Miracle-dz/UniFAR-FTUs huggingface dataset:
PENGARUH FAKTOR-FAKTOR DALAM DIMENSI FRAUD TRIANGLE TERHADAP PERILAKU KECURANGAN AKADEMIK SISWA KELAS XI AKUNTANSI SMK NEGERI 1 TEMPEL TAHUN AJARAN 2014/2015

Penelitian ini bertujuan untuk mengetahui: (1) Pengaruh Tekanan Akademik terhadap Perilaku Kecurangan Akademik Siswa Kelas XI Akuntansi SMK Negeri 1 Tempel Tahun Ajaran 2014/2015; (2) Pengaruh Kesempatan Menyontek terhadap Perilaku Kecurangan Akademik Siswa Kelas XI Akuntansi SMK Negeri 1 Tempel Tahun Ajaran 2014/2015; (3) Pengaruh Rasionalisasi Menyontek terhadap Perilaku Kecurangan Akademik Siswa Kelas XI Akuntansi SMK Negeri 1 Tempel Tahun Ajaran 2014/2015; dan (4) Pengaruh Tekanan Akademik, Kesempatan Menyontek, dan Rasionalisasi Menyontek secara bersama-sama terhadap Perilaku Kecurangan Akademik Siswa Kelas XI Akuntansi SMK Negeri 1 Tempel Tahun Ajaran 2014/2015. Penelitian kausal komparatif ini menggunakan subjek penelitian siswa kelas XI Akuntansi SMK Negeri 1 Tempel yang berjumlah 95 siswa. Teknik pengumpulan data yang digunakan adalah angket. Uji Instrumen yang digunakan adalah uji validitas dengan teknik Product Moment Pearson dan uji reliabilitas dengan rumus Alpha Cronbach. Uji prasyarat analisis yang dilakukan adalah uji linieritas dan uji multikolinieritas. Teknik analisis data yang digunakan adalah Analisis Regresi Sederhana untuk menguji hipotesis pertama, kedua, dan ketiga, serta Analisis Regresi Ganda Tiga Prediktor untuk menguji hipotesis keempat. Hasil penelitian menunjukkan bahwa: (1) Terdapat pengaruh positif Tekanan Akademik terhadap Perilaku Kecurangan Akademik Siswa dengan rx1y sebesar 0,314 dan r2x1y sebesar 0,099; (2) Terdapat pengaruh positif Kesempatan Menyontek terhadap Perilaku Kecurangan Akademik Siswa dengan rx2y sebesar 0,414 dan r2x2y sebesar 0,171; (3) Terdapat pengaruh positif Rasionalisasi Menyontek terhadap Perilaku Kecurangan Akademik Siswa dengan rx3y sebesar 0,578 dan r2x3y sebesar 0,334; dan (4) Terdapat pengaruh positif Tekanan Akademik, Kesempatan Menyontek, dan Rasionalisasi Menyontek secara bersama-sama terhadap Perilaku Kecurangan Akademik Siswa Kelas XI Akuntansi SMK Negeri 1 Tempel Tahun Ajaran 2014/2015 dengan Ry(1,2,3) sebesar 0,621 dan R2y(1,2,3) sebesar 0,385. Sumbangan Relatif Tekanan Akademik 49,36%, Sumbangan Relatif Kesempatan Menyontek 42,05%, Sumbangan Relatif Rasionalisasi Menyontek 8,59%. Sumbangan Efektif Tekanan Akademik, Kesempatan Menyontek, dan Rasionalisasi Menyontek sebesar 38,5%. Kata Kunci: Dimensi Fraud Triangle (Tekanan Akademik, Kesempatan Menyontek, dan Rasionalisasi Menyontek) dan Perilaku Kecurangan Akademik.
Observations of the formation and maintenance of beach cusps on Del Monte Beach in Monterey, California

Abstract : During the period of 5 April 2001 - 16 May 2001, topographic surveys of Del Monte beach in Monterey, California, were performed on a regular basis to record changes in beach cusp development for comparison to wave data being collected by the Oceanography Department of the Naval Postgraduate School. The surveys were conducted with a Real Time Kinematic Global Positioning System (RTK-GPS) secured to an all-terrain vehicle (ATV). The surveys were performed by driving the ATV on longshore transects of the beach to measure the vertical variation. From these surveys, the size and shape of the cusps were determined for each survey, and cusp variations between surveys were compared to the changes in wave conditions. Cusp spacing was determined through spectral analysis of the survey data, which produced peaks at the primary longshore wave numbers of the surf zone and swash cusps. The field data were then compared to current theory regarding beach cusp formation and maintenance in an attempt to determine the causative, maintenance, and destructive mechanisms.
Relativistic electron and energetic ion precipitation spikes near the plasmapause

