bluuebunny/crossref_metadata_2025_split huggingface dataset:
O cuidado ao adolescente com câncer na perspectiva da equipe multiprofissional
Authors: Souza Tamara Santos de , Gabarra Letícia Macedo 
Published: July 2019

Resumo O adoecimento por câncer na adolescência apresenta especificidades do ponto de vista biopsicossocial, o que coloca desafios à equipe na prestação de uma assistência de qualidade. Diante disso, este estudo teve como objetivo compreender a vivência do cuidado ao adolescente com câncer, na perspectiva da equipe multiprofissional de um Serviço de Onco-Hematologia adulto, de um hospital geral do sul do país. Para tal, foram realizadas entrevistas semiestruturadas com nove profissionais que compõem a equipe multiprofissional. A análise foi qualitativa, através do método de análise de conteúdo. Os dados foram organizados em quatro categorias: especificidades do cuidado ao adolescente com câncer, sentimentos mobilizados nos profissionais de saúde, estratégias de enfrentamento utilizadas pela equipe e desafios na assistência. A partir dos resultados, identificou-se que o cuidado ao adolescente oncológico tem impacto emocional significativo nos profissionais de saúde, exigindo investimento técnico e emocional por parte dos mesmos.
Articulaciones educativas para la inclusión de la diversidad
Authors: Munevar Dora Inés 
Published: July 2019

En el artículo se sostiene que las transformaciones educativas exigen compromisos individuales y acciones colectivas; también que en el marco de la ciudadanía y la justicia social se articula el debate sobre la inclusión en franca relación con las exclusiones. Este debate ha dado origen a la inclusión en la educación como un derecho que interroga a las complejas relaciones entre escuela e inclusión, como la base del ejercicio material de los derechos económicos, sociales y culturales, DESC, y como medio para hacer visibles los matices de la diversidad humana y escuchar la polifonía de sus voces. Por eso mismo, en los escenarios escolares se introduce el proceso de advocacy o abogacía como un mecanismo de exigibilidad política y jurídica de la educación inclusiva en clave de derechos. Esta alternativa exige pensar las articulaciones educativas en una institución resistente a las transformaciones.
DEVELOPMENT OF COSSACK POPULAR EDUCATION IN KUBAN REGION IN THE SECOND HALF OF THE 19TH CENTURY
Authors: Shturba V. A. , Shturba E. V. 
Published: July 2019

The article considers activity of official bodies of Cossack power of Kuban region in relation to changing the system of popular education for Cossack class in the light of the changes taken place in the middle of the 19th century in all the life spheres of the Russian Empire. The main attention has been paid to the problem of teachers’ training i.e. the main problem in the sphere of education of that time in Kuban.
RUSSIAN PARTICIPATION IN INTERNATIONAL ORGANIZATIONS ACTIVITIES IN THE SECOND HALF OF THE 1990S AND THE ISSUE OF THE COUNTRY’S NATIONAL SECURITY PROTECTION
Authors: Shturba E. V. 
Published: July 2019

The article considers the new approach of the Russian government in the sphere of foreign integration and cooperation with international organizations in the second half of the 1990s. Based on the analysis of factual and documentary proved data the reasons for the transfer of the country’s foreign policy into multi-vector direction and its diversification have been explained. The author’s evaluation of the attempts of Russia to integrate into multipolar world and the role of international cooperation in this process has been given.
José Gestoso y la historiografía artística de su tiempo (1852-1917)
Authors: De Tena Ramírez Carmen 
Published: July 2019

