bluuebunny/crossref_metadata_2025 huggingface dataset:
La “libertad de invertir” a la luz del caso argentino: un análisis de los Tratados Bilaterales de Inversión
Authors: Ghiotto Luciana
Published: October 2018

Este artículo se propone revisar el andamiaje legal internacional construido para garantizar la libre circulación de las inversiones, lo cual se ha vuelto central en el capitalismo contemporá- neo, caracterizado por el comando del capital en su forma dineraria. Es así que en los últimos treinta años hemos asistido a una búsqueda creciente de protección del movimiento del dinero, generada a través de esquemas legales que sostienen la circulación irrestricta del capital a través de las fronteras estatales. En particular,aquí nos concentramos sobre los Tratados Bilaterales de Inversión (tbi). Dentro de estos, adquiere una importancia particular la cláusula de prórroga de jurisdicción, que permite a las empresas transnacionales demandar a los Estados en instancias supra-nacionales, como el Centro Internacional de Arreglo de Diferencias sobre Inversiones (CIADI).
Derechos humanos de las niñas y los niños y la prohibición del matrimonio infantil en los tratados internacionales
Authors: Nares Hernández José Julio , Colín García Ricardo , García Suárez Rod
Published: October 2018

En México, las niñas desde los 14 años y los niños desde los 16 pueden contraer matrimonio con el consentimiento de sus tutores. Al emanciparse, adquieren legalmente las obligaciones de una persona adulta y pierden los derechos humanos de los niños, lo cual, a esa edad, agudiza su estado de vulnerabilidad. Para evitar este problema, los tratados internacionales más progresistas en la materia han recomendado a los Estados parte legislar para prohibir el matrimonio infantil, estableciendo la edad mínima de 18 años para contraer matrimonio. El objetivo de este artículo es analizar, con base en los principios constitucionales del interés superior del menor, en relación con los principios de progresividad, interpretación conforme y pro persona, la obligación del Estado de cumplir con los tratados que garantizan una protección más eficaz a los derechos humanos de los niños.
Hacia una democracia paritaria. La evolución de la participación política de las mujeres en México y sus entidades federativas
Authors: Torres Alonso Eduardo
Published: October 2018

El libro que nos entregan Manuel González, Karolina Gilas y Carlos Báez es un insumo fundamental para comprender el largo y arduo trayecto que las mujeres han recorrido para ejercer con plenitud sus derechos políticoelectorales. Es, pues, un trabajo integral sobre la participación femenina en el espacio público y sobre la labor de protección jurisdiccional de los derechos de las mujeres en el ámbito electoral
La representación política en Puebla (entrevista al doctor Raymundo García)
Authors: Sánchez Espinoza Francisco
Published: October 2018

Entrevista realizada en Ciudad Universitaria, Facultad de Derecho y Ciencias Sociales de la Benemérita Universidad Autónoma de Puebla. Martes 3 de diciembre de 2013. El interés por conocer los puntos de vista del entrevistado se dan en el desarrollo de mi proyecto de investigación sobre el sistema electoral de México, donde analizo el caso federal, y los de Tlaxcala, Puebla, Chiapas y Veracruz, además de Costa Rica y Chile. Específicamente, busqué a Raymundo García 2 para discutir el caso de Puebla. La presentación no tiene un formato específicamente de entrevista, porque fue más bien una charla, de la cual guardo la grabación de audio y notas escritas. Se usará la primera persona para la voz del doctor García, específicamente cuando habla de la publicación de su libro, su propuesta de reforma como legislador, o su adscripción partidista. Asumo las notas a pie de página. El fondo del artículo está constituido por ideas compartidas en la charla.
Subvirtiendo la democracia. Viejas y nuevas claves de lectura
Authors: Cansino César
Published: October 2018

La cuestión de la democracia aparece hoy como simple, pero en realidad es bastante compleja, ya que bajo la palabra democracia se ocultan muchas cosas diferentes. En este sentido, la palabra democracia se convirtió en un asunto político neurálgico. La complejidad de la cuestión de la democracia se pone en evidencia a través de todos los debates que hay actualmente sobre la noción de promoción de la democracia, lo cual está en el centro de la acción de la Unión Europea y, por supuesto, en el centro de la acción americana. Pero los europeos y los americanos no le dan la misma definición. Para simplificar, los americanos dan una definición que es estrictamente liberal e institucional, mientras que los europeos intentan defender una visión un poco más societal de la democracia. El aporte de la reflexión sobre la historia y la acción de la democracia es poner de manifiesto que el desarrollo de la democracia no es simplemente el desarrollo de más democracia directa, sino de más reflexión, de más deliberación. Introducir la razón en el mundo público, eso es una definición de la democracia altamente subversiva.
Perspectivas jurídicas de las relaciones internacionales: el constitucionalismo, la fragmentación y el pluralismo jurídico en debate
Authors: Peixoto Batista Juliana
Published: October 2018

El presente trabajo trae a la luz los diferentes aportes teóricos que interrelacionan el derecho internacional y las relaciones internacionales en el análisis e interpretación de los cambios vividos por el sistema internacional a fines del siglo xx y principios del siglo xxi. Detalla las posiciones teó- ricas enfrentadas que componen los estudios acerca de la constitucionalización y la fragmentación del derecho internacional, así como los enfoques del pluralismo jurídico. En ese sentido, la primera parte está dedicada al debate sobre la constitucionalización del sistema internacional. La segunda parte está dedicada a las críticas estructurales a dicho enfoque, además de hacer un recorrido por literatura dedicada a la fragmentación para al final analizar algunos enfoques más relacionados con el pluralismo jurídico. Por último, se tejen conclusiones acerca del debate teórico entre esos enfoques, considerando sus aspectos más relevantes con los que describen el panorama internacional en clave jurídica.
Movimientos sociales, democracia y Estado de derecho. Una mirada a la contribución de los movimientos sociales a la democratización e institucionalización del Estado de derecho
Authors: Zamora Lomelí Carla Beatriz
Published: October 2018

