bluuebunny/crossref_metadata_2025_split huggingface dataset:
APLIKASI BAHASA ISYARAT UNTUK TUNA RUNGU MENGGUNAKAN PLATFORM ANDROID
Authors: Mandarani Putri , Putra Yogi 
Published: June 2020

Di indonesia bahasa isyarat telah dibakukan dengan nama SIBI (Sistem Isyarat Bahasa Indonesia). SIBI merupakan salah satu media yang berbentuk buku. Akan tetapi belajar bahasa isyarat dengan buku kurang efektif karena buku tidak memiliki media video dan buku memiliki jumlah halaman yang tebal sehingga susah untuk dibawa kemana-mana. Tujuan dari pembuatan Aplikasi Mobile Learning Bahasa Isyarat ini adalah, agar tunarungu yang ada di indonesia bisa memanfaatkan smartphone untuk belajar bahasa isyarat dimanapun dan kapanpun. Dan aplikasi ini menyajikan materi berupa video yang mempermudah tunarungu untuk belajar bahasa isyarat. Setelah di implementasikan dan dilakukan pengujian, pada umumnya responden belum pernah menggunakan aplikasi bahasa isyarat sejenis sebelumnya. Oleh sebab itu maka aplikasi ini sangat dibutuhkan oleh tunarungu sebagai alternatif lain selain buku untuk belajar materi-materi dasar bahasa isyarat. Hasil pengujian menunjukkan 75% responded setuju bahwa aplikasi bahasa isyarat ini sudah layak untuk digunakan

In Indonesia sign language has been standardized by the name of SIBI(Sistem Bahasa Isyarat Indonesia). SIBI is one of the media in the form of books. But learning sign language with book less effective, because the book does not have video and the book has a number of pages thick, so hard to carry anywhere. The purpose of the Application of Mobile Learning Sign Language is, so deaf that exist in Indonesia can use a smartphone to learn sign language wherever and whenever. And this application presents the material in the form of video that makes it deaf to learn sign language. Once implemented and tested, in general respondents had never used sign language previous similar applications. So the application is very much needed by the deaf as an alternative books to learn the basic materials of sign language and also the test. The results showed 75 % Responded agree that the application of sign language is can be use by the deaf.
Motivasi Berprestasi: Konsep Diri, Kecerdasan Emosional dan Efikasi Diri
Authors: Bangung Podensiana , Hariani Lilik Sri , Walipah Walipah 
Published: June 2020

Motivasi berprestasi didorong oleh keinginan individu untuk melakukan sesuatu yang berharga atau penting demi tercapainya suatu target yang telah ditetapkannya. Motivasi berprestasi juga dapat dikatakan sebagai keinginan yang dimiliki seseorang untuk mengatasi hambatan atau mencari solusi untuk menyelesaikan suatu masalah dengan penuh tanggung jawab dan ketelitian berdasarkan standart yang ditetapkan oleh dirinya sendiri untuk mencapai suatu kesuksesan. Penelitian ini bertujuan untuk mengetahui pengaruh konsep diri, kecerdasan emosional dan efikasi diri terhadap motivasi berprestasi mahasiswa pendidikan ekonomi Universitas Kanjutuhan Malang baik secara simultan maupun parsial. Jenis penelitian ini termasuk penelitian ex-post-facto menggunakan metode pendekatan kuantitatif. Populasi dalam penelitian ini adalah mahasiswa pendidikan ekonomi Universitas Kanjuruhan Malang dengan jumlah 87 respinden. Penelitian ini adalah penelitian populasi karena semua anggita populasi dijadikan sampel. Teknik pengumpulan data dalam penelitian ini menggunakan kuesioner. Hasil penelitian ini menunjukkan bahwa terdapat pengaruh positif dan signifikan secara simultan dan parsial antara variabel konsep diri, kecerdasan emosional dan efikasi diri terhadap motivasi berprestasi mahasiswa pendidikan ekonomi UniversitasKanjuruhan Malang.
Bed-thickness frequency distributions and recurrence intervals of sediment-gravity-flow deposits intercalated in lacustrine varved diatomite: examples from the middle Pleistocene Hiruzenbara Formation, southwest Japan
Authors: Sasaki Hana , Sasaki Yasunori , Saito-Kato Megumi , Naruse Hajime , Ishihara Yoshiro 
Published: June 2020