La finalidad de este trabajo de investigación es dar a conocer la figura deJosé Gestoso y sus aportaciones a la historiografía artística española.Para ello nos hemos valido de un estudio sobre las características de la práctica historiográfica restauracionista y de un análisis de las investigaciones llevadas a cabo por este erudito, así como de algunos aspectos de su personalidad. Como conclusión a este estudio destacamos el carácter precursor de las investigaciones de José Gestoso sobre el patrimonio histórico-artístico español y la aplicación del estudio y conocimiento del mismo para su tutela.
seismo‐live: An Educational Online Library of Jupyter Notebooks for Seismology
Authors: Krischer Lion , Aiman Yongki Andita , Bartholomaus Timothy , Donner Stefanie , Driel Martin van , Duru Kenneth , Garina Kristina , Gessele Kilian , Gunawan Tomy , Hable Sarah , Hadziioannou Céline , Koymans Mathijs , Leeman John , Lindner Fabian , Ling Angel , Megies Tobias , Nunn Ceri , Rijal Ashim , Salvermoser Johannes , Soza Sujania Talavera , Tape Carl , Taufiqurrahman Taufiq , Vargas David , Wassermann Joachim , Wölfl Florian , Williams Mitch , Wollherr Stephanie , Igel Heiner 
Published: July 2019

ABSTRACT
Efficient computer programming is becoming a central requirement in quantitative Earth science education. This applies not only to the early career stage but—due to the rapid evolution of programming paradigms—also throughout professional life. At universities, workshops, or any software training events, efficient practical programming exercises are hampered by the heterogeneity of hardware and software setups of participants. Jupyter notebooks offer an attractive solution by providing a platform‐independent concept and allowing the combination of text‐editing, program execution, and plotting. Here, we document a growing library with dozens of Jupyter notebooks for training in seismology. The library is made “live” through a server that allows accessing and running the notebooks in the browser on any system (PC, laptop, tablet, smartphone), provided there is internet access. The library seismo‐live contains notebooks on many aspects of seismology, including data processing, computational seismology, and earthquake physics, as well as reproducible papers and graphics. It is a community effort and is intended to benefit from continuous interaction with seismologists around the world.
Seismic Activity in the Permian Basin Area of West Texas and Southeastern New Mexico, 1975–79
Authors: Keller G. R. , Rogers A. M. , Orr C. D. 
Published: July 2019

Abstract
A seismic network of 12 self-contained, radio-telemetered seismograph systems was operated in the Kermit, Texas area for a period of 46 months. The main object of this study was to improve our understanding of the seismicity of this region where the first events were observed in 1964 and the first feit event occurred in 1966. Over 1300 events were located during this study, and the hypocenters displayed complex relationships with known geologie structures and oll field activity. Swarm activity was prominent, particularly in the southwest portion of the network. Most of the large events occurred near Kermit, Texas in the vicinity of the Keystone oil field and surprisingly few smaller events occurred in this area. The greatest concentrations of events (none feit), showed a strong spatial correlation with the War-Wink gas field.
Recurrence Intervals for Intraplate Earthquakes in Eastern North America from Paleoseismological Data
Authors: Talwani Pradeep , Collinsworth Keith 
Published: July 2019

Abstract
In intraplate settings in eastern North America, paleoseismological studies have been used to obtain recurrence of earthquake at three locations. As causative faults are usually inaccessible at these locations the effects of paleoearthquakes have been studied. While calculating recurrence intervals we have tacitly assumed that the earthquakes at each locality repeatedly occurred on the same faults. Indicators of paleoearthquakes that were studied include deformed soft sediments due to seismically induced liquefaction (New Madrid and Charleston, SC, seismic zones), warped lake sediments and anomalous silt layers in otherwise organic rich sediments (Charlevoix, Canada seismic zone). The resulting recurrence intervals for New Madrid (≈ 600 years) and Charleston (1500–2000 years) are in general agreement with those obtained from statistical studies. At Charlevoix it was estimated that a MM intensity VI event (sufficient to disturb varves) occurs every ≈ 400 years.
A Brief Update on the Focal Depths of Intracontinental Earthquakes and their Correlations with Heat Flow and Tectonic Age
Authors: Chen Wang-Ping 
Published: July 2019