Este trabajo tiene por objetivo comprender la incidencia de los movimientos sociales en los procesos de democratización de la sociedad y el establecimiento del Estado de derecho. Así, tomando como eje la constitución de la democracia, se abordan los aportes de Jürgen Habermas, Robert Dahl y Guillermo O’Donnell, a fin de establecer los principios que teóricamente deberían regir en la democracia contemporánea. Además, se vinculan dichos aportes para definir su correspondencia con la institucionalización de las normas a través del Estado democrático de derecho. Se estima que bajo regímenes democráticos la triada movimientos sociales, democracia y Estado de derecho contribuye a la apertura política y a la obtención de derechos en la sociedad, toda vez que se encuentre una estructura de oportunidades políticas que posibilite la inclusión de las demandas de los movimientos sociales al sistema jurídico y se obtengan avances democráticos en la vida normativa. Así, se afirma que la democracia trasciende el marco institucional y puede encontrar nuevos causes a través de los conflictos sociales que inauguran los movimientos sociales, siempre y cuando se encuentre un régimen democrático tendiente a incluir tales expresiones.
About Late Gagary-Ostrovian biota (Late Permian) at the North of the Siberian platform
Authors: Sadovnikov G. N.
Published: October 2018

Prior to the beginning of a trap volcanism of Central Siberia there was a plain, covered by Cordaitanthales. Slope herbaceous cover consisted mainly of ferns. Equisetopsida prevailed in the swampy lowlands. Volcanic eruptions at the end of Vishkilian (Severodvinian) led to the formation of a hill. It was covered by similar vegetation, but vegetation of herbaceous slopes substantially prevailed. Woody vegetation was dominated at only two locations, it was also about 50% at three locations and absent at two ones. Associations of the grassy slopes in most places were at least 46%, they were about 100% in two places and absent in 42% of the places. Ferns dominated sharply. Todites (?) anthriscifolia, Todites (?) sibirica, Prynadaeopteris (?) karpovii, rarely Cladophlebis aff. taimyrensis were dominants. Sometimes Prynadaeopteris (?) venusta were codominants. Yavorskyia radczenkovii sometimes codominated among gymnosperms. The herbaceous cover of the lowlands was dominated by Equisetopsida. At two locations, they are about 100%, and more than 50% at two ones , and from 12 to 33% at four ones. They are absent only at two localities. Paracalamites were usually dominants. Sometimes hyllotheca turnaensis, P. minuta, Paraschizoneura codominated. In the basins, Palaeoanodonta (Bivalve) had a significant role. Thus, the composition of the flora of the Late Gagary-Ostrovian time has a little difference from the Early Gagary-Ostrovian, but the ecological differences are significant. Forest communities are inferior to the dominant role of herbaceous slopes ones. This makes the flora of the Late Gagary-Ostrovian time be similar to the followed Tutonchanian - Early Dvurogyan flora in the ecological sense.
About tectonic zoning and features of the structure of Russian part of Arctic mobile belt
Authors: Karaulov V. B.
Published: October 2018

The principles of the tectonic zoning of the continents are discussed. The tectonic zoning of the Russian sector of Arctic mobile belt is considered and a brief characteristic of the West-Arctic and East-Arctic recent platforms, formed at the place of this belt, is given. The data about the position of the boundaries of the recent platforms, about the structure of their basement and sedimentary. The possible approaches to the determination of the structure and tectonic nature of the «transient» complex of the plates of the recent platforms.
Two generations of scapolite at Snezhnoe ruby deposit, Central Pamir
Authors: Litvinenko A. K. , Moiseeva S. B. , Sharifi D. D.
Published: October 2018

At Snezhnoe ruby deposit, localized in the eastern part of the tectonic zone of Central Pamir, two generations of sсapolite have been discovered by the textural and structural features. The first one is in paragenesis with ruby, plagioclase, phlogopite, muscovite, margarite and fuchsite. It was formed under the regional metamorphism of the high-temperature amphibole facies in the Early Proterozoic. The second generation is localized in the veins of the crossing ruby bodies. Two types of the veins have been distinguished: monomineral scapolite veins and polymineral - scapolite-margarite-muscovite ones. They were formed at the regressive stage of Cretaceous-Paleogene tectonic metamorphic cycle.
MINERAL COMPOSITION AND STRUCTURAL FEATURES OF JEWELER AMMONITES FROM KOSTROMA REGION
Authors: Petrochenkov D. A.
Published: October 2018

Detailed mineralogical examination of ammonites of jewelry quality has been carried out by means of radiographical, X-ray microanalyses and electronic microscopy. The ammonites consist mainly of calcite, apatite and some cells are constituted of phosphorite. The walls and shell’s septums consist of apatite and calcite, which have replaced original aragonite and maintain inclusions of pyrite of globular shape, aluminosilicate and organic matter. Dispersed apatite determines the black color of walls and shell’s septums. The color and transparency of the calcite, filling up the shell’s chambers, are determined by the quantity of micropores and microinclusions, mainly of apaTite. Ammonites from Kostroma region by its decorative and technology characteristics will be able to use widely in jewelry and interior articles.
PLACERS OF MAJOR VALLEYS IN THE LENA GOLD-PLACERS REGION
Authors: Vinogradova O. V.
Published: October 2018