ABSTRACTBed-thickness frequency distributions of sediment-gravity-flow deposits, especially turbidites, are one of the major interests of sedimentology. Lognormal, power-law, exponential, and truncated normal distributions have all been proposed for their frequency distributions. Although these frequency distributions have been obtained from many field observations and estimated from statistical models, problems associated with the complexity of sedimentary processes have remained. In this study, bed-thickness frequency distributions and the recurrence intervals of sediment-gravity-flow deposits intercalated in the Pleistocene lacustrine varved diatomite in southwest Japan were analyzed. The results reveal that the bed thicknesses of sediment-gravity-flow deposits induced by different mechanisms show different types of frequency distribution. For example, flood-induced sediment-gravity-flow deposits show power-law-like distributions, whereas such deposits caused by lake-slope-failure show lognormal distributions. The suggestion is that flood-induced types are deposited from floods having a power-law scale. However, the bed thicknesses of the deposits induced by lake-slope-failure do not purely reflect the event scale, because the lateral variation of their thicknesses reflects the depositional processes. The recurrence intervals of both types of event show Poisson-like distributions except for lake-slope-failure deposits at the slope-base section. Despite observed ranges, the distributions of lake-slope-failure deposits at the slope-base section have a high amount of zero value and the recurrence interval show exponentially decreasing. These results suggest that both events were generated randomly, despite different origins. In addition, the incompleteness of the records was also suggested from sediment bypass of a lake-slope-failure event at the slope-base section.
Dynamique de mise en place des extrasions monoclinales liasiques de la region de Taourirt (Maroc oriental); l'apport d'une etude d'inclusions fluides
Authors: Giret Philippe , Touray Jean-Claude , Ildefonse Jean-Pierre , Jebrak Michel 
Published: June 2020

Abstract
Fluorite samples collected at Jbel Tirremi and Koudiat Titeft, near Taourirt contain abundant secondary fluid inclusions which recorded various T and P information during the burial and subsequent uplift of these extrusions. The oldest inclusions are grouped along heterogeneous families with CO &lt;sub&gt;2&lt;/sub&gt; -bearing inclusions and halite-bearing ones in the same healed cracks. The minimum trapping temperature is 160 degrees C. Two independent geobarometers indicate trapping pressures higher than 0.5 Kb, implying a minimum burial of 3 to 4 km. Later epirogenesis, possibly related to deep faulting and associated halokinesis brought these structures to outcrop, probably from Miocene to present.
Precisions nouvelles au sujet des diapirs de Suzette (Vaucluse) et de Propiac (Drome)
Authors: Lapparent Albert F. de 
Published: June 2020

Abstract
Study of the contact zones of the Suzette diapir in Vaucluse and the Propiac diapir in Drome, France, shows that the emplacement of these Triassic blocks took place between the Miocene and Pliocene.
Complements a la geologie du nord de Figuig (Maroc SE)
Authors: Verlet Cecile , Roch Edouard 
Published: June 2020

Abstract
The Grouz and Maiez-Araiera mountains are two anticlinal massifs in the Figuig region, southeast Morocco, composed primarily of lower Liassic and Pliensbachian (Jurassic) strata. Triassic beds are exposed in some of the ravines. They are separated by the Tisserfine valley, a syncline composed of middle and upper Liassic and Bajocian strata. Cephalopods from various Jurassic zones are briefly described.
Sur la faune ordovicienne de Reaumur (Vendee) et les consequences geologiques qui en decoulent
Authors: Mathieu Gilbert 
Published: June 2020

Abstract
The discovery of an Ordovician fauna, mainly taxodont pelecypods, in shales of unknown age near Reaumur in the Saint-Pierre-du-Chemin syncline, Vendee, France, makes it possible to correlate the early Paleozoic of Vendee and Brittany.
Les phases de plissements tertiaires dans la region du Mont Ventoux et de la Montagne de Lure
Authors: Lapparent Albert F. de 
Published: June 2020

Abstract
Distinguishes three phases of Tertiary folding in the region of the Ventoux and Lure mountains, Provence, France: 1, post-Lutetian and pre-Sannoisian, 2, post-Sannoisian and pre-Burdigalian (first Alpine phase), and 3, post-Miocene (second Alpine phase).
Observation d'un "front" de metamorphisme regional
Authors: Perrin Rene , Roubault Marcel 
Published: June 2020

Abstract
Study of the contact between the crystalline schist of the Beaufortin massif and the overlying Triassic conglomerate in the Arly-Isere valley region, France, shows that the processes whereby the schist was metamorphosed likewise metamorphosed the conglomerate locally, and reveals that the progressive continuity of regional metamorphism was halted abruptly, thus forming a regional metamorphic "front."
De quelques manieres d'etre des calcispheres
Authors: Derville H. 
Published: June 2020