Abstract
This paper summarizes the characteristics of focal depths of intracontinental earthquakes based on a compilation of reliably determined depths reported in the past five years. Since the study of Chen and Molnar (1983), several additional moderate-sized sub-crustal events (mb ≥ 5) have occurred in southern Tibet, the Tien Shan, and the Karakorum where such events are known to exist. Furthermore, three events have been identified near the Moho beneath the Brazilian shield, the coldest part of the Baltic shield, and the passive margin of Newfoundland. Since these events took place in stable parts of the continent, they must be an integrated part of the deformation of the intracontinental lithosphere at depth, not that of subducted material. Therefore there seems to be little doubt that earthquakes near the Moho is an incessant element of intracontinental seismicity. Due to the lack of detailed information on the crustal and mantle structures in the source regions, many of the events near the Moho seem to be located in the uppermost mantle but some might have occurred in the lowermost crust. In any case, the events near the Moho in most regions seem to be separated from the familiar seismicity in the upper part of the crust, forming a pattern of two seismogenic zones straddling an aseismic region in the lower crust. With data from South America and the Baltic shield, the maximum depth of earthquakes in cratons can be correlated with tectonic age within a single continent, and with low heat flow of the source region in a given tectonic province, respectively. These observations reinforce the view point that to a first approximation, the distribution of focal depth serves as an indicator of temperature or mechanical strength of the lithosphere, a result consistent with extrapolation of data from experimental rock mechanics. The aseismic zone in the lower crust is interpreted as a relatively weak region of the lithosphere sandwiched between two layers of more competent material where sufficient strain can accumulate to produce earthquakes.
Peak Accelerations From the 17 October 1989 Loma Prieta Earthquake
Authors: Boore David M. , Seekins Linda , Joyner William B. 
Published: July 2019

Abstract
Peak accelerations of the Loma Prieta main shock have been tabulated from instruments maintained by a number of organizations. We have analyzed a subset of 86 records from nominally free-field sites, which have been subdivided into rock, alluvium, and bay-mud categories according to data available in various reports. After correction for attenuation, the peak accelerations on rock, alluvium, and bay-mud sites are factors of 1.6, 1.8, and 4.5 larger, on the average, than Joyner and Boore’s (1988) predicted values for a M= 6.9 earthquake. The mean motions for the rock and alluvium sites are somewhat greater than one standard deviation away from the predicted value, but the mean acceleration from the bay-mud sites is well outside the range expected from analyses of data from previous earthquakes from rock and alluvium sites. Large amplitudes of motions on bay-mud sites relative to rock sites (a factor of 2.8 for the average of the recordings of the Loma Prieta main shock) has been found previously from recordings of distant earthquakes and explosions, but the Loma Prieta earthquake provided the first opportunity to study the relative amplitudes from strong-motion recordings.
Observational Test for Wave Propagation Effects in Local Earthquake Seismograms
Authors: Williams David E. , Langston Charles A. 
Published: July 2019

Abstract
Strong motion data for aftershocks of the 1982 Miramichi earthquake are analyzed to determine site effects on recorded waveforms. Although aftershocks vary in source mechanism, the complicated vector particle motion of P and S arrivals are often coherent between events recorded at the same station. This suggests that near-surface receiver structure has a significant effect on the recorded waveforms. Resonance features dominate the wavetrains with P reverberations existing on the vertical components and S reverberations prominent on the radial components indicating near vertical incidence. These reverberations take the form of peaks in the amplitude spectra which may complicate corner frequency interpretation. As an example, a corner frequency shift, fc(S) < fc(P), is evident and is attributed to structure induced effects. Synthetic seismograms computed using the propagator matrix method indicate that a thin low velocity layer of unconsolidated glacial till located directly beneath the receivers is responsible for most waveform effects. Attenuation effects in the thin layer are included in the computation of the synthetics in order to help match amplitude ratios. The geometry of the till-bedrock interface is interpreted as being three dimensional due to high tangential P amplitudes and anomalous particle motions. The observed waveforms are believed to consist mainly of direct waves, reverberations within the thin layer, and scattered arrivals resulting from the nonplanar interface. A careful analysis of three component waveform data in earthquake aftershock data sets such as this one considered here may be useful in determining local site conditions independent of assumed source models.
Characteristics of Seismically Induced Liquefaction Sites and Features Located in the Vicinity of the 1886 Charleston, South Carolina Earthquake
Authors: Amick David , Maurath Garry , Gelinas Robert 
Published: July 2019