The morphology and inner structure of the placers in the maj or valleys of the Lena gold-bearing area are considered. The morphology of placers in the plan and the distribution of gold within the contours of the valleys are determined by the morphodynamic type of the channels and their evolution in different parts of the valley. The influence of the major tributaries on the placers structure is found out. They determine the presence of the gold-bearing formations, transverse to the axis of the valley, as well as the abrupt changes of the elevation values of the bottom of the metal-bearing layers, which are located on the outcrops of different height levels and in the erosion hollows - paleochannels of the tributaries. Taking these facts into account allow predicting the position and morphology of the gold formations in buried valleys, to identify undiscovered fragments of placers and to increase the accuracy of delimitation blocks for the estimation of the gold reserves.
METHODS FOR THE CHOOSING THE RATIONAL COMBINATION AND COMPARISON OF THE CHARACTERISTICS AND FACTORS OF THE EFFICIENCY OF THE PRODUCTION PROCESSES AND TECHNOLOGIES OF THE BOREHOLE DRILLING
Authors: Kulikov V. V.
Published: October 2018

The paper considers the methods for choosing the rational combination and comparison of the measured characteristic sand factors, used during decisions making, designing and assessment the efficiency of the production processes and boreholes drilling technologies. When choosing the rational comparison of the homogeneous characteristic sand factors, in abas is of the formalized representation of the methods the reisa coordinate geometrical approach, based on the definition of the maximum (minimum) distance between the points, located in the arithmetical n-dimensional Euclidean space and characterized by the given object of the analysis and decision making. Formalized representation of the methods for the choosing the rational combination of non-homogeneous as well as the homogeneous characteristics and factors bases on the definition of the maximum (minimum) value of the product of the their values. The examples are given from the different fields of the drilling production processes and technologies.
SPHERE OF MINERAL RESOURCES USE: FORMATION OF THE SECTORIAL INDUSTRIAL TECHNOLOGICAL SYSTEMS
Authors: Lisov S. V. , Vinslav YU. B.
Published: October 2018

The paper gives the definition of the term «sectorial industrial technological system» as an instrument for the realization of macro-level industrial policy, with regard to the features of concrete kinds of economical activity. The main methodic demands for the designing of such systems are formulated. The key ones are to define the perspective demands to the technological development of the sector, to define the subject-technological priorities and organizational ecomonical mechanisms of integration of economic subjects in corresponding directions. The feasibility and possibilities of such sectoral systems formation with regard to the geological sector specifics are characterized. The presence of the powerful scientific indusirial cenier as JSC «Rusgeology» gives the significant competitive advantages in the sectoral industrial technological systems design.
Mineral resources and budget of the country
Authors: Kozlovsky E. A.
Published: October 2018

An issue about the role of mineral resources in the economic development of Russia has been considered. The divergence between the given possibilities and real budget has been marked. A conclusion has been made, that the system of the strategic investigation of mineral resources does not correspond the problem of country’s mineral safety provision and a complex of measures has been suggested, which are to lead to the improvement of the system of mineral deposits searching.
Some features of the competitive relations in high school
Authors: Kushel’ E. S.
Published: October 2018

An analysis of the competitiveness of the high school is considered as a patch of the subsystems, which level of development determines its competitive advantages. The subsystems have been distinguished: basic high school activity, additional high school activity, providing high school activity.
About a new type of redeposition of fossils
Authors: Yushin K. I. , Komarov V. N.
Published: October 2018

At the final stage of the taphonomic cycle, after the deposit has gone to the surface in a result of different processes, the alteration of the deposit in the zone of surface weathering occurs, due to the mechanic destruction as well as the processes of soiution and replacement. A phenomenon of the deposition in thanatocenosis the reburied fossils - redeposition - has a widespread occurrence in this time. On the basis of the unique finding of the cervical vertebra of the Upper Pleistocene European roe deer in the modern freshwater catfish (Silurus glanis Linnaeus) a new type of the fossils redeposition - biogenic, which can be realized by a variety of the organisms. Its account can be used for a more complete breakdown of the processes, which lead to the forming of the deposits.
New approaches to the determination of the density of the solid bodies
Authors: Kulikov V. V.
Published: October 2018

New approaches to a definition of the basic characteristic of the bodies - density, have suggested. To improve the technique of the caring out the laboratory investigations, increasing the safety of the investigations and preventing the damages of the diagnosed products in liquid medias, instead of caring out the traditional hydrostatic weighting of the studied samples (in liquids, in particular heavy immersion ones, demanding the special conditions of the safe usage), a method of the aerostatic weighting (a determination of the weight in a compressed air) and a method of the weighting in finely-dispersed loose materials have been considered.
«Platinum» from the collection of A.F. Keller in the State geological museum RAS
Authors: Braynchaninova N. I. , Makeyev A. B. , Makavetskas A. R.
Published: October 2018