Abstract
Describes the different modes of occurrence of calcareous spheres in Carboniferous limestone of Avesnois, Nord, France. Those with a homogeneous granular structure and those with radial canals are assigned to Calcisphaera canaliculata n.sp., those with concentric form to C. cancellata Williamson, and those with three distinct rings to C. polyderma n.sp.
Notes paleontologiques sur le tonnelet des tourbieres (Amphitrema flavum Archer)
Authors: Dubois Georges , Dubois Camille 
Published: June 2020

Abstract
Discusses the systematic position, nomenclature, characteristics, and stratigraphic significance of the microfossil Amphitrema flavum, considered a specialized rhizopod, and describes its occurrence in Flandrian peat deposits (Quaternary) of France.
Distinction des sables marins et fluviatiles
Authors: Cailleux Andre 
Published: June 2020

Abstract
On the basis of analyses of different types of sands from various localities in order to establish criteria for distinguishing sands of marine and fluviatile origin, the general rule is formulated that, if the frequency percentage of grains with a diameter of three millimeters is greater than 30 percent, the sands are unquestionably marine; if the percentage is between 20 and 30 percent, the sands are probably marine. Application of the rule to a study of red sands of the Nantes region, France, demonstrates that the sands are Pliocene marine deposits formed in place, or (less probably) they are composed of Eocene marine material which was reworked in the Pliocene.
Sur les rhyolites et les granites prevarisques en Normandie et en Vendee
Authors: Mathieu Gilbert 
Published: June 2020

Abstract
An account of the pre-Carboniferous rhyolites and granites of Normandy and Vendee, France. Precambrian granite masses and Precambrian and Cambrian conglomerates containing ancient granite and rhyolite pebbles occur in both regions, and indicate that the Carboniferous granites of the Armorican massif were emplaced during the Variscan orogeny in a zone of subsidence between the rigid mass of Normandy to the north and Vendee to the south.
Festons au sommet de la craie de Normandie
Authors: Romanovsky V. , Cailleux A. 
Published: June 2020

Abstract
In the contact between detrital beds and the fissured chalk deposit which they cap, exposed in a quarry west of Gasny, Normandy, France, occurs a series of regularly spaced pockets, filled with calcareous material and rounded at the base, which gives the appearance of a festoon. It is concluded that the pockets represent transverse sections of postglacial polygonal soils rather thanproducts of decalcification or mud flow.
Le front nord-pyreneen entre le Salat et l'Adour
Authors: Schneegans D. , Michel P. 
Published: June 2020

Abstract
The zone of imbricate structures between the main ridge of the Pyrenees and its northern foreland in the Salat-Adour region, France, represents a cordillera which was formed during pre-Cenomanian embryonic crustal movements, discordantly covered by breccias during the Cenomanian (Cretaceous), and subjected to overthrusting during the main Pyrenean orogeny at the end of the Eocene.
Observations sur la tectonique des Pyrenees basques, a propos des travaux geologiques d'Eugene Fournier
Authors: Lamare Pierre 
Published: June 2020

Abstract
Describes the structural features of the Pyrenees in the Basque region, southern France, in the light of modern studies on the tectonics of the range, as well as of earlier concepts, especially that of Eugene Fournier who held that no nappes were present. It is suggested that the structural anomalies may be attributed to superposition of tectonic units associated with three orogenic phases--pre-Aptian (the major phase), pre-Cenomanian, and Turonian (Cretaceous).
Roches greseuses a ciment calcaire du Stampien; etude petrographique
Authors: Alimen Henriette 
Published: June 2020

Abstract
Describes sandstones with a calcareous cement which occur in places in the Stampian (Tertiary) deposits of France. Their formation is due to local conditions, such as the invasion of lakes by the Stampian sea, whereas the well-known Stampian sands of the Paris basin are dune deposits whose cement is siliceous.
Sur un depot de pente villafranchien cryoturbe a Vazeilles (Haute-Loire)
Authors: Bout Pierre J. 
Published: June 2020

Abstract
Ancient slope deposits exposed in a road cut near Vazeilles in the Velay range, France, are characterized by the presence of pockets and contorted layers which are considered due to frost action under Villafranchian (Pleistocene) periglacial conditions.
Note preliminaire sur quelques observations et interpretations nouvelles concernant les peridotites et serpentines de Nouvelle-Caledonie (secteur central)
Authors: Avias Jacques 
Published: June 2020

