Segunda encuesta estructural de la pesquer��a artesanal peruana: Regiones Moquegua y Tacna

El presente informe es el primero de una serie de informes sobre los resultados, an��lisis, conclusiones y discusi��n de la Segunda Encuesta Estructural de la Pesqueria Artesanal en el Litoral Peruano (II ENEPA). Tiene por finalidad facilitar al sector pesquero de un conocimiento actualizado de la pesca artesanal.

An��lisi geom��trica del Diaclasat de les Guilleries en el sector de la Vall del Ter entre els embassaments del Pasteral i Susqueda (Girona)

The Guilleries are a small and mountainous area located in the north-westem part of the Catalonian Coastal Ranges where metamorphic and igneous Paleozoic rocks are exposed. After the main hercynian folding this area was affected by a brittle deformation that is mainly manifested by the intrusion of a very large number of dykes of granodiorite and the development of a complex joint system. Trends of dykes indicate that their intrusion was related to a SE-NW extension, whose estimated value is 40% on an average. This extension seems to stand, although without any associated igneous event, with the development of NE-SW directed joints which make the main set. Five families more were developed later, onegently-dipping and fou upright; the latter trending roughly SE-NW, ENE-WSW, ESE-WNW and N-S. AU the joint sets appear in the metasedimentary Paleozoic rocks and in the hercynian intrusive bodies. Concerning the ages, joints that belong to the NE-SW and SE-NW directed sets and also those slightly dipping have been attributed to the late-hercynian times and all the other are considered to be later

Aportaciones al conocimiento de la geolog��a de Bac Grillera (prepirineo, Girona)

The Bac Grillera nappe (Prepirenean of Girona) shows a stratigraphic section composed of two unconformi ty-bounded units. The lower unit is composed by rethian (marly limestones) and liassic (brechoid marly limestones and limestones). The upper unit (sandstones and marly limestones) belongs to the upper Cretaceous (Campanian)

Aportaciones al conocimiento del Cret��cico del macizo del Montgr�� (Girona)

ln this paper we describe a stratigraphic column of the Cretaceous of the Montgr��. This description is based on several partial stratigraphic cross sections as well as on the lithological characterof the different levels and their faunal content, specially megafossils

Morfog��nesis del valle de Sant Miquel de Campmajor

A series of circumstances which converge in a little valley in the province of Girona, result in a peculiar type of morphogenetic evolution and a quite singular mechanical instability of its buttons. Very recent tectonic movements as well as dissolution phenomena of its subsoil due to pressurized underground water have played an important role in the morphogenesis. Such conditions have resulted in a fast morphological evolution which a progressive lowering of the valley floor as well as peculiar morphological features which favour the existence of numerous pits caused by sudden collapses distributed in altitude and time

���AN��LISIS DEL CUMPLIMIENTO e INCUMPLIMIENTO DE LOS PRINCIPIOS DE TRANSPARENCIA Y BUENAS PR��CTICAS DE LA FUNDACI��N LEALTAD EN LAS ONG ESPA��OLAS���

En este trabajo, fueron abordadas la contextualizaci��n de las Entidades Sin Fines Lucrativas (ESFL) u Organizaciones No Gubernamentales (ONG) y sus debidas relevancias en fomentar la confianza de los usuarios. El objetivo de este trabajo consiste en analizar el cumplimento e incumplimiento de los principios de transparencia y buenas pr��cticas de la Fundaci��n Lealtad en las ONG. La metodolog��a empleada, es mediante el programa SPSS estudiando una serie de variables, que pueden dar respuestas a la problem��tica planteada. Tras este an��lisis, nos permite concluir que, existen varios factores causantes del incumplimiento de los principios de transparencia y buenas pr��cticas, que a trav��s de las variables porcentaje de distribuci��n de ingresos p��blicos y privados son, una de las mayores causas del cumplimiento e incumplimiento de estos principios, en parte, afectadas por la crisis econ��mica. Tambi��n se pone en evidencia que los principios menos cumplidos a nivel contable son el 6�� principio (Principio de pluralidad en la financiaci��n) y el 7�� principio (Principio de control en la utilizaci��n de fondos) siendo, las ONG medianas con mayor porcentaje del incumplimiento y ONG muy grandes, micro-ONG con mayor porcentaje del cumplimiento de los principios, de entre ellos las fundaciones con mayor porcentaje del cumplimiento de estos principios

Geolog��a del Montgr��

This paper, fundamentally stratigraphic, is based on the vertical distribution of fauna in sediments which constitute the Montgri Massif. The stratigraphic series is composed of two units: one allochtonous (Mesozoic) and a second one autochtonous (Paleogene). The latter crops out in front of the thrust belt and presents the typical facies described by PALLI (1972). The allochtonous part is formed by the following units (from bottom to top): variegated gypsiferous shales of Keuper age; marls, limestones and dolomites from the Lias (Domerian); gray breccia ted dolomites: supraliassic; and Cretaceous limestones with rare interbeds of calcareous marls and nodular shaly marls. In this unit the Neocomian, Barremian (?), Aptian, Albian, Cenomanian, Turonian (?) and Santonian haven been recognized. Structurally, the Montgri Massif is part of a thrust belt which has been divided into three parts of different development ang age. Both parts are affected by ample synclinal folds of NE-SW directions and fractures of NW-SE orientation. The fractures condition the torrential streams as well as the karstic phenomena present in the Massif. These and the eolian actions are the main causes of the present geomorphology of the Montgri

Contribuci��n al estudio morfolitol��gico del sector costero central del macizo de Begur (Girona)

This paper makes a contribution to the knowledge of the coastal fringe morphology of the ���Macizo de Begur���. A lithological study, macro and microscopic, has been carried out of a variety of a series of metamorphic, plutonic, phyllonianic and effusive rocks

Factores pron��sticos en el tratamiento adyuvante del c��ncer de vejiga

El c��ncer de vejiga es el cuarto tumor m��s frecuente en hombres. En este estudio se recogen 70 pacientes diagnosticados de carcinoma urotelial resecables en el Hospital Germans Trias y Pujol(1994 -2011). El objetivo es analizar que factores pron��sticos determinan la realizaci��n del tratamiento adyuvante.La edad fue un factor pron��stico: menores de 70 a��os alcanzaban una mediana de supervivencia de 77 meses.Pacientes sin afectaci��n ganglionar ten��an una mediana de supervivencia de 77 meses frente a 26 meses (con afectaci��n ganglionar)siendo significativo.La afectaci��n linfovasular tambi��n evidenci�� peor supervivencia siendo significativa.En nuestra serie la quimioterapia adyuvante en c��ncer de vejiga aporta un beneficio cuando existe afectaci��n ganglionar y linfovascular.