The microprobe tests of the supposed platinum from the collection of F.A. Keller at the State geological museum of Russian Academy of Sciences have been carried out for the first time. The results have shown that the samples were indeed acquired in the XIX century in the Urals in Nizhnyi Tagil, a famous industrial area, supplied from Gospodskaya mine, being operated in that times. Concentrate platinum according to the shape and mineral compound corresponds to Isovsko-Turinskaya concentrates from Svetloborsky concentrically zoned dunite-clinopyroxenite platinum-bearing massif. Analyses of the chemical composition of the mineral phases have allowed making a list of the native metals minerals and platinum group minerals (PGM) in this collection: isoferroplatinum, r-isoferroplatinum, golden isoferroplatinum, copper-nickel tetraferroplatinum, osmium, Ru-osmium, iridium, Ru-iridium (ruthenosmiride), fine gold and tin.
Automation of the complex ecological monitoring of the territory of the airport using the method of machine learning
Authors: Ekzarian V. N. , Rukavitsyn V. V. , Zyulyaeva M. V.
Published: October 2018

The main criteria of the airport territory pollution have been revealed during both studying of the data for the ecological conditions of the various airports of the world and carrying out a number of the field measurements. They have been: atmospheric air analysis, analysis of the ground, surface and waste water, measurements of the noise. The structure of such system, the sources of its data and the functionality have been described. The system of the environmental forecasts formation with machine learning elements has been presented. It includes stations of the automatic environmental monitoring, a subsystem of the information analysis and a subsystem of the processed information publication.
RELATION OF THE MORPHOSTRUCTURE OF THE CREST POSITION OF THE VORONEZH ANTECLISE WITH THE DEEP INHOMOGENEITIES OF THE LITHOSPHERE
Authors: Ezhova I. T. , Nadezhka L. I. , Tregub A. I.
Published: October 2018

The morphostructure of an crest part of the Voronezh anteclise is closely related to the neotectonics of the territory. A feature of the newest structure, in contrast to the Paleozoic, Mesozoic and Paleogene structures, is predominantly the submeridional orientation of the interchanging raised and downdip blocks. The following regularities of the degree of the reflection of the deep inhomogeneities in neotectonic and geomorphological characteristics have been revealed. The zones of the reduced density at the top of the mantle have been noted to be corresponded in general by neotectonic blocks with the elevated relief. Areas of the high density values in a number of cases are corresponded by the Neogene-Quaternary blocks of the second rank with the reduced values of relief depth marks. Both of the relationships of the thickness of the earth’s crust and the height of the relief, negative and straight, have been observed. A complete spatial correlation between these parameters has been not observed, but on the whole, the structural plan of the Neogene-Quaternary structural-material complex is consistent with the spatial location of large heterogeneities in the litho sphere.
A vertical water exchange of the groundwater in the central part of Moscow artesian basin
Authors: Fisun N. V.
Published: October 2018

The hydrogeological features of the central part of the Moscow artesian basin (MAB) under the natural conditions provided the existence of the downward vertical flows of the groundwater, the formation of the fresh underground waters of the Carboniferous complex, desalination of the Upper Devonian subterranean waters. The long exploitation of the Aleksin-Protvino horizon in the central part of the MAB led to the formation of a depression of the piezometric level with a depth of 80 m, as well as a change in the ratio of the absolute marks of the piezometric surfaces of the groundwater of the Lower Carboniferous and the Upper Devonian, and the creation of prerequisites for the changing of the orienfafion of the vertical wafer exchange between them. A map of the difference in pressures between the Aleksin-Protvino and the Upper Devonian horizons, compiled by the author, shows this situation. In a vast zone of the central part of the MAB, the pressure surface of the Alexin-Protvino horizon is 30-50 m below the upper Devonian horizon. Under these conditions, it seems important to study the Upper Devonian aquiferous complex as a possible source of the «contamination» of the groundwater of the Lower Carboniferous, especially in the zones of active lineaments of the Moscow syneclise.
Estimation of the dimensional variability in the properties of soils in the basement of the atomic power station (APS) territory
Authors: Gousseltsev A. S. , Pendin V. V. , Barulin G. P. , Gorobtsov D. N.
Published: October 2018

A method of the estimating the variability of the physical and mechanical characteristics of soils has been considered. The applying of this method in practice can be used to find out the weakened zones and tectonic structures at the territory of the atomic power stations, and also - traditionally - to estimate the influence on the behavior of the elementary natural technical system «construction - soils». The tasks of the revealing the character of the occurrence of the various possible structural non-homogeneities, which may influence on the atomic power station territory estimation, as well as a general plan allocation, have been estimated in geological parameters fields’ assessment at the one of the constructed atomic power stations territory and environs. The characteristics of the physical properties (humidity, density, zero-air dry unit weight, index fluidity) have been compared on the base of the analyses of the laboratory tests. The analysis has been done for a layer-marker which corresponds to the chalk deposits of the Turonian stage. A selective analysis of the dimensional variability of the soils’ properties has been done for the engineering-geological researches results on the territory of the atomic power-station and, in particular, reactor divisions. It has been concluded, that to make a right forecast, the additional engineering and geological investigations of the atomic power station are needed. Such researches will allow the sustainable definition, or confirmation, of the existing deformation and strength properties of the soils which are in the basement of the buildfngs for the depth, which is deeper than compressible thickness depth.
Modeling of the stress-strain state in the earthquake epicenter area (Kumamoto Earthquake, Japan), 16.04.2016 M 7.3
Authors: Morozov V. N. , Manevich A. I.
Published: October 2018

