Prospecção geoquímica: estaurolita, ilmenita e magnetita como minerais traçadores para depósitos do tipo VMS

A região de Itutinga foi alvo de estudos prospectivos por parte da empresa BP mineração na década de 80, onde foram encontradas mineralizações em lentes de sulfetos metálicos (Zn-Cu-Ag-Fe) associados a rochas komatiíticas peridotíticas e basaltos toleíticos (anfibolitos) do greenstone belts, nas proximidades da fazenda São Jerônimo, enquadrando-se em um depósito do tipo VMS. A partir destas informações encontradas na literatura propôs-se estudar a estaurolita, a magnetita e a ilmenita para, a partir da determinação do seu conteúdo em zinco, indicar a aplicabilidade destes três minerais como traçadores desses tipos de depósitos. Para isso foram coletadas amostras de sedimentos de corrente e concentrados de batéia na região próxima à ocorrência, no entorno da cidade de Itutinga, e também em uma região próxima a cidade de Itumirim, já que existem semelhanças litológicas entre as duas áreas. Os sedimentos de corrente, as frações magnéticas e as frações de 0,3A (separador eletromagnético Frantz) foram enviados para análises químicas por absorção atômica e ICP-OES. Os concentrados de batéia foram descritos, separando-se cristais de estaurolita de cada amostra coletada, e analisando-os em MEV-EDS para determinação da química mineral. Os resultados dos sedimentos de corrente apontaram que os pontos da fazenda São Jerônimo (ME-03, Itutinga 51,7 ppm de Zn) e o ponto do Ribeirão Santa Cruz, (ME-06, Itumirim 36,1 ppm de Zn) foram os que apresentaram melhores resultados, indicando anomalias em zinco nas duas áreas estudadas . As estaurolitas, retiradas dos concentrados de batéia de cada ponto estudado, foram divididas em três conjuntos, de acordo com os teores de ZnO encontrados: 1 - entre 2,96% e 3,25% de ZnO em peso; 2 - entre 2,03% e 2,76% de ZnO em peso; 3 - < 1,67% de ZnO em peso, sendo comparável com outras estaurolitas encontradas em diversos depósitos de Zn do mundo, como Dry River, Austrália e Palmeirópolis Goiás. Assim, as estaurolitas apresentam bons resultados como minerais indicadores na área estudada. Em relação as magnetitas e ilmenitas estudadas, o número de amostras coletadas no presente estudo foram muito pequenas para se ter informações conclusivas sobre o papel destes minerais como traçadores. Por outro lado, os resultados das análises químicas nos concentrados de ilmenita (até 856 ppm de Zn) e nos concentrados de magnetita (até 216 ppm de Zn), indicam a disponibilidade deste metal nas áreas estudadas. Assim, é possível se detectar a presença do zinco por dois meios: através de sedimentos de corrente, através de halos de dispersão química do elemento zinco, e através dos minerais resistatos (estaurolita zincífera, magnetita e ilmenita), a partir de uma dispersão clástica do grão.

Los depósitos de sulfuros masivos vulcanogénicos (VMS) de la cuenca Lancones Piura - Perú

La Cuenca Lancones se encuentra ubicada en la región noroccidental del Perú, en el Departamento de Piura y en el borde oriental de la Franja Costanera, su límite oeste lo constituye el Macizo de Amotapes y hacia el este la región pre-cordillerana de la Cordillera Occidental de los Andes. Esta cuenca se extiende hacia Ecuador, en donde se la ha denominado Cuenca Celica. (Ver Fig. 1) La Cuenca Lancones de acuerdo a las características geológicas, mineralógicas y litológicas debe ser considerada como el principal objetivo en la prospección por yacimientos vulcanogénicos de sulfuros masivos (VMS) en el Perú (Ríos, 2004). Actualmente el yacimiento de Tambo Grande, situado dentro de la Cuenca Lancones, cuenta con tres depósitos de sulfuros masivos (TG1, TG3 y B5), considerados como depósitos de clase mundial (Tegart, 2000).