An investigation has been made of electron and associated ion precipitation spikes near the plasmapause that are narrow in L shell and in which relativistic electrons are favored. The electron energy spectra during the spikes sometimes had equivalent e fold energies in excess of 500 keV. In approximately 31% of these spike events observed from the low-altitude polar orbiting satellites P72-1, P78-1, and S81-1, nearly simultaneous precipitation was measured in energetic ions above ∼30 keV at about the same L value. Several of the precipitation spikes occurred primarily in the drift loss cone, but in some cases, significant precipitation (∼10−2 ergs/cm² s) was also observed in the bounce loss cone. The electron spikes occurred preferentially in the evening sector, and all of the associated narrow ion spikes were in that local time interval. Narrow relativistic electron spikes were observed on less than 1% of the crossings of the plasmapause. From the set of S81-1 events a search was made for those also observed on the NOAA 6 spacecraft. On rare occasions, nearly simultaneous (<2000 s) narrow spikes with hard electron spectra were found at approximately the same L value from both spacecraft and at longitudes differing by 8°–47°. These findings suggest a patchy profile, sometimes with an arc structure which may extend over longitude intervals as great as 25° and time intervals as long as 2000 s. From consideration of the AE index for 17 events, 12 were found to occur close to the times of substorms. The spike precipitation is interpreted in terms of cyclotron resonance wave-particle interactions involving radiation belt particles, the narrow widths being associated with fine structure in the cold plasma density profiles near the plasmapause and the energy selectivity associated with an upper frequency cutoff in the waves.
CHATTANOOGA SHALE AND RELATED ROCKS OF CENTRAL TENNESSEE AND NEARBY AREAS

The Chattanooga shale crops out on the steep slope between the Nashville basin and the surrounding Righland Rim, and on many high hills within the basin in Tennessee. Outside the basin the black shale sequence is exposed in several river valleys and around tbe large Lexington Basin of Kentucky, Ohio, and lndiana. It also crops out along the ridges and valleys of the folded Appalachians in Tennessee, Georgia, and Alabama. lnformation is presented on the stratigraphy, composition, structure, paleography, and origin of the Chattanooga shale. Its relationship to the underlying and overlying formations is discussed. (C.H.)
Tourist destination image and consumer behaviour: The case of the Azores

Destinations are currently seeking to become more distinctive in an increasingly competitive market in which image is a decisive element in tourists’ destination selection. This study sought to understand the Azores’ overall image as a tourist destination in major source markets and to ascertain these markets’ level of satisfaction and behavioural intentions concerning the archipelago. The literature review in this paper addresses the definition of tourist destination image and the issue of satisfaction, since these influence intention to return and/or intention to recommend tourist destinations. The results indicate that (1) overall image influences satisfaction and intention to recommend and/or return to tourist destinations and (2) satisfaction influences intention to recommend and/or return to tourist destinations. This study also verified that most tourists are very satisfied with the Azores, as well as having a quite positive overall image of this destination.
Long waves in the equatorial Pacific Ocean

Westward traveling waves, with a period of 3 weeks and a wavelength of ∼1000 km, are observed intermittently in the central and eastern equatorial Pacific Ocean (see cover). The waves were first detected in 1975 in satellite measurements of the sea surface temperature [Legeckis, 1977]. Since then, additional measurements (under the auspices of the NOAA program Equatorial Pacific Ocean Climate Studies (EPOCS)) with a variety of instruments—drifting buoys, current meters and temperature sensors on moorings, and inverted echo sounders—have provided considerable information about these waves and have confirmed the hypothesis that they are caused by instabilities associated primarily with the latitudinal shear of the surface currents near the equator [Philander, 1978a; Cox, 1980].
Crystallization kinetics in a multiply saturated basalt magma - An experimental study of Luna 24 ferrobasalt

The paper deals with the effects of kinetics on mineral/melt partitioning and on fractional crystallization for a Luna-24 ferrobasalt. The composition is nearly multiply saturated under lunar surface conditions, making it possible to study the response of several mineral phases to kinetic factors during cooling. The differential suppression of the temperature of appearance of olivine, clinopyroxene, and plagioclase causes changes in the liquid line of descent. The course of liquid line of descent is mapped as a function of the cooling rate, and the partitioning of elements between pyroxene/liquid and olivine/liquid is examined.
Three‐dimensional dynamic models of subducting plate‐overriding plate‐upper mantle interaction