On the 16th of April, 2016, a strong earthquake with M 7,3 occurred in the Kumamoto prefecture (Kyushu, Japan). This earthquake is the strongest in the last 30 years in this area. For a day before the main shock, two foreshocks with M 6,4 were registered. For seven days after the main shock, aftershocks activity spread to the north-east and south-west, most of the hypocentres of the aftershocks with M 6,4 were localized within the seismogenic layer in the depth interval from 5 to 10 km. The authors have modeled a stress-strain state (SSS) of the epicentral area be fore the earthquake and after it (after the formation of the main fault). For this purpose, a software package is used, that allows 2-D formulation (plane strain condition), for modeling SSS block heterogeneous geological environment, disrupted by a system of tectonic faults. The faults are modeled in the form of extended zones of the dispersed geomaterial, which elastic modulus are significantly lower than the elastic modulus of the environmental media. A structural-tectonic scheme of the Kumamoto earthquake area is used. An analysis of the results of SSS modeling has been done for the area 30x40 km before and after the earthquake. It is shown that the area and magnitude of the stress intensity in anomalous zones are the predictive signs of the location and intensity of a possible strong crustal earthquake, and the vector of the rapid decrease in the potential energy of deformation could be a guide for the most probable direction of tectonic rupture during a crustal earthquake. The results received can be useful in a deterministic approach to seismic hazard assessment and carrying out the geophysical observations focused on the forecast of the strong crustal earthquakes in the continental areas.
A new representative of the Hadrocheilus (Arcuatobeccus) Shimansky subgenus (rhyncholites) from the Lower Cenomanian of the South-West Crimea
Authors: Komarov V. N. , Aglutdinova K. R. , Agafonova G. V. , Huzina I. R. , Babitsky E. F. , Glukhov M. A.
Published: October 2018

Rhyncholites of the Arcuatobeccus subgenus represent a big group, counting about 25 species and known from the Western Europe, Mountain Crimea and also San-Salvador Island. A stratigraphic distribution of the Arcuatobeccus covers an interval from the Middle Jurassic up to the Middle Cenomanian, inclusively. In the Mesozoic deposits of the Mountain Crimea, Arcuatobeccus are not popular and distributed in the section unevenly. To the last moment four Cenomanian species of Arcuatobeccus were known there. A Lower Cenomanian complex included H. (A.) alekseevi Komarov, H. (A.) ratus Shimansky и H. (A.) selbuchrensis Komarov. In the Middle Cenomanian complex, a one species of Arcuatobeccus was found - tiny H. (A.) prima Komarov. It is important to note, that the Middle Cenomanian Arcuatobeccus have not been known anywhere else in the world yet. The paper illustrates a new Lower Cenomanian species of Arcuatobeccus, found in 2017 during the Crimean training geological practice of MGRI-RSGPU. It differs from the closest species Hadrocheilus (Arcuatobeccus) selbuchrensis by a bigger size, shorter and narrower handle (in relation to the hood) and sharper, knee-like transition of the hood to the handle. The results of the detailed study of the bearlng-rock have been shown.
RHYNCHOLITES AND THE PROBLEM OF NARROW AND BROAD CONCEPTION OF TAXONS
Authors: Khuzina I. R. , Komarov V. N.
Published: October 2018

The paper considers a point of view, based on the conception of the broad understanding of taxons. According to this point of view, rhyncholites of the subgenus Dentatobeccus and Microbeccus are accepted to be synonymous with the genus Rhynchoteuthis, and subgenus Romanovichella is considered to be synonymous with the genus Palaeoteuthis. The criteria, exercising influence on the different approaches to the classification of rhyncholites, have been analyzed (such as age and individual variability, sexual dimorphism, pathological and teratological features, degree of disintegration of material), underestimation of which can lead to inaccuracy. Divestment of the subgenuses Dentatobeccus, Microbeccus and Romanovichella, possessing very bright morphological characteristics, to have an independent status and denomination to their synonyms, has been noted to be unjustified. An artificial system (any suggested variant) with all its minuses is a single probable system for rhyncholites. The main criteria, minimizing its negative sides and proving the separation of the new taxon, is an available mass-scale material. The narrow understanding of the genus, used in sensible limits, has been underlined to simplify the problem of the passing the view about the genus to the other investigators and recognition of rhyncholites for the practical tasks.
DEFORMATIONS AND THE SEQUENCE OF THE STRUCTURES FORMATION IN THE NORTHERN PART OF THE ZONE OF DEVELOPMENT OF MAKSUTOVO METAMORPHIC COMPLEX (SOUTHERN URALS)
Authors: Golionko B. G. , Ryazantsev A. V.
Published: October 2018

Composition and structural evolution of the Maksutovo metamorphic complex in the its northern part has been examined. The early folds 77) plunging in the SE direction have been established to be developed only in the rocks of the Maksutovo metamorphic complex. The problem of the definition of the geodynamic nature of the 7Л deformation stage, marked by the folds 77), has not been solved yet. Tectonic inclusions of the metamorphic rocks adjacent to the western border of the Main Uralian Thrust without traces of 7Л deformation stage must not be considered as parts of the Maksutovo metamorphic complex. 7Л1 deformation stage expressed in formation of thrusts and 77. west vergent folds is connected with late Paleozoic continental collision. The third stage of deformation 7JIII is marked by development of 77) folds with steep hinges associated with post collision strike slip movements
CRUSTS OF WEATHERING AS BASIC SUPPLIERS OF TERRIGENOUS MATERIAL DURING FORMATION OF ANCIENT DIAMONDIFEROUS PLACERS
Authors: Zinchuk N. N.
Published: October 2018