A new period of volcanogenic massive sulfide formation in the Yilgarn: A volcanological study of the ca 2.76 Ga Hollandaire VMS deposit, Yilgarn Craton, Western Australia

The Archean Hollandaire volcanogenic massive sulfide deposit is a felsic–siliciclastic VMS deposit located in the Murchison Domain of the Youanmi Terrane, Yilgarn Craton, Western Australia. It is hosted in a succession of turbidites, mudstones and coherent rhyodacite sills and has been metamorphosed to upper greenschist/lower amphibolite facies and includes a pervasive S1 deformational fabric. The coherent rhyodacitic sills are interpreted as syndepositional based on geochemical similarities with well-known VMS-associated felsic rocks and similar foliations to the metasediments. We offer several explanations for the absence of textural evidence (e.g. breccias) for syn-depositional origins: 1) the subaqueous sediments were dehydrated by long-lived magmatism such that no pore-water remained to drive quench fragmentation; 2) pore-space occlusion by burial and/or, 3) alteration overprinting and obscuring of primary breccias at contact margins. Mineralisation occurs by sub-seafloor replacement of original host rocks in two ore bodies, Hollandaire Main (~125 x >500 m and ~8 m thick) and Hollandaire West (~100 x 470 m and ~5 m thick), and occurs in three main textural styles, massive sulfides, which are exclusively hosted in turbidites and mudstones, and stringer and disseminated sulfides, which are also hosted in coherent rhyodacite. Most sulfides have textures consistent with remobilisation and recrystallisation. Hydrothermal metamorphism has altered the hangingwall and footwall to similar degrees, with significant gains in Mg, Mn and K and losses in Na, Ca and Sr. Garnet and staurolite porphyryoblasts also exhibit a footprint around mineralisation, extending up to 30 m both above and below the ore zone. High precision thermal ionisation mass spectrometry of zircons extracted from the coherent rhyodacite yield an age of 2759.5 ± 0.9 Ma, which along with geochemical comparisons, places the succession within the 2760–2735 Ma Greensleeves Formation of the Polelle Group of the Murchison Supergroup. Geochemical and geochronological evidence link the coherent rhyodacite sills to the Peter Well Granodiorite pluton ~2 km to the W, which acted as the heat engine driving hydrothermal circulation during VMS mineralisation. This study highlights the importance of both: detailed physical volcanological studies from which an accurate assessment of timing relationships, particularly the possibility of intrusions dismembering ore horizons, can be made; and identifying synvolcanic plutons and other similar suites, for VMS exploration targets in the Youanmi Terrane and worldwide.

Implementación del protocolo de depósitos OK-CASAFE en la Facultad de Ciencias Agrarias de la UCA

Resumen: Los agroquímicos son definidos por FAO como “cualquier sustancia o mezcla de sustancias destinadas a prevenir, destruir o controlar cualquier plaga que perjudique o interfiera en la producción agrícola”. Durante el transporte, almacenamiento y utilización de los mismos se corre el riesgo de sufrir intoxicaciones y de ocasionar daños al medio ambiente. El correcto transporte y seguro almacenamiento y utilización de agroquímicos es un punto clave para minimizar estos riesgos. Existe normativa y programas internacionales que brindan los lineamientos para el correcto almacenamiento de agroquímicos. La República Argentina no posee normativa sobre este tema. Sin embargo existe el Programa de Certificación en Seguridad de Depósitos de Agroquímicos denominado “Depósitos OK” perteneciente a la Cámara de Sanidad Agropecuaria y Fertilizantes (CASAFE). Considerando que una universidad como la Universidad Católica Argentina (UCA) debe ser ejemplo del correcto transporte, almacenamiento y utilización de agroquímicos y ante la ausencia de normativa oficial sobre almacenamiento de agroquímicos; En este trabajo se analizó en forma crítica la implementación del Programa “Depósitos OK” en el depósito de agroquímicos de la Facultad de Ciencias Agrarias (FCA) de la UCA. En base al análisis realizado se elaboraron tres alternativas para la implementación de mejoras en materia de seguridad y calidad de almacenamiento de agroquímicos.

Sistema para la federación de depósitos de datos enlazados

En este proyecto, enmarcado dentro del campo de la web semántica, se ha desarrollado un sistema llamado littera que permite la federación de depósitos de datos enlazados. Dicho sistema permite consultar depósitos del dominio de la literatura de forma unificada a través de una interfaz web, así como construir colaborativamente un nuevo depósito de datos abiertos y enlazados.

