfaunas indicate that the basal zone is Oligocene, the upper zone is Miocene and the intermediate zone marks the top of the Oligocene.
Sur la stratigraphie et la paleogeographie du Frioul occidental: Le Val Cellina (Alpes meridionales, Udine, Italie)
Authors: Cousin Michel 
Published: March 2020

Abstract
The Jurassic, Cretaceous, and Eocene beds cropping out on the northern and southern flanks of the Claut syncline are compared and contrasted with the Barcis series to the south. Description of six sections reveals the dissimilarity of the facies and thicknesses between the northern and southern flank beds. From north to south the passage from reefal to pelagic sedimentation can be observed, accompanied by an increase in the thickness of the series. During the Malm a reef zone SW of Barcis was oriented SSW-NNE. Red nodular limestones, characteristic of a pelagic shoal, were deposited during the Kimmeridgian and Tithonian. The reef zone persisted throughout the lower Cretaceous depositing microbreccias on its NW flank. The reef zone is recognized in the upper Cretaceous of the Claut syncline. Terrigenous deposits of Scaglia (upper Campanian-Maestrichtian) and sandy marls (Danian-lower Paleocene) represent the subflysch of Vassoevitch. True flysch is recognized in the Paleocene and Eocene and is homogeneous throughout the Val Cellina with no positive relationship with the Malm and Cretaceous limestone series. The flysch is progressively younger from north to south.
Sur une nouvelle espece de Thecideidae, Glazewskia sp. (Brachiopode) du Jurassique de Podolie
Authors: Glazewski Konstanky , Pajaud Daniel 
Published: March 2020

Abstract
A new species of brachiopod, Glazewskia sp., is described from the top of a bed of Jurassic marl in the Dnestr river valley near Bukovna, Podolia plateau, southwestern USSR. The mode of development of the brachial septae is unusually well shown.
Influence de la tectonique du Pays de Bray sur les formations paleogenes au voisinage de sa terminaison orientale
Authors: Blondeau A. , Cavelier Claude , Pomerol Charles 
Published: March 2020

Abstract
Major facies changes in the Paleogene formations at the southeast end of the Pays de Bray anticline of the Paris basin, in the vicinity of Beaumont-sur-Oise, date tectonic movements and periods of remission during the Paleogene. Although the anticline developed during the late Cretaceous, it seems to have had no significant effect upon sedimentation until its emergence and the concurrent establishment of continental sedimentation in the upper Thanetian (lower Eocene). Tectonic activity occurred again in the lower Sparnacian and the upper Cuisian (lower Eocene), the lower and the upper Lutetian (middle Eocene), the Ledian (lower Priabonian: upper Eocene), the Ludian (upper Priabonian: upper Eocene), and the lower Stampian (middle Oligocene).
Donnees micropaleontologiques sur les couches inferieures du flysch dans le Val Cellina (Alpes meridionales, Udine, Italie)
Authors: Marie Pierre , Cousin Michel 
Published: March 2020

Abstract
The Maestrichtian to Paleocene microfauna of the lower flysch beds of the Cellina valley in the Carnic Prealps of northern Italy is similar to that of a nearby area. The microfauna, especially of the upper beds, is described.
Observations nouvelles sur le passage du Cambrien a l'Ordovicien dans la Montagne-Noire
Authors: Boyer Francois , Guiraud Rene 
Published: March 2020

Abstract
Recent discovery of fossiliferous horizons in the Cambro-Ordovician shale-sandstone series of Montagne-Noire in southern France indicates a stratigraphic discontinuity involving thinning or possible absence of the upper Cambrian under transgressive lower Ordovician. It is not known whether the upper Cambrian was not deposited, or was eroded prior to the Ordovician deposition.
Phases terminales et tectogenese de la montagne Sainte-Victoire
Authors: Touraine Fernand 
Published: March 2020