Abstract
Concludes that serpentinites of central New Caledonia are products of metamorphism (pseudomorphic serpentinization) of certain preexisting rocks (mainly volcanic rocks, particularly andesites), during which metallic ions, particularly magnesium ions, were added or concentrated, probably by diffusion processes. Peridotites were formed by a similar process of metamorphism of similar preexisting rocks, but in a zone of slightly higher temperature and pressure.
Observations sur les galets d'argile de la molasse dans la region lyonnaise
Authors: Maillard C. 
Published: June 2020

Abstract
Study of the character and distribution of clay pebbles in arenaceous Molasse (Tertiary) deposits of the Lyons region, France, leads to the conclusion that they were derived from estuarine muds and were formed under conditions of intense erosion, rather than in a calm lagoonal environment.
Silicifications nord-sahariennes [with discussion]
Authors: Auzel Marguerite , Cailleux A. 
Published: June 2020

Abstract
Describes samples of silicified continental limestone (and a silicified wood) from the Beni- Abbes region in the north Sahara, Algeria, compares their mode of silicification with that of marine limestones, and concludes that silicificationof the continental beds may be the result of sublacustrine processes in a permanent lake basin or of subaerial processes in stagnant pools which developed during sheet flood erosion.
Observations de metamorphisme du Trias dans les Alpes autochtones au lac de la Girotte (Savoie)
Authors: Perrin Rene , Roubault M. 
Published: June 2020

Abstract
Field work, confirmed by laboratory petrographic studies, demonstrates that autochthonous Triassic formations of the Girotte lake area in the Savoy Alps, France, were subjected to regional metamorphic processes which also caused metamorphism of the underlying crystalline basement rocks but which did not affect Liassic strata to any considerable degree. The Triassic formations probably constituted an obstacle to the advance of the metamorphic front, indicating that alteration was a process of solid diffusion.
Observations sur la position, l'age et les rapports des fractures de la region de Saint-Bonnet-de-Joux (Saone-et-Loire)
Authors: Russo Philibert 
Published: June 2020

Abstract
The north-northeast fractures in the Saint-Bonnet-de-Joux granitic dome, France, and in the Triassic-Jurassic formations on its flanks are due to gravity dislocations caused by pressure from the east during Oligocene Alpine movements and the radial fractures to upper Miocene crustal movements of greater depth.
Etude mineralogique des provinces distributives du materiel sedimentaire d'Aquitaine
Authors: Vatan Andre 
Published: June 2020

Abstract
A study of the mineral composition of various rock masses in the Pyrenees which supplied the detrital material forming alluvial, as well as Cretaceous and Eocene, deposits in the Aquitaine basin, France. For the most part the material supplied by the Pyrenees contains contact metamorphic minerals (garnet, andalusite, hornblende), whereas that supplied by the Central Massif contains minerals characteristic of a general regional metamorphism.
Etude morphologique de quelques sables de la region bordelaise
Authors: Balland R. , Cailleux A. 
Published: June 2020

Abstract
Investigation of the morphology of sand grains in detrital deposits of the Bordeaux region, France, shows that the so-called Landes sand formation is composed of two distinct units of different origin, one of which is characterized by an abundance of eolian grains and the other by grains exhibiting no evidence of wear. Material from older deposits contained rounded, well-worn grains.
Esquisse geologique de la commune de Sainte-Marie-de-Gosse (Landes)
Authors: Cuvillier J. , Schoeffler J. 
Published: June 2020

Abstract
The hilly terrain of the Sainte-Marie-de-Gosse area, Landes, France, previously mapped as an extensive outcrop of Keuper (Triassic) marls, is actually a lower Eocene massif. Keuper beds accompanied by upper Senonian (Cretaceous) strata occur in the core of the massif, and are exposed in places.
Remarques sur les flexures continentales de Chine
Authors: Teilhard de Chardin Pierre 
Published: June 2020

Abstract
The mountain ranges of China form an east-west series of north- south arcs, whose development is considered to have been cyclical and to have been accompanied by intrusion of extensive granitic masses which became consolidated near the surface. Three arcs are distinguished; from west to east they are accompanied by Carboniferous-Permian, Jurassic, and Tertiary granites respectively.
Etude pollenanalytique d'un lignite de la formation cineritique du Lac Chambon (Puy-de-Dome)
Authors: Firtion Fridolin 
Published: June 2020

Abstract
The pollen content of a lignite bed in lacustrine deposits of the Chambon lake region, France, is characterized by an abundance of Pinus silvestris, and indicates that the lignite is upper Tertiary in age.
Problemes de la geologie du Levant
Authors: Dubertret Louis 
Published: June 2020

