Thèse (M.sc.A.)- Université du Québec à Chicoutimi, 1981. / "Mémoire présenté en vue de l'obtention du grade de maître en sciences appliquées" CaQCU Document électronique également accessible en format PDF. CaQCU

Mémoire (M. Sc. A. (geologie))- Université du Québec à Chicoutimi, 1982. / "Mémoire présenté en vue de l'obtention d'un diplôme de M.Sc.A. (géologie)" CaQCU Document électronique également accessible en format PDF. CaQCU

Made available in DSpace on 2015-03-13T17:08:18Z (GMT). No. of bitstreams: 1 RielvaSCN.pdf: 3363359 bytes, checksum: 71cc2b344ad3105f66f630bfecb08e76 (MD5) Previous issue date: 1998-05-14 / Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior / The Brasiliano Cycle in the Serid? Belt (NE Brazil) is regarded mostly as a crustal reworking event, characterized by transcurrent or transpressional shear zones which operated under high temperature and low pressure conditions. In the eastern domain of this belt- the so-called S?o Jos? de Campestre Massif (SJCM), a transtensional deformation regime is evidenced by extensional components or structures associated to the strikeslip shear zones. The emplacement of the Neoproterozoic Brasiliano granitoids is strongly controled by these discontinuities. Located in the southern border of the SJCM, the Rem?gio-Pocinhos shear zone (RPSZ) displays, in its northern half, top to the SW extensional movement which progressively grade, towards its southern half, to a dextral strike-slip kinematics, defining a negative semi-flower structure. This shear zone is overprinted upon allocthonous metasediments of the Serid? Group and an older gneiss-migmatite complex, both of which containing metamorphic parageneses from high amphibolite to granulite facies (the latter restricted to the strike-slip zone), defining the peak conditions of deformation. Several granitoid plutons are found along this structure, emplaced coeval with the shearing event. Individually, such bodies do not exceed 30 km2 in outcropping area and are essentially parallel to the trend of the shear zone. Petrographic, textural and geochemical data allow to recognize five different granitoid suites along the RPSZ: porphyritic granites (Serra da Boa Vista and Janda?ra), alkaline granites (Serra do Algod?o and Serra do Boqueir?o) and medium to coarse-grained granites (Olivedos) as major plutons, while microgranite and aluminous leucogranite sheets occur as minor intrusions. The porphyritic granites are surrounded by metasediments and present sigmoidal or en cornue shapes parallel to the trend of the RPSZ, corroborating the dextral kinematics. Basic to intermediate igneous enclaves are commonly associated to these bodies, frequently displaying mingling textures with the host granitoids. Compositionally these plutons are made up by titanite-biotite monzogranites bearing amphibole and magnetite; they are peraluminous and show affinities to the monzonitic, subalkaline series. Peraluminous, ilmenite-bearing biotite monzogranites and titanite-biotite monzogranites correspond, respectivally, to the Olivedos pluton and the microgranites. The Olivedos body is hosted by metasediments, while the microgranites intrude the gneiss-migmatite complex. Being highly evolved rocks, samples from these granites plot in the crustal melt fields in discrimination diagrams. Nevertheless, their subtle alignment also looks consistent with a monzonitic, subalkaline affinity. These chemical parameters make them closer to the I-type granites. Alkaline, clearly syntectonic granites are also recognized along the RPSZ. The Serra do Algod?o and Serra do Boqueir?o bodies display elongated shapes parallel to the mylonite belt which runs between the northern, extensional domain and the southern strike-slip zone. The Serra do Algod?o pluton shows a characteristic isoclinal fold shape structure. Compositionally they encompass aegirine-augite alkali-feldspar granites and quartz-bearing alkaline syenite bearing garnet (andradite) and magnetite plus ilmenite as opaque phases. These rocks vary from meta to peraluminous, being correlated to the A-type granites. Aluminous leucogranites bearing biotite + muscovite ? sillimanite ? garnet (S-type granites) are frequent but not volumetrically important along the RPSZ. These sheet-like bodies may be folded or boudinaged, representing partial melts extracted from the metasediments during the shear zone development. Whole-rock Rb-Sr isotope studies point to a minimum 554��10 Ma age for the crystalization of the porphyritic granites. The alkaline granites and the Olivedos granite produced ca. 530 Ma isochrons which look too young; such values probably represent the closure of the Rb-Sr radiometric clock after crystallization and deformation of the plutons, at least 575 Ma ago (Souza et al. 1998). The porphyritic and the alkaline granites crystallized under high oxygen fugacity conditions, as shown by the presence of both magnetite and hematite in these rocks. The presence of ilmenite in the Olivedos pluton suggests less oxidizing conditions. Amphibole and amphibole-plagioclase thermobarometers point to minimum conditions, around 750?C and 6 Kbars, for the crystallization of the porphyritic granites. The zirconium geothermometer indicates higher temperatures, in the order of 800?C, for the porphyritic granites, and 780?C for the Olivedos pluton. Such values agree with the thermobarometric data optained for the country rocks (5,7 Kbar and 765?C; Souza et al. 1998). The geochemical and isotope data set point to a lower crustal source for the porphyritic and the alkaline granites. Granulite facies quartz diorite to tonalite gneisses, belonging or akin to the gneiss-migmatite complex, probably dominate