We present fully dynamic generic three‐dimensional laboratory models of progressive subduction with an overriding plate and a weak subduction zone interface. Overriding plate thickness (TOP) is varied systematically (in the range 0–2.5 cm scaling to 0–125 km) to investigate its effect on subduction kinematics and overriding plate deformation. The general pattern of subduction is the same for all models with slab draping on the 670 km discontinuity, comparable slab dip angles, trench retreat, trenchward subducting plate motion, and a concave trench curvature. The narrow slab models only show overriding plate extension. Subduction partitioning (vSP⊥ / (vSP⊥ + vT⊥)) increases with increasing TOP, where trenchward subducting plate motion (vSP⊥) increases at the expense of trench retreat (vT⊥). This results from an increase in trench suction force with increasing TOP, which retards trench retreat. An increase in TOP also corresponds to a decrease in overriding plate extension and curvature because a thicker overriding plate provides more resistance to deform. Overriding plate extension is maximum at a scaled distance of ~200–400 km from the trench, not at the trench, suggesting that basal shear tractions resulting from mantle flow below the overriding plate primarily drive extension rather than deviatoric tensional normal stresses at the subduction zone interface. The force that drives overriding plate extension is 5%–11% of the slab negative buoyancy force. The models show a positive correlation between vT⊥ and overriding plate extension rate, in agreement with observations. The results suggest that slab rollback and associated toroidal mantle flow drive overriding plate extension and backarc basin formation.
Evaluation of Lightning Incidence to Elements of a Complex Structure: A Monte Carlo Approach

There are complex structures for which the installation and positioning of the lightning protection system (LPS) cannot be done using the lightning protection standard guidelines. As a result, there are some "unprotected" or "exposed" areas. In an effort to quantify the lightning threat to these areas, a Monte Carlo statistical tool has been developed. This statistical tool uses two random number generators: a uniform distribution to generate origins of downward propagating leaders and a lognormal distribution to generate returns stroke peak currents. Downward leaders propagate vertically downward and their striking distances are defined by the polarity and peak current. Following the electrogeometrical concept, we assume that the leader attaches to the closest object within its striking distance. The statistical analysis is run for 10,000 years with an assumed ground flash density and peak current distributions, and the output of the program is the probability of direct attachment to objects of interest with its corresponding peak current distribution.
No association between a single nucleotide polymorphism in CYP19 and breast cancer risk.

Genetic polymorphisms in CYP19 have been hypothesized to alter aromatase activity and have been examined in relationship with breast cancer risk [(1][1], [2][2], [3][3], [4)][4] . A greater frequency of tetranucleotide (TTTA) n repeat alleles in intron 4 have been reported among affected women [(1][
Seismic Swarm Associated With the 2008 Eruption of Kasatochi Volcano, Alaska

[1] An energetic seismic swarm accompanied an eruption of Kasatochi Volcano in the central Aleutian volcanic arc in August of 2008. In retrospect, the first earthquakes in the swarm were detected about 1 month prior to the eruption onset. Activity in the swarm quickly intensified less than 48 h prior to the first large explosion and subsequently subsided with decline of eruptive activity. The largest earthquake measured as moment magnitude 5.8, and a dozen additional earthquakes were larger than magnitude 4. The swarm exhibited both tectonic and volcanic characteristics. Its shear failure earthquake features were b value = 0.9, most earthquakes with impulsive P and S arrivals and higher-frequency content, and earthquake faulting parameters consistent with regional tectonic stresses. Its volcanic or fluid-influenced seismicity features were volcanic tremor, large CLVD components in moment tensor solutions, and increasing magnitudes with time. Earthquake location tests suggest that the earthquakes occurred in a distributed volume elongated in the NS direction either directly under the volcano or within 5–10 km south of it. Following the MW 5.8 event, earthquakes occurred in a new crustal volume slightly east and north of the previous earthquakes. The central Aleutian Arc is a tectonically active region with seismicity occurring in the crusts of the Pacific and North American plates in addition to interplate events. We postulate that the Kasatochi seismic swarm was a manifestation of the complex interaction of tectonic and magmatic processes in the Earth's crust. Although magmatic intrusion triggered the earthquakes in the swarm, the earthquakes failed in context of the regional stress field.
Spatial Mobility and Access to Resources among the African Pygmies