Caracterización de los depósitos fluviales del río Ebro en la cuenca de Miranda de Ebro (Burgos)

[ES] La evolución fluvial del río Ebro ha sido analizada de forma desigual, siendo más numerosas las investigaciones centradas en su curso medio y bajo. En este trabajo se describe el sistema de terrazas fluviales elaborado por el río Ebro a su paso por la Cuenca de Miranda de Ebro (Álava – Burgos). Se han reconocido cinco niveles de terrazas (T1-T5) mediante su análisis estratigráfico, morfológico y sedimentológico. Las terrazas se sitúan a unas alturas que oscilan entre los 68 y los 5 m sobre el nivel actual del río Ebro. El relleno sedimentario de los niveles más elevados (T1-T4) está compuesto por gravas poligénicas bien clasificadas y muy redondeadas con presencia puntual de niveles de arenas; mientras que el nivel más bajo (T5) está constituido enteramente por partículas finas. Los resultados apuntan hacia variaciones de caudal y aportes sedimentarios, en relación con las oscilaciones climáticas cuaternarias, como los factores que gobiernan la evolución fluvial en la Cuenca de Miranda de Ebro, en coherencia con los modelos de evolución propuestos para otros puntos de la cuenca hidrográfica

计算机中心资源管理系统：基于VAXRdb/vms数据库的资料介质管理信息系统

本文首先阐述了在中、小型计算机上如何实现管理信息系统。论述了实现信息系统的方法、步骤及有关技术问题，并以计算机中心机房资料介质的管理为例，剖析在编目及外借等诸多业务中的特点，在实现计算机管理中，得到满意结果。其次，本文对VAX 8700计算机上的VAX Rdb/VMS关系数据库管理系统做了较深入的探索与研究，详细分析了VAX Rdb/VMS锁机制，实现了数据库系统中的封锁机构。同时成功地解决了由多用户并发存取数据库而导致的数据库存取产生致命错误问题。圆满地解决了高级语言同排队式打印机之间的通讯问题，从而实现了用FORTRAN语言调用打印机具备的各种功能。分析并实现了软件加密，解决了密码屏蔽和利用高级语言调用DCL命令等问题。

阿尔泰南缘侧向增生过程中的VMS矿床：地质、地球化学特征与成矿机制

The Chinese Altai is one of the most important volcanogenic massive sulfide (VMS) deposit districts in China. All orebodies were lenticular or bedded and stratabounded by a suite of early Devonian volcanic-sedimentary rocks. Hydrothermal feeder zones developed under some of the orebodies. All the ores are massive or laminated, and show typical characteristics of VMS deposit. Based on the mineralizing time and the metal assembles, we divide 3 metallogenic stages: 1, Fe orefroming stage associated with basaltic and sedimentary rocks during very early Devonian; 2, Cu-Pb-Zn oreforming stage associated with rhyolitic and sedimentary rocks during early Devonian; 3， Cu-Zn oreforming stage in the dacitic and basaltic rocks during mid. Devonian. The hosting rocks for all orebodies are different, but they show very similar geochemical and isotopic characteristics. All the felsic rocks show enriched lighted rare earth elements (REE) patterns (La/Yb>5), and with an obvious Eu negative anomalies (Eu/Eu*<0.6). In the meanwhile, all the mafic rocks show flat REE pattern and no Eu anomalies. The Ashele basalt show an apparent Ce negative anomalies (Ce/Ce* <0.76), All the volcanic roks in Chinese Altai show the decoupled property between the high field strength elements (HFSE) and large ion lithophile elements (LILE). The negative Nb, Ta characteristics with respect to adjacent elements indicate that subduction-modified source. The Nd(t) of the hosting rocks for all orebodies changed in a small range (-1.5~5), and the (87Sr/86Sr)i change in a big range. The initial Sr value of the hosting rocks in Mengku and Tiemuerte are obviously affected by the seawater (0.705~0.710), and initial Sr values of hosting rocks Ashele change in a small range (0.704~0.706). All Sr-Nd isotopes of ores have the same range with the hosting rocks, indicating that both the ores and volcanic rocks have the same island arc source. The mean sulfur isotopes of sulfides from Ashele and Mengku are 6.2‰ and 3.4‰, respectively, indicating a deep magmatic source. However, the sulfur isotopes of sulfides from Keketale, Tiemuerte and Keyinbulake changed in -15.8‰~9.9‰, -23.5‰~1.87‰, -8.3‰~1.6‰, respectively. And the big sulfur isotope range indicated that the sulfur of the ores was a combination biogenic and magmatic source. All volcanic rocks from the VMS deposits in the southern Chinese Altai show a typical subduction related environments. Based on the regional and locally geological evidence, here we propose that the southern Chinese Altai is an island arc system, and all VMS deposits formed during the lateral accretion process. No VMS deposit formed during the formation of the island arc during Silurian; Fe VMS deposit formed during the beginning of the opening of the backarc basin in very early Devonian; Cu-Pb-Zn VMS deposits formed during the mature stage of the backarc basin in early Devonian; at last the Cu-Zn VMS deposit formed during the rifted stage of the island arc itself.