Abstract
Outlines problems relating to the structure and the Cretaceous-Oligocene stratigraphy of the coastal ranges (and intervening basin) bordering the Mediterranean in the Middle East. The ranges are blockfaulted massifs characterized by the juxtaposition and superposition of two types of structures--fractures related to deep-seated Jurassic formations and folds associated with Cretaceous strata. Uplift of the massifs subsequent to transgression of the Cretaceous sea is considered to have been caused by extensive subsidence of adjacent blocks now submerged in the Mediterranean.
Infrastructure des Alpes et tremblement de terre du 25 janvier 1946 [with discussion]
Authors: Oulianoff Nicolas 
Published: June 2020

Abstract
Distinguishes four structural complexes in the Alps, noting in particular that the crystalline basement is composed not only of Hercynian (late Paleozoic) masses but also of recrystallized material which had been subjected to extensive folding prior to emplacement of Hercynian granite massifs, probably during the Caledonian (early Paleozoic) orogeny rather than in an early stage of the Hercynian orogeny. The earthquake in the Valais region, Switzerland, was undoubtedly tectonic in origin, but whether it represented a continuation of Alpine movements or was caused by subsidence associated with isostatic readjustment of crustal blocks cannot yet be determined.
Contribution a l'etude tectonique de la Mediterranee occidentale
Authors: Russo Philibert 
Published: June 2020

Abstract
Summarizes the tectonic history of the ranges bordering the western Mediterranean. Their formation was due primarily to tangential pressures from the southeast, as a result of which two major upwarps separated by a generally north-south trans-Mediterranean syncline were produced. Continued pressure from the southeast caused folding, overthrusting, rotation of crustal blocks, and other dislocations, whose development was controlled by the fracturing of the upwarps, accompanied by the downdropping of the axial zone, and the relative position of rigid and plastic masses.
Le bassin tertiaire de Saint-Martin de Londres et l'orogenese de l'anticlinal du Pic Saint-Loup (Herault)
Authors: Dreyfuss Maurice , Gottis M. 
Published: June 2020

Abstract
Pre-Lutetian (probably early Eocene for the most part) and pre-Oligocene crustal movements caused the formation and folding of the Saint-Martin de Londres lacustrine basin at the foot of the north slope of the Pic Saint-Loup anticline, Herault, France. Post-Oligocene dislocations caused thrusting and overturning of Jurassic strata of the northern flank of the anticline.
Les mammiferes pleistocenes d'Afrique
Authors: Arambourg Camille 
Published: June 2020

Abstract
The Pleistocene mammalian assemblages of the Omo valley region (Ethiopia) and other African localities constitute a relatively homogeneous indigenous fauna, characterized by the presence of Tertiary survivals, which disappeared during the course of the Quaternary. It is concluded that instead of being a refuge for Tertiary relics, Africa was a center of evolution and dispersion.
Presence d' "algal balls" dans le Bathonien de la Sarthe; considerations sur les girvanelles
Authors: Dangeard Louis 
Published: June 2020

Abstract
Reports the discovery of algal balls (calcareous nodules containing Girvanella sp.) in Bathonian (Jurassic) deposits of the Sarthe region, France. Although algal balls are of no stratigraphic value, they are significant for facies determinations, in that they are diagnostic for extremely shallow-water depositional basins.
Le Maestrichtien du domaine sous-pyreneen a l'est de Saint-Gaudens
Authors: Rech-Frollo Marguerite 
Published: June 2020

Abstract
Petrographic study of Maestrichtian (Cretaceous) rocks, mainly sandstones, from the Pyrenees foreland region east of Saint-Gaudens, France, shows that lateral variations in facies are frequent, that two types of sedimentation obtained during formation of the deposits, and that the sandstones exhibit striking similarities with Flysch sandstones of the Romanian Carpathians.
Hydrogeologie du pertuis de Saint-Remy- de-Provence et ses abords
Authors: Corroy Georges 
Published: June 2020

Abstract
Hydrogeologic investigations in the pass separating the Alpilles Urgonian (Cretaceous) limestone range, at whose base Saint-Remy-de-Provence, France, is located, from the Crau Vindobonian (Tertiary) plateau to the north, support the conclusion that the Durance river did not flow through the pass in the geologic past.
Conditions lacustres en milieu marin; le Danien de la partie orientale du sillon nord-pyreneen
Authors: Rech-Frollo Marguerite 
Published: June 2020

Abstract
Study of the lithologic and faunal composition of Danian limestones of the eastern part of the Cretaceous trough at the foot of the north slope of the French Pyrenees leads to the conclusion that a variety of petrographic types is present and that the so-called lacustrine limestones were formed in a marine basin in which lacustrine conditions were produced at times by the introduction of fresh waters from rivers flowing down ranges bordering both sides of the trough.