Abstract
Sainte-Victoire mountain has been considered as the eroded remnant of a massif whose first signs are known from the upper Cretaceous but which was actually emplaced during the lower Eocene. Three studies of the area have shown that the basic structure, but not the relief, was formed in the Eocene; intense erosion in the Oligocene and Miocene peneplaned the area. In a post-Tortonian phase the structure was uplifted and acquired its present morphology. The uplift is limited on the west by a fault at the foot of the Bau-Roux plateau; the eastern limit is the Delubre fault. The tectonic history of the area developed in seven phases and interphases from the upper Cretaceous to the post-Tortonian.
Observations nouvelles sur la flore de charophytes du Stampien du bassin de Paris
Authors: Grambast Louis , Paul Philippe 
Published: March 2020

Abstract
Seventy charophyte species, three of which are new, are described from marls associated with Etampes limestones near Fontainebleau and Soisy-sur-Ecole (Seine-et-Marne, France). Two other species are recorded for the first time from the Paris basin. The age of these beds, based on the new charophytes, is Stampian (Tertiary).
Etude sedimentologique des principaux facies du Turonien de Touraine
Authors: Riveline-Bauer Janine 
Published: March 2020

Abstract
Outcrops and cores in Touraine, France, have exposed lower Turonian (or Salmurian) and upper Turonian (or Angoumian) facies which contain varying amounts of detrital minerals, carbonates, and silica, the latter represented partly by opal-cristobalite. The facies include tuffs, shelly sand, spongolite, and chalk. The clay mineralogy of kaolinite in the upper Turonian chalk facies suggests an origin from a kaolinite deposit or from a mixture of montmorillonite, illite, and kaolinite. The study reveals an increase of carbonates and silica in the lower Turonian from northwest to southeast accompanied by a decrease in detrital material.
Extraction des fractions granulometriques d'un sediment par elutriation, et utilisation de ces fractions pour l'etablissement de diagrammes de distribution du calcaire
Authors: Casta Lucien 
Published: March 2020

Abstract
Granulometric fractions are obtained from the fine portion of loose sediment isolated in the center of the Bahco elutriator-centrifuge. The possibility of using this method for obtaining each granulometric fraction separately would permit comparison between them. These fractions can be used to plot limestone distribution as a function of the diameter of the particles.
Observations sur la mise en place du granite de Saint-Guiral-Liron (Cevennes meridionales)
Authors: Prager Michel 
Published: March 2020

Abstract
The Saint-Guiral-Liron granite consists of a porphyritic granodiorite intruded into folded Paleozoic schists of the Cevennes mountains to the north and the Vigan nappe area to the south. The composition of the granodiorite is homogeneous and nearly isotropic. Metamorphism at the northern border of the granodiorite resulted in the formation of gneiss, and at the southern border, of flint. The southern contact indicates extremely intense emplacement with development of an aureole of exothermal contact metamorphism. The joint systems of the northern and southern borders are described and interpreted.
Esquisse geologique du prolongement nord du granite de Saint-Maurice-Chateauneuf (Saone-et-Loire, Massif central francais)
Authors: Tempier Paul 
Published: March 2020

Abstract
In the Charolais ridge in the northeastern part of the Central Massif (France) two granites can be distinguished. The Vauzelles granite to the south, is subalkaline, medium-grained, slightly porphyritic, and poor in inclusions. The Mary granite to the north is a coarse-grained monzonitic porphyry, containing green hornblende, and rich in inclusions. Identical granophyres are associated with both granites, but in differing modes of occurrence. This is ascribed to the difference in depth of the granites, the Vauzelles being deeper. The age of the granites is Visean (Carboniferous).
Le Quaternaire de la cote libanaise compare a celui du Maroc atlantique
Authors: Gigout Marcel 
Published: March 2020

Abstract
The Quaternary of the Lebanese and Moroccan coasts reflects five or six transgressions. Littoral marine sedimentation is represented by rich shell deposits in Morocco, but not in Lebanon. Inland from the coasts, entrenched fluvial terraces are observed in Morocco, whereas the same areas in Lebanon are occupied by slopes whose gradients are related to the maritime plains.
Premieres observations sur les alentours de la baie de Tongoy (Chili)
Authors: Herm Dietrich , Paskoff Roland , Stiefel Joerg 
Published: March 2020