Estudo dos depósitos lutíticos da orla ocidental: matérias-primas minerais

Neste trabalho foram efectuados estudos de natureza químico – mineralógica e tecnológica em quatro depósitos sedimentares: Vale Grande, Aguada de Cima, Anadia e Monsarros. Estes estudo permitiram o estabelecimento da coluna tipológica em cada um dos depósitos. No jazigo de Aguada evidencia-se a existência de dois níveis argilosos: a unidade “Barro Negro” de natureza ilito-quartzo-caulinítica (argilas especiais) e a unidade “Argilas de Boialvo” com composição quartzo – ilite – caulinite (argilas comuns). Nos jazigos de Anadia e Monsarros o enchimento argiloso é constituído por argilas compatíveis com as da unidade “Argilas de Boialvo” do jazigo de Aguada, não existindo evidências de deposição de argilas de natureza da unidade “Barro Negro”. Em complemento, foram realizados estudos químicos (elementos menores e Terras Raras) nos diferentes depósitos lutíticos para inferir a importância dos minerais acessórios e argilosos na sua distribuição, de modo a poder determinar-se a sua proveniência. Neste trabalho foi também realizado um estudo de pormenor, de natureza mineralógica (DRX) e química (maiores, menores e Terras Raras), das possíveis rochas-fonte. Perante os resultados obtidos através do estudo mineralógico, químico (elementos maiores, menores e Terras Raras) e, ainda, dos estudos isotópicos Rb-Sr e Sm-Nd, pode inferir-se que o Complexo Xisto-Grauváquico foi a formação geológica que mais material forneceu para a formação dos sedimentos argilosos que ocorrem nas áreas de Vale Grande, Aguada, Anadia e Monsarros. Por último, apresenta-se uma definição para o conceito de argila especial cerâmica, utilizado na gama alta da indústria cerâmica, tendo em consideração o padrão químico, mineralógico e tecnológico.

Paleoalterações e cimentações nos depósitos continentais terciários de Portugal central: importância na interpretação de processos antigos

This paper describes the palaeoweathering, cementation, clay minerals association and other closely related characteristics of central Portugal allostratigraphic Tertiary units (SLD's), that can be used for palaeoclimatic interpretation and palaeoenvironmental reconstruction. Lateral and vertical changes in palaeosols are of value for improving our understanding of the autocyclic and allocyclic controls on sediment acumulation in an alluvial basin, but they can also have stratigraphic importance. In some cases it is concluded that the geomorphological setting may have been more decisive than climatic conditions to the production of the palaeoweathering. During late Palaeogene (SLD7-8), surface and near-surface silicification were developed on tectonically stable land surfaces of minimal local relief under a semi-arid climate; groundwater flow was responsible for some eodiagenesis calcareous accumulations, with the neoformation of palygorskite. Conditions during the Miocene (SLD9-11) were favourable for the smectization of the metamorphic basement and arenization of granites. Intense rubefaction associated with basement conversion into clay (illite and kaolinite), is ascribed to internal drainage during late Messinian-Zanclean (SLD12). During Piacenzian (SLD13) intense kaolinization and hydromorphism are typical, reflecting a more humid and hot temperate climate and important Atlantic fluvial drainage. Later on (Gelasian-early Pleistocene ?; SLD14). more cold and dry conditicns are interpreted, at the beginning of the fluvial incision sage. Silica cementation is identified in the upper Eocence-Oligocene ? (SLD18; the major period of silicification), middle to upper Miocene (SLD10)and upper Tortonian-Messinian (SLD11); these occurrences are compatible with either arid or semi-arid conditions and the establishment of a flat landscape upon which a silcrete was developed.