Abstract
The ages of seismically induced paleoliquefaction features located in the Charleston, S. C. area suggest that the return period between large events similar to the 1886 earthquake is much longer than the historic record. If large prehistoric earthquakes have occurred elsewhere along the Atlantic Seaboard, then evidence of liquefaction features associated with them should be present in unconsolidated Pleistocene and Holocene deposits. To establish a comprehensive control data base for a regional analysis, liquefaction sites and features located in the Charleston area have been evaluated. Over 100 liquefaction sites were identified on the basis of a detailed review of historical accounts of the 1886 earthquake, and results of recent field studies. These studies then centered on characterizing the geologic, stratigraphic, and hydrologic setting of these sites and identifying criteria by which similar locales could be recognized elsewhere in the Atlantic Coastal Plain. This investigation also included the development of recognition criteria to distinguish seismically induced liquefaction features from pseudoliquefaction features (other features which look similar but are not seismic in origin). Guided by these findings, a systematic search for paleoliquefaction features outside the epicentral area of the 1886 Charleston earthquake is now underway.
Structural Relations and Earthquake Hazards of the Crittenden County Fault Zone, Northeastern Arkansas
Authors: Crone Anthony J. 
Published: July 2019

Abstract
A preliminary interpretation of about 135 km of seismic-reflection data provides new information on the structural relations between the the Crittenden County fault zone and the subjacent rift-bounding faults along the southeastern margin of the Reelfoot rift in the New Madrid seismic zone. On the reflection data, the rift boundary is marked by a 4- to 8-km-wide zone of incoherent reflected energy and disrupted reflectors in the lower part of the well-stratified, lower Paleozoic sedimentary rocks and in the underlying Precambrian crystalline basement. In places, the zone of disrupted reflectors extends into the upper part of the Paleozoic rocks, and, on some lines, disrupted reflectors and distinct faults are present in the Upper Cretaceous and Tertiary rocks of the Mississippi Embayment. The Crittenden County fault zone is interpreted as a northwest-dipping, high-angle reverse fault with an up-to-the-northwest throw, which is opposite to the net structural relief in the subjacent graben. The fault zone is at least 32 km long and coincides with the rift margin in southwestern Crittenden County, but to the northeast, it diverges away from the aeromagnetically defined margin of the rift by almost 4 km. Most faults in the Crittenden County fault zone are apparently ancient rift-bounding normal faults that were reactivated with a significant amount of reverse slip during the Mesozoic and Cenozoic. On the basis of its apparent connection with the rift-bounding faults, the evidence of its long history of recurrent movement, and its orientation with respect to the modern stress field, the Crittenden County fault zone might be considered to potentially generate major earthquakes. In contrast, the possibility that the Crittenden County fault zone could be a bending-moment fault argues against it being extremely hazardous. Precambrian crystalline basement interpreted on the profiles is commonly deeper than magnetic basement by as much as 2.5 km. This discrepancy between shallow magnetic basement and deeper crystalline basement could be explained by the presence of igneous intrusions in the Paleozoic strata immediately above Precambrian basement.
Shallow Seismic Reflection Survey of the Bootheel Lineament Area, Southeastern Missouri
Authors: Schweig Eugene S. , Shen Fan , Kanter Lisa R. , Luzietti Eugene A. , VanArsdale Roy B. , Shedlock Kaye M. , King Kenneth W. 
Published: July 2019

Abstract
During 1990 we collected eight lines (11.5 km) of shallow seismic reflection data across the Bootheel lineament, a discontinuous feature that extends about 135 km in a north-northeast direction through northeastern Arkansas and southeastern Missouri. The profiles image reflectors at depths between about 55 m to 800 m. Gentle folding with wavelengths of about 800 m and amplitudes of 10 m to 25 m is evident on nearly every profile, generally coinciding with the surface traces of the lineament. We interpret our lines to show a complex zone of strike-slip deformation consisting of multiple flower structures, with deformation at least as young as the Eocene/Quaternary unconformity.
Un paso hacia la internacionalización de Dictamen Libre
Authors: Chajin Flórez Miguel 
Published: July 2019