Abstract
The Tongoy bay area, situated 300 km north of Valparaiso (Chile), is a graben bordered by two uplifted blocks. During the Pliocene and Quaternary this graben served as a depositional trap. From a geomorphic point of view, three marine stages are recognized, corresponding to periods of stillstand above present sea level. Geomorphic, paleontologic, and sedimentologic studies permit a precise determination of the Pliocene-Quaternary evolution of this region.
Stratigraphie et paleogeographie du Cretace inferieur de l'anticlinal de Gourdan et du bassin du Var moyen de Daluis a la Mescla
Authors: Cotillon Pierre 
Published: March 2020

Abstract
The Var basin (Provence Alps, southeastern France) is separated from the Esteron basin to the south by the Gourdan anticline. During much of early Cretaceous time the geography of this area closely resembled the present, with two basins separated by a fault scarp at the position of the present Gourdan anticline. In the Var basin a thick Vocontian-type section of dark pelagic marls to the west graded into a neritic section of thicker Berriasian sediments, very calcareous Valanginian sediments, and glauconitic Hauterivian deposits to the east. In the Esteron basin to the south, sediments were subneritic, with numerous interruptions of sedimentation and abundant glauconite. After Bedoulian (early Aptian) time the scarp disappeared so that the basins coalesced and sedimentation became uniform.
Donnees nouvelles sur le Cretace de la haute et moyenne vallee du Tagliamento (Alpes meridionales, Frioul, Italie)
Authors: Cousin Michel , Durand Delga Michel , Sigal Jacques 
Published: March 2020

Abstract
From the Cretaceous of Monte San Simeone [southern Alps, Italy], where the middle and upper Cretaceous stages are known (Selli, 1963), we have investigated and more precisely defined the known Cretaceous beds and have discovered other terrains whose stratigraphic assignment is yet to be established. The data are applied to certain stratigraphic problems (dating of a break and of breccias from the lower or middle Cretaceous), different types of sedimentation are described and compared, and some paleogeographic correlations are proposed.
Styles tectoniques de l'unite de l'Aljibe au nord du detroit de Gibraltar (Espagne meridionale)
Authors: Didon Jean 
Published: March 2020

Abstract
Different tectonic styles are recognized within the Aljibe unit N of the Strait of Gibraltar [southern Spain]. The lithology of this unit and that of the basement are, to a large extent, the cause. An anticline of the Penibetic basement, against which the sandstone of the Numidian facies has accumulated in tight folds and shingle blocks, seems to have played a large role during the emplacement of the unit. Elsewhere, it [the Aljibe unit] was dislocated into separate layers which have been overturned, welded, or overthrust. The westward displacements have local N-S components.
Etude geologique de la region de Stenico (Alpes meridionales, province de Trente, Italie)
Authors: Charvet Jacques 
Published: March 2020

Abstract
Marine facies ranging in age from Liassic to Eocene are present in the Stenico region (southern Alps, Trento province, Italy). The facies represent a transition between the Trentino flexure to the east and the Lombardy depression to the west. Neritic deposits in the Liassic are succeeded by pelagic deposits; pelagic sedimentation predominated from the upper Jurassic through the lower Eocene and became neritic in the middle Eocene. Evidence from brecciated formations indicates that movement at the beginning of the upper Cretaceous caused emergence in certain sections and reworking of submarine deposits in others.
Une espece nouvelle de Metrionaxon Glinski 1963 (Tetracoralla) dans le Couvinien du Finistere
Authors: Plusquellec Yves 
Published: March 2020

Abstract
Three Couvinian deposits in Finistere have yielded examples of a new species of Metrionaxon, M. paucitabulatum n. sp. Both internal molds and nondecalcified specimens of this small form are described. The genus, which seems to be restricted to the middle Devonian, has been previously known only in Germany (Eifel, Bergisches Land) and in Poland (Skala Podolskaya).
تطوير مادة تعليم المفردات لبرنامج “صباح اللغة” على أساس النظرية السلوكية لطلبة معهد الجامعة
Authors: Mujib Ahmad , Bashori Ahmad 
Published: March 2020