On the example of Mesozoic deposits of one of the main diamondiferous regions of the Siberian platform, basic suppliers of terrigenous material into the ancient diamondiferous placers under formation and their occurrences have been characterized. Special attention has been paid to characteristics of local sources of allothigenous material removal to sedimentation basins of the said period, the main of which were Middle-Late Triassic crusts of weathering on terrigenous-carbonate rocks, formations of trappean origin (dolerites, tuffs, tufogene thick layers) and kimberlites. Comparatively short transfer of weathering products and their accumulation mainly in freshwater continental basins determined weak hydrothermal effect of environment on allothigenous minerals. The received specific features of the mineral composition of various rocks' crusts of weathering have been recommended for application during paleogeographical reconstructions in diamondiferous regions, to determine source areas of terrigenous material, in particular. The stated recommendations have been implemented when assessing material from local sources of drift (including diamondiferous material as well) to continental (Irelyakh and Ukugut suites) and coastal (Pliensbachian and Toarcian stages) deposits of MaloBOtuobinsky region, where primary and placer diamond deposits are successfully mined.
ABOUT LITHOMINERALOGICAL COMPOSITION OF ANCIENT SEDIMENTARY DIAMONDIFEROUS ROCKS
Authors: Zinchuk N. N.
Published: October 2018

Litho-mineralogical and structural-formation generation features of Upper Devonian-Carboniferous crusts of weathering on terrigenous-carbonate rocks, kimberlites and deposits enriched by products of their redeposition, have been studied, that allowed restoring of the specific features of upper Paleozoic productive horizons generation of the main diamondiferous regions of the Siberian platform, and then, the areas, favorable for generation and preservation of kimberlite (including diamondiferous) material dispersion haloes, have been distinguished within them. Analysis of Upper Paleozoic deposits facies, as well as specific features of their location, has allowed to establish that denudation of the rocks of the region was insignificant since the moment of their crust formation and up to completion of upper Paleozoic sedimentation, and occurred only along the stream flows. The omnipresent availability of crusts of weathering on terrigenous-carbonate rocks of lower Paleozoic, preserved from washout by upper Paleozoic deposits, points on it. These formations are usually elongated in the form of narrow streams and represent fragments of most initial erosion of the crusts of weathering in post-Carboniferous time. That is why, at such minimal shear, practically all kimberlite minerals, occurring in Upper Paleozoic deposits, are redeposited from more ancient pre-Lapchanian formations. The necessity of differentiated approach to studying formation conditions of various facies of diamondiferous upper Paleozoic deposits of continental and coastal genesis has been substantiated, and firstly — studying of their specific features. The complex research is required, with application of structural-tectonic, lithological-facial and formation-cyclic analyses, which would allow allocating specific areas favorable for generation of ancient placers of diamonds or discovering kimberlite pipes.
CARBONIFEROUS 40Ar/39Ar AGE OF THE RARE METAL-ENRICHED RHYOLITES AND IGNIMBRITES IN THE SAKMARA ALLOCHTHON OF THE SOUTHERN URALS, THEIR GEOCHEMICAL FEATURES AND GEODYNAMIC SETTING
Authors: Ryazantsev A. V. , Pilitsina A. V. , Novikov I. A. , Degtyarev K. E.
Published: October 2018

In the structure of the Sakmara allochthon of the Southern Uralssequence with rhyolites and ignimbrites locally occures. They have Nb-Zr-REE geochemical specialization. This sequence unconformably overlays folded Paleozoic complexes, including the Devonian ones. Rhyolite contains K-feldspar and quartz phenocrysts, K-feldspar glomeroporphyrites and granite xenolith. Geochemical features of the rhyolites show intraplate-originated affinities and A-type granite composition.40Ar/39Ar age of the felsitic matrix of the rhyolites of 303±2 Ma defines the age of the volcanic complex origin. For feldspar phenocrysts the age of 306±3 Ma and 337±3 Ma is obtained. The first value coincides to the matrix age and connected with formation of the volcanic complex. The second value belongs, apparently, to xenogenic material. Obtained age values reflect the evolution of Carboniferous active continental margin magmatism, widespread in different structural zones of the Urals. Rare-metal rhyolites characterize the final late Carboniferous intraplate (rift-related) back-arc magmatism at the active continental margin. Volcanism preceded to a collision-related ophiolitic thrust nappes emplacement.
LATE PALEOZOIC ALKALI-GRANITOID MAGMATISM OF SOUTHERN KAZAKHSTAN AND ITS ROLE IN THE FORMATION OF THE ORE-BEARING VOLCANIC STRUCTURES OF KENDYCTAS-CHU-ILI-BETPAK-DALA URANIUM ORE PROVINCE
Authors: Maliutin S. A.
Published: October 2018