First paragraph of Introduction : African Pygmies have occupied a prominent place in the debate about mobility and territoriality among hunters and gatherers, being one of the two examples used by Tiirnbull to define the notion of flux (1968). It is well known by now that arnong hunting and gathering societies, the problem of the determination of tenitoriality is linked with the definition of bot. group structure and spatial mobility (cf. Lee 1972). We cannot forget, however, that the emergence of territonality is sometimes assumed to be connected with agriculture, with sedentarity, or with trade (as the fur-trade in the case of subarctic North American Indians, Leacock 1954). African Pygmies, as a mobile but only semi-nomadic population, also provide us with the example of a hunting and gathenng society strongly linked with agricultural people; we have then to examine the consequences of these relations for the territorial behaviour of the Pygmies. In this paper 1 will present data concerning the three major Pygmy groups of Central Africa: the Mbuti Pygmies of eastern Zaire, the Aka of the Central African Republic, whom 1 studied for several years (Bahuchet 1985) and the Baka of eastern Cameroon, who show many similarities with the Aka although they speak a different language.
The magmatic plumbing of the submarine Hachijo NW volcanic chain, Hachijojima, Japan: Long‐distance magma transport?

[1] Recent geophysical observations on basaltic composite volcanoes in Izu-Bonin arc reveal the process of long-distance lateral magma transport within arc crust. To clarify a long-distance magma transport system of the basaltic arc volcano from geological and petrological aspects, we investigated 20-km-long submarine volcanic chains (Hachijo NW chain and Hachijo-kojima chain) and cones on the northeastern slope (NE edifices) as well as subaerial satellite cones nested Hachijo Nishiyama volcano in the northern Izu arc front. Basalts from Hachijo NW chain have more primitive composition than those from other edifices. The composition of the Hachijo NW chain basalts is controlled by fractional crystallization, while plagioclase accumulation occurred in NE edifices and subaerial satellite cones. Trace element and isotopic characteristics indicate that the same basaltic primary magma is involved in all sections of the volcano. This leads us to consider that magma was transported long distances between the Nishiyama volcano and the Hachijo NW chain. Primitive magma was laterally transported NNW for at least 20 km in the middle to lower crust (10–20 km deep) from Nishiyama volcano with only minimal crustal level modifications and formed Hachijo NW chain. On the other hand, magmas experienced crystal fractionation and accumulation at shallow magma chamber beneath Nishiyama volcano seems to have been transported in a short distance (<5 km) and formed NE trending edifices and subaerial satellite cones. The long-distance magma transport seems to be controlled by a regional extensional stress regime, while short-distance transport may be controlled by local stress regime affected by load of main volcanic edifice.
Alteration processes at Deep Sea Drilling Project/Ocean Drilling Program Hole 504B at the Costa Rica Rift: Implications for magnetization of oceanic crust

Magnetics properties and oxide petrography results are presented from the most recent penetration at hole 504B during Ocean Drilling Program leg 111. Our results, combined with those from previous studies, show abrupt first-order changes in magnetic properties at alteration boundaries. Within the 504B crustal section, changes in style and degree of alteration fall near the boundaries of the three well-defined lithologic units: the extrusive basalts, the transition zone, and the sheeted dike complex. This postemplacement alteration heavily influences magnetic properties and is observed to change, in both style and degree, with depth within each lithologic unit. Our results indicate that, at 504B, the extrusive crustal section deeper than 600 m below seafloor has become magnetically less stable due to postemplacement reheating and alteration. The upper, more permeable basalts above this critical depth have not experienced this reheating. Within the sheeted dike complex, the subsolidus cooling rate and the degree of hydrothermal alteration of the opaque minerals both decrease with depth. The changes in alteration of the oxide minerals occur in parallel with the decrease in bulk permeability associated with increasing depth. Overall, these observations suggest that the effective penetration of water into layer 2C decreased with increasing depth and resulted in a lower rate of convective cooling. Magnetic properties of rock samples from the sheeted dike complex suggest that as a result of this gradient in hydrothermal alteration, the upper dikes have become magnetically more stable than the lower dikes. A review of all magnetic properties indicate that the dike section at 504B carries a lower remanent magnetization than its intrinsic rock magnetic properties and mineralogy would predict. We suggest that this lower remanent magnetization is a result of the long and complex thermal and alteration history which involves the acquisition of magnetic components in different directions. Despite a magnetization which is lower than expected, it appears that the sheeted dike complex at hole 504B is capable of making a substantial contribution to the overlying marine magnetic anomaly. Because of the systematic decrease in hydrothermal alteration of magnetic minerals, the ability of the dike section to contribute decreases as a function of depth.
Modelling and experimental analysis of frequency dependent MIMO channels.