in the source regions. In the case of the alkaline rocks, subordinate contributions of mantle material may be present either as a mixing magma or as a previously added component to the source region. Tonalite to granodiorite gneisses, with some metasedimentary contribution, may be envisaged for the Olivedos granite. The diversity of granitoid rocks along the RPSZ is explained by its lithospheric dimension, allowing magma extraction at different levels, from the middle to lower crust down to the mantle. The presence of basic to intermediate enclaves, associated to the porphyritic granites, confirm the participation of mantle components in the magma extraction system along the RPSZ. This mega-structure is part of the network of Brasiliano-age shear zones, activated by continental collision and terrane welding processes at the end of the Neoproterozoic / O Ciclo Brasiliano na Faixa Serid? (NE do Brasil) ? considerado principalmete como um evento de retrabalhamento crustal atrav?s de zonas de cisalhamento transcorrentes ou transpressionais operando sob condi??es de alta temperatura e baixa press?o. Na por??o oriental desta faixa, mais especificamente no Maci?o S?o Jos? de Campestre (MSJC), a deforma??o em regime transtracional ? caracterizada atrav?s de um componente ou estruturas extensionais associadas aos cisalhamentos transcorrentes. O alojamento dos corpos granit?ides brasilianos ? controlado fortemente por essas descontinuidades. Localizada na borda sul do MSJC, a Zona de Cisalhamento Rem?gio-Pocinhos (ZCRP) apresenta, na sua por??o norte, movimentos extensionais com topo para SW, que gradam progressivamente a movimento transcorrentes dextrais a sul, definindo uma geometria em meia-flor negativa. Esta estrutura est? implantada sobre metassedimentos al?ctones do Grupo Serid? e um substrato gn?issico-migmat?tico mais antigo, que mostram parag?neses metam?rficas indicativas de condi??es do f?cies anfibolito a granulito (este ?ltimo restrito ao setor transcorrente), durante a atua??o dos cisalhamentos. Acompanhando esta estrutura??o s?o encontrados diversos pl?tons granit?ides com alojamento sincr?nico ao cisalhamentos. Esses corpos n?o ultrapassam 30 km2 de ?rea aflorante e apresentam-se alongados segundo o trend NE da ZCRP. Os dados petrogr?ficos/texturais e geoqu?micos permitiram a divis?o das rochas granit?ides da ZCRP em cinco unidades distintas, representadas por: granitos porfir?ticos (Serra da Boa Vista e Janda?ra), granitos alcalinos (Serra do Algod?o e Serra do Boqueir?o) e granito de textura m?dia a grossa (Olivedos), compondo os corpos de maior expressividade na ?rea, e por sheets de microgranitos e leucogranitos aluminosos Os granitos porfir?ticos encontram-se alojados nos metassedimentos, apresentando formas sigmoidais e en cornue paralelas ao trend da ZCRP, indicando uma cinem?tica dextral. Associados a estes corpos s?o comuns a presen?a de encraves magm?ticos de composi??o b?sica a intermedi?ria, que freq?entemente desenvolvem textura do tipo mingling com os granit?ides hospedeiros. Composionalmente s?o constitu?dos por titanita-biotita monzogranitos com anfib?lio e magnetita, com car?ter peraluminoso e afinidade com as rochas da s?rie subalcalina monzon?tica. Biotita monzogranitos com ilmenita e titanita-biotita monzogranitos, peraluminosos, representam, respectivamente, o pl?ton de Olivedos e os microgranitos. O corpo de Olivedos est? alojado nos metassedimentos, e os microgranitos seccionam o substrato gn?issico-migmat?tico. Por tratar-se de rochas extremamente evolu?das, as amostras desses corpos plotam, nos diagramas discriminantes de s?ries, nos campos dos granitos de fus?o crustal, todavia com um alinhamento tamb?m sugerindo uma afinidade subalcalina monzon?tica. Suas caracter?sticas qu?micas os aproximam dos granitos tipo I. Granitos de afinidade alcalina, claramente sin-tect?nicos, s?o tamb?m reconhecidos na ZCRP. Os corpos de Serra do Algod?o e Serra do Boqueir?o apresentam forma alongadas, paralelas ao cisalhamento que limita o setor extensional, a norte, do setor transcorrente, a sul, sendo que o corpo de Serra do Algod?o apresenta uma estrutura em antiforme isoclinal. Composicionalmente englobam aegirina-augita ?lcali-feldspato granitos e quartzo ?lcali-sienito com granada (andradita), e magnetita + hematita como opacos. S?o rochas variando de meta a peraluminosas, correlacionadas aos granitos tipo A. De ocorr?ncia volum?trica restrita na ZCRP s?o ainda encontrados leucogranitos aluminosos com biotita + muscovita �� silimanita �� granada (tipo S), truncando os micaxistos e o complexo gn?issico-migmat?tico. Estes corpos podem estar dobrados e boudinados, e s?o considerados como produto da fus?o parcial dos metassedimentos, concomitante ? atua??o da ZCRP. Estudos isot?picos pelo m?todo Rb-Sr em rocha total indicam uma idade m?nima de 554 Ma para a cristaliza??o dos granitos porfir?ticos. Os granitos alcalinos e o granito de Olivedos fornecem idades isocr?nicas ca. 530 Ma; este valor, muito jovem, representa a idade de fechamento do sistema Rb-Sr ap?s a cristaliza??o e deforma??o dos corpos, ocorrido a pelo menos 575 Ma (Souza et al. 1998). Os granitos alcalinos e porfir?ticos cristalizaram-se sob condi??es de alta fugacidade de oxig?nio, que ? marcado pela presen?a de magnetita e hematita nestas rochas. A presen?a de ilmenita no pl?ton de Olivedos reflete condi??es menos oxidantes. Termobarometria de anfib?lio e anfib?lio-plagiocl?sio fornece condi??es m?nimas de 750?C e 6 Kbar para a cristaliza??o das rochas porfir?ticas. O geoterm?metro do zirc?nio indica temperaturas mais elevadas, na ordem de 800?C, para os corpos porfir?ticos, e 780?C para Olivedos. Estes dados s?o concordantes