Areas of distribution of alkaline granitoids in southernKazakhstanhave been identified, most of which are located within the Kendyktas-Chu-Ili-Betpakdalin uranium-bearing province, traditionally considered as Late Devonian-early Carboniferous. Arguments in favor of late Paleozoic age of alkaline rocks have been given. The proximity of the petrographic composition, petrochemical and geochemical features of the alkaline granites of the Chu-Ili-West-Balkhash area and late Paleozoic alkaline granites of the Zailiysky area has been established, confirming their age and continental rift origin. Similarity in the development of magmatism and hydrothermal mineralization of ore-bearing volcanic structures of the Chui area (Kurmanshitinskoe) and North-Western Chingiz (Ulkentuz and Dostar) has been revealed. In these structures, Devonian volcanic rocks are interspersed with subvolcanic bodies of comendites and later dikes of microgabbrodiorites and microdiorites. The hydrothermal mineralization of these structures took place in multiple stages. The early stage includes secondary quartzites, which developed in Devonian volcanogenic rocks. Comendite is associated with K-feldspated and albitized rocks, as well as with zones of rare-metal (Zr, Nb, Th, U and TR) Fe-Mg metasomatites that originated in the middle stage. In the later stage, after the introduction of microgabbrodiorite dikes, berezites with U-Mo mineralization formed. Comendites in the structures of the North-Western Chingiz break through the deposits D2-3 and D3-C1 and are considered to be the comagmatic alkaline granites of the neighboring late Paleozoic massifs (Tleumbet and Kuyrektykol). The noted similarity may also indicate that the Chui area comendites are likely to be dated to the late Paleozoic age. Examples have been given to the superposition of berezites and U-Mo mineralization on the late Paleozoic granosyenites, which are widespread in the Kurdai volcanic structure, as well as on the alkaline granites of Karasai volcanic structure. Their age may also be late Paleozoic. Additional research has been recommended for the final conclusions on the age of alkaline rocks and uranium mineralization.
RESULTS OF GEOLOGICAL SURVEY IN THE EASTERN SIDE OF THE SOUTHERN PART OF THE PRE-URALS FOREDEEP
Authors: Osipov A. V. , Bondarev A. V. , Mustaev R. N. , Monakova A. S. , Zakharchenko M. V. , Minligalieva I. I.
Published: October 2018

The results of field work carried out by the authors in September2017, inthe region of the eastern side of the southern part of the Pre-Urals foredeep, have been presente. It has been shown that the studied object has significant prospects of oil and gas potential, which has been confirmed by a number of marked signs and assumptions (oil manifestations, presence of a smell of oil). The results of studies of 21 samples of Paleozoic rocks of different ages, selected during the field work, by the Rock-Eval express method have been presented. At such analytical level, for the first time in the region, the Silurian deposits (Sakmar Formation of the Llandoveri Stage) have been studied. According to the results of pyrolytic studies it has been proved that the rocks of this age within the southern part of the Pre-Urals trough are oil and gas source rocks and are characterized by a rich generation potential.
LONG-LIVED STRUCTURAL ENSEMBLES OF THE EAST EUROPEAN PLATFORM. Article 2. THE STRUCTURE OF THE TOP OF THE BASEMENT
Authors: Kolodyazhny S. Y.
Published: October 2018

The basement’s top tectonics of the East European platform (EEP) has been considered on the basis of the modern mapping data. The importance of the long-lived tectonic zones that form the vortex megastructure has been justified.

Their Riphean — early Vendian evolution was associated with activation of the Paleoproterozoic tectonic zones, which were transformed into paleorifts (aulacogens). The systems of the EEP aulacogens show the features of nonlinear structure and development: their evolution proceeded in the mode of transtension inside asymmetrically organized space between the active and passive paleocontinental margins; most of the paleorifts display wedge-shaped morphology, signs of asymmetric rifting and blocks rotation, a complex combination of elements of shear zones and gentle detachment zones tectonics, the vortex megastructure of the entire rifts system. Using an «iris diaphragm» model and the reconstructions with reversing plate rotation makes possible to explain the main patterns of the long-lived vortex structure of the EEP.
DISCOVERY AND DEVELOPMENT OF IULTINSKOYE TIN-TUNGSTEN DEPOSIT
Authors: Romanova V. V.
Published: October 2018

The Iultinskoye deposit was discovered 80 years ago in the remote and unexplored region of Chukotka. Discovery and development of the deposit were accompanied by serious difficulties. A brief biographic data about the discoverer of the deposit V.N. Milyaev has been presented here. The Iultinsky mining processing plant, which was opened in 1959, was closed in 1994 due to the changing in the economic situation. The deposit was conserved, Iultinsky village was liquidated. Vernadsky State Geological Museum RAS has samples of cassiterite and wolframite, collected by geologists of the Second Chukotka Glavsevmorput expedition in the year of the deposit discovery.
THE ZIRCON CHRONOLOGY OF THE INTRUSIVE MAGMATISM OF THE KANIN PENINSULA
Authors: ANDREICHEV V. L. , SOBOLEVA A. A. , SERGEEV S. A. , PRESNYAKOV S. L.
Published: October 2018

The Kanin Peninsula is an elevated block of the Timan Ridge where Precambrian sedimentary-metamorphic sequences and magmatic  rocks, intruding them, form the Kanin Kamen Ridge. In the  northwestern part of the Peninsula on the coast of the Barents Sea,  there is a unique outcrop of two-mica granites, monzonitoids and  lamprophyres cutting metaterrigenous rocks of the Upper Riphean  Tabuyev series and overlain by Lower Permian limestones. To establish the age of magmatic rocks, U-Pb dating of zircons has been carried out by secondary ion mass spectrometry (SIMS) method. In  zircons from granites, an age of 883 ± 16 Ma has been obtained,  which corresponds to the beginning of the Late Riphean, and the  subsynchronous formation of subalkaline rocks occurred in the Late  Cambrian. The age of monzogabbro is 505 ± 7 Ma, and  lamprophyres – 504±7Ma.
GEMMOLOGICAL CHARACTERISTICS OF SENGILIT — A NEW KIND OF JEWELRY-ORNAMENTAL RAW MATERIALS OF THE ULYANOVSK REGION
Authors: PETROCHENKOV D. A.
Published: October 2018