La integracion de tecnologias de ulta-wideband, radio-cognitiva y MIMO representa una herramienta podersoa para mejorar la eficiencia espectral de los sistemas de comunicacion inalambricos. En esta direccion, nuevas estrategias para el modelado de canales MIMO y su caracterizacion se hacen necesarias si se desea investigar como la frecuencia central y el acho de banda afectan el desempeno de los sistemas MIMO. Investigaciones preliminares han enfocado menos atencion en como estos parametros afectan las caracteristicas del canal MIMO. Se presenta una caracterizacion del canal MIMO en funcion de la frecuencia, abondandose puntos de vista experimentales y teoricos. Los problemas indicados tratan cinco areas principales: medidas, post-procesado de datos, generacion sintetica del canal, estadistica multivariable para datos y modelado del canal. Se ha disenado y validado un sistema de medida basado en un analizador vectorial de redes y se han ejecutado medidas entre 2 y 12 GHz en condiciones estaticas, tanto en linea de vista como no linea de vista. Se ha propuesto y validado un procedimiento confiable para post-procesado, generacion sintetica de canal y analisis experimental basado en medidas en el dominio de frecuencia. El procedimiento experimental se ha focalizado en matrices de transferencia del canal para casos no selectivos en frecuencia, estimandose ademas las matrices complejas de covarianza, aplicandose la factorizacion de Cholesky sobre ls CCM y obteniendose finalmente matrices de coloreado del sistema. Se presenta un procedimiento de correccion para generacion sintetica del canal aplicado a casos MIMO de grandes dimensiones y cuando la CCM es indefinida. Este CP permite la factorizacion de Cholesky y de dichas CCM. Las caracteristicas multivariables de los datos experimentales han sido investigadas, realizandose un test de normalidad compleja multivariable.
ENERGIA RENOVÁVEL: UMA ANÁLISE SOBRE OFERTA E DEMANDA DE ETANOL NO BRASIL

A grande necessidade de diminuir a dependencia em relacao ao petroleo devido aos seus precos em constante elevacao, a preocupacao com o meio ambiente (protocolo de kyoto) e a crescente demanda por carros flex tem colocado o etanol - uma energia totalmente renovavel - em papel de destaque, como fonte alternativa de energia. A demanda e a oferta por este biocombustivel sao crescentes nos ultimos anos e com grande possibilidade de se manter forte e dinâmica por varios anos. Neste contexto, o estudo teve como objetivo analisar quais as variaveis que afetaram a oferta e a demanda de etanol no Brasil, no periodo de 1995 a 2006. O metodo de analise utilizado foi o modelo de equilibrio simultâneo por meio de minimos quadrados em dois estagios, com correcao de variância via metodos de momentos generalizados (GMM). Para ilustrar o uso do modelo em simulacoes de politicas, investiga-se o efeito de um aumento relativo no preco do petroleo no mercado do etanol, ceteris paribus. Os resultados do modelo foram significativos, mas o interessante e que o alcool nao se mostrou substituto perfeito da gasolina no periodo analisado, pois o seu papel fundamental foi de aditivo da gasolina. ----------------------------------------------The great necessity for reducing the dependency upon oil due to its price, which is constantly increasing, the concern about the environment (Kyoto Protocol) and the increasing demand for flex cars have highlighted the role of ethanol - a totally renewable source of energy. The supply and demand for this biofuel are increasing in the past years and with a great chance to keep strong and dynamic for many years. In this context, the objective of the study was to analyse which variables affected the supply and demand for ethanol in Brazil, considering the period from 1995 to 2006. The method of analysis used was a simultaneous equilibrium model by means of two stages, least squares with correction of the variance by the generalized method of moments (GMM). To illustrate the use of the model in policy simulation it is studied the effect of a relative increase in oil price in the market of ethanol, ceteris paribus. The results of the model were significant, but what is interesting is that the alcohol did not appear to be a perfect substitutive for gasoline in the mentioned period, since his fundamental role was of an additive of gasoline.