Relatório de estágio na Caixa Geral de Depósitos

This report will describe the activities undertaken during my internship at the Personnel Department (DPE-UPE4.1) in Caixa Geral de Depósitos (CGD), Lisbon, between September 22, 2014, and February 28, 2015. I consider that it is important to note from the outset i) that the subject of my training was suggested by my supervisor in the DPE and accepted by me; and ii) that the internship consisted essentially of carrying out research and information gathering into the different social systems that coexist within the bank and the application of each legal system in solving concrete situations of the CGD employees. The research and analysis of information was important not only for my study but for the CGD itself, as it enables the department to have such an important matter, full of specific characteristics, condensed into a single document, i.e. this report. This is a complex reality. The various welfare systems differ according to the contractual agreement linking the employee to the employer at the date when the labour contract is signed, and also the unique/singular characteristics of the CGD. In the early stage I started by trying to understand the financial institution and its organization and role and the department where I worked. So I analyzed the CGD Statutes and the legal measures that crystallized the scheme for its employees and I also researched its domestic and international operations. The first month was devoted to the research and analysis of such legislation to understand the creation of the CGD and its path to date. In the second and third months I studied the legal social systems that are applied to different groups of CGD workers. This period was quite important to identify and understand the differences between those regimes of CGD employees as well as the procedure inherent in each case. I highlighted the non-implementation of “the social protection regime of convergence” to the workers of this institution; the differences regarding the allocation of sickness subsidies paid to workers who belong to Social Security and CGA contributors, as well as the enforcement of internal rules to all the workers when a work-related accident happens.Then I focused on to assessing and examining external legislation and several internal regulations in order to obtain solutions to questions raised and situations involving by the workers, in order to understand how the DPE solves these situations. Over the last three months of internship, after this more theoretical work, I began the analysis of concrete situations involving employees carrying out their duties in Portugal and abroad. Some of these situations had been received by the department before the beginning of my internship and others over this period. When I was “working” in the DPE I analyzed “cases” that had been solved and some others without a final solution because they were still in courts. As for the last ones (new cases) I was able to follow their assessment and sometimes their outcome. Some of them became study cases for me. Over these five months of my internship, several cases were analyzed and discussed by legal experts of DPE in which I could participate. I always worked hard. I know that this action contributed to elucidate me about the treatment of the issues, and allowed me to have a direct contact with some workers and be part of a dynamic work team. For these reasons, my internship report is not merely descriptive of activities. It consists of an analysis of rules (legislation) and a regulatory framework of activities and it is also a description of several specific situations solved or in a solution process. Through this work I intend to make known the particular reality of a modern Portuguese financial institution not only because of its importance in our country but also such a large number of employees work here (in Portugal and abroad). I should add that throughout my internship I was allowed to attend conferences, within the scope of the bank in order to get a broader view of some issues related to the daily life of the DPE and the CGD. So, I participated in I Jornadas Bancárias and the Conferência Internacional do Contrato a Termo, given that the CGD is a bank and the DPE deals with legal and labour relations.

Colonización de mosquitos en depósitos artificiales en la zona sur del Area Metropolitana de Monterrey, Nuevo León, México [por] Josefina Cecilia Trujillo García

Tesis (Maestría en Ciencias con Especialidad en Entomología Médica) U.A.N.L.

El beneficiario en materia de depósitos bacarios por Gerardo Garza Valdés

Tesis (Maestría en Derecho Mercantil) U.A.N.L.

Problema de rutas con múltiples depósitos y ventanas de tiempo.

Tesis (Maestría en Ciencias con orientación en Matemáticas) UANL, 2014.