Sengilite is a trade mark of florogenic jewelry and ornamental material being mined around the village Sengilei of the Ulyanovsk  region. The sangilite is a lithofected marine plant remains cemented  in marl. The sangilite mainly consists of calcite (from 86 to 94 wt.  %). The following minerals have been established (wt. %): pyrite  2,5—6, quartz 2, montmorillonite 3, dolomite 2, in minor quantities  illite, kaolinite, jarosite, gypsum, chalcopyrite can be presented. Among the elements-admixture, Sr is presented up to 0,053 wt. %  and Ba up to 0,023 wt. %. The content of radioactive and  carcinogenic elements is at the background level. The original  structure of plant remains is inherited in sengilite. The differently  colored zones of sengilite are determined by the size and structural  features of the calcite crystals, as well as the amount of pyrite  inclusions, and the presence of marl. In the calcite, the following elements-admixture, (wt. %) are noted: Mg from 0,68 to  1,29, Fe from 0,14 to 0,52, insignificant amounts of Mn. According to its technological and decorative characteristics, sengilite is a new  high-quality jewelry and ornamental material that allows to produce  a wide range of jewelry and souvenirs. Collection and processing of  sengilit in the Ulyanovsk region along with ammonites and other  types of jewelry and ornamental raw materials will increase the profitability of the deposit and the range of products.
THE CHANGE OF ROLE OF THE HYDROGEOLOGICAL CONDITIONS AT THE DIFFERENT STAGES OF THE FUNCTIONING OF NATURAL-ARCHEOLOGICAL SYSTEMS
Authors: VYAZKOVA O. E. , CHEREPANSKY M. M. , BELOV K. V.
Published: October 2018

The time-varying resources for water supplies of historical settlements, fortifications and fortresses in periods of their creation and usage have  been analyzed. Nowadays it is necessary to assess the role of  hydrogeological conditions as an important component of engineering- geological conditions in order to study the reasons of conservation and destruction of archaeological sites. The contribution of groundwater  in protection (conservation) of organic origin artifacts has been  considered. It is necessary to ensure a safe groundwater level to avoid  flooding and chemical weathering during the process of the museumification of the archaeological sites.
Razón narrativa y razón histórica.
Authors: Cruz Cruz Juan
Published: October 2018

El presente histórico es una acumulación de los pasados que lo han posibilitado. Referir esa acumulación real es precisamente “narrar”. Tanto Ortega y Gasset como Ricoeur han descrito el  sentido de la “razón narrativa”, que para Ortega es también la “razón histórica”. Pero, a juicio del  autor, la razón histórica no expresa todo lo que el hombre es; por lo que apela a una  inteligencia sensibilizada que permita comprender no sólo el ser histórico, mediante una  configuración inventiva de los eventos, sino el fondo ontológico del hombre.
“La infancia de Jesús”, de RATZINGER, Joseph (Benedicto XVI).
Authors: Encinas Cantalapiedra Arturo
Published: October 2018

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“El Resurgimiento Católico en la Literatura Europea Moderna (1890-1945)”, de SÁNCHEZ COSTA, Enrique.
Authors: Miró López Susana
Published: October 2018

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Nanoética. Una reflexión ética necesaria por una nueva revolución científica, la Nanotecnología.
Authors: Canabal Berlanga Alfonso
Published: October 2018

El artículo muestra los orígenes y desarrollo de la nanotecnología. La producción de los nanoproductos y su comercialización supone un reto a la hora de respetar los intereses del ser humano, conservar el equilibrio medioambiental y económico, siendo protagonista de las reflexiones éticas iniciales la bioseguridad en la fabricación de sus componentes y sus repercusiones medioambientales. La nanotecnología supone una oportunidad de mejorar la vida de las personas, pero también puede constituir una oportunidad para el desequilibrio socieoeconómico, la carrera armamentística y una amenaza para la naturaleza del ser humano. Recogemos las recomendaciones más importantes que deberían gobernar este proceso innovador en todas sus vertientes, directrices procedimentales, otras más filosóficas, intentando no perder la perspectiva ética de un mundo tan tecnificado.
La Riqueza de las Naciones de Adam Smith en España.
Authors: Hernández Andreu Juan
Published: October 2018

El presente estudio analiza la recepción de la obra de Adam Smith en España, las traducciones y ediciones de la Riqueza de las Naciones y el modo en que eludieron la censura, si bien con significativos recortes y adaptaciones, y la mediación de la obra del economista francés Jean Baptiste Say, cuyos libros de economía política fueron la principal fuente en España para el estudio y conocimiento del liberalismo económico y el individualismo metodológico de Smith. La conclusión del trabajo es un punto de partida abierto a nuevos trabajos sobre el tema, que han de arrojar nueva luz sobre el modo en que el contexto social e histórico influyó decisivamente no sólo en la recepción temporal de esas aportaciones, sino también en la comprensión de las mismas.
“La idea de la Universidad (II temas universitarios tratados en lecciones y ensayos ocasionales)”, de NEWMAN, John Henry.
Authors: Agejas Esteban José Ángel
Published: October 2018

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“El demonio del mediodía. La acedia, el oscuro mal de nuestro tiempo”, de NAULT, Dom Jean-Charles.
Authors: Agejas Esteban José Ángel
Published: October 2018

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“Sin ética no hay desarrollo”, de RODRÍGUEZ MADARIAGA, Óscar A.
Authors: Agejas Esteban José Ángel
Published: October 2018

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“Palabra de Hannah Arendt. Ser o no ser periodista en la era punto cero”, de GUTIÉRREZ DE CABIEDES, Teresa
Authors: Agejas Esteban José Ángel
Published: October 2018

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