Uno de los mayores retos de una revista es poder mantener un enfoque sin caer en lo monotemático, porque se le cierra así la puerta a la complejidad de la realidad, y especialmente a la evidente necesidad de la articulación de saberes que se entretejen de múltiples maneras en cualquier objeto de conocimiento. Esta edición toca temas puntuales y concretos como la referencia a la empresa Electricaribe en Colombia, y otros de carácter epistemológicos e investigativos, de carácter general; de igual forma en lo disciplinar, relacionado con la Contaduría Pública, como los temas tocantes a la Administración y el emprendimiento empresarial.
The prevalence of obesity and the factors affecting obesity in the students of secondary education
Authors: Gokosmanoglu Feyzi , Cengiz Hasret , Varim Ceyhun , Yaylaci Selcuk , Nalbant Ahmet , Karacaer Cengiz 
Published: July 2019

Background: Childhood obesity has reached alarming dimensions all around the world. In this study, our objective is to determine the prevalence of childhood obesity in the secondary education as well as genetic, cultural and environmental factors giving rise to obesity, nutritional habits, family history and activity status.Methods: The research was performed on 750 students aged between 14-18. Body Mass Index (BMI= weight/height2 (kg/m²)) and Relative Body Mass Index (Rel BMI) values of each child were calculated by making use of their height and weight measurements. An evaluation was made through the use of a questionnaire form consisting of 46 questions that questioned the family history, nutritional habits and activity status of the children at issue.Results: About 41.7% of 750 children incorporated into the study were female, whereas 58.2% of them were male. The age distribution was between the age range, 14-18. According to BMI values, 12.3% of the children were overweight, while 4% of them were obese. According to Relative BMI values, on the other hand, 10.4% of the children were overweight, whereas 12.9% of them were obese. When the children’s nutritional habits, activity status and family history were evaluated, we ascertained that doing physical exercises irregularly, consuming pastry foods at home and the presence of obesity history within the family had all led to the development of obesity as well as being overweight (p <0.05).Conclusions: In these research subjects comprising children of secondary education, we showed that the nutritional habits, cultural nutritional differences and the insufficiency in physical activities as well as the genetic susceptibility in children could be the determinants in obesity development.
Antibiotic resistance profiles of Acinetobacter baumannii isolates from surgical wound infections at Kamuzu Central Hospital in Malawi:a retrospective study
Authors: Chitandale Edwin , Choonara Faheema , Mwenyephiri George , Zulu Mike , Chisale Master , Kipandula Wakisa 
Published: July 2019

Background: Acinetobacter baumannii has emerged as one of the most significant pathogen due to its ability to develop antimicrobial resistance to a broad range of commonly available antibiotics. It represents a serious iatrogenic complication of modern healthcare, where patients acquire infections in healthcare facilities with limited treatment options, resulting in increased morbidity, mortality and health costs. Methods: In this retrospective study, results of culture and antimicrobial susceptibility tests of samples collected from surgical wounds of patients from January to December 2017 were extracted from Laboratory information management system at Kamuzu Central Hospital (KCH) in Malawi.Results: This study ranks A. baumannii as the fourth common cause of surgical wound infections at KCH, with a prevalence of 12.3%. Other most prevalent isolates were: E. coli (25.9%), S. aureus (25.9%) and Proteus species (17.5%). All A. baumannii isolates were resistant to Amoxicillin/Clavulanate and Ceftriaxone; 96.4% were resistant to Ampicillin; 92.9% were resistant to Gentamycin, Ceftazidime and Sulphamethoxazole-trimethoprim; 89.3% were resistant to Ciprofloxacin; and 85.7% were resistant to Cefuroxime and Piperacillin/Tazobactam; while 17.9% were resistant to Meropenem. A total of 82% of the A. baumannii isolates were Multi-Drug Resistant (MDR), while 14% were Extremely Drug Resistant (XDR).Conclusion: The emergence of MDR and XDR A. baumannii at KCH calls for rational use of available antibiotics and regular monitoring of antimicrobial resistance patterns to prevent dissemination of current strains and emergence of new resistant strains.