قام معهد أولى الأبصار بالجامعة الإسلامية الحكومية فونوروكو ببرنامج تعليم المفردات مقتصرا بطريقة حفظها وفهمها. هذا الواقع مشكلة هامة في تعليم المفردات لأن الهدف الأقصى لتعليم المفردات هو استخدام المفردات في الكلام. ومع ذلك أن مادة تعليم المفردات المستخدمة لم تساعد المدرسين والطلبة في تحقيق أهداف تعليم المفردات. انطلاقا مما سبق، فقام الباحث بتطوير مادة تعليم المفردات لبرنامج “صباح اللغة” على أساس النظرية السلوكية. أما منهجية البحث المستخدمة في هذا البحث هي البحث والتطوير الذي صممه Borg و Gall. وأما نتائج البحث فهي 1) إن خطوات تطوير مادة تعليم المفردات لبرنامج “صباح اللغة” على أساس النظرية السلوكية لطلبة معهد أولى الأبصار بالجامعة الإسلامية الحكومية فونوروكو هي تحديد المشكلات والاحتياجات، وجمع المعلومات كأساس تطوير المادة، وتصميم إطار تعليم المفردات على أساس النظرية السلوكية، وتصميم هيكل كتابة مادة تعليم المفردات، واختيار الموضوعات وترتيبها، وتصميم المحتوى والتدريبات، وتصميم إخراج الكتاب. 2) إن مادة تعليم المفردات المطورة صلاحة الاستخدام في برنامج تعليم المفردات بمعهد أولى الأبصار بالجامعة الإسلامية الحكومية فونوروكو.3) إن مادة تعليم المفردات على أساس النظرية السلوكية فعالة لمساعدة الطلبة والمدرسين في تحقيق أهداف تعليم المفردات
A model to predict unstable carotid plaques in population with high risk of stroke
Authors: Yin Junxiong , Yu Chuanyong , Liu Hongxing , Du Mingyang , Sun Feng , Yu Cheng , Wei Lixia , Wang Chongjun , Wang Xiaoshan 
Published: March 2020

Abstract
Background : Several models have been developed to predict asymptomatic carotid stenosis (ACS), however these models did not pay much attention to people with lower level of stenosis (＜50% or carotid plaques, especially instable carotid plaques) who might benefit from early interventions. Here, we developed a new model to predict unstable carotid plaques through systematic screening in population with high risk of stroke.
Methods : Community residents who participated the China National Stroke Screening and Prevention Project (CNSSPP) were screened for their stroke risks. A total of 2841 individuals with high risk of stroke were enrolled in this study, 266 (9.4%) of them were found unstable carotid plaques. A total of 19 risk factors were included in this study. Subjects were randomly distributed into Derivation Set group or Validation Set group. According to their carotid ultrasonography records, subjects in derivation set group were further categorized into unstable plaque group or stable plaque group.
Results : 174 cases and 1720 cases from Derivation Set group were categorized into unstable plaque group and stable plaque group respectively. The independent risk factors for carotid unstable plaque were: male (OR 1.966, 95%CI 1.406-2.749)，older age (50-59, OR 6.012, 95%CI 1.410-25.629; 60-69, OR 13.915, 95%CI 3.381-57.267;≥70, OR 31.267, 95%CI 7.472-130.83) , married(OR 1.780, 95%CI 1.186-2.672)，LDL-C(OR 2.015, 95%CI 1.443-2.814), and HDL-C(OR 2.130, 95%CI 1.360-3.338). A predictive scoring system was generated, ranging from 0-10. The cut-off value of this predictive scoring system is 6.5. The AUC value for derivation and validation set group were 0.738 and 0.737 respectively.
Conclusions ：For those individuals with high risk of stroke, we developed a new model which could identify those who have a higher chance to have unstable carotid plaques. When an individual’s predictive model score exceeds 6.5, the probability of having carotid unstable plaques is high, and carotid ultrasonography should be conducted accordingly. This model could be helpful in the primary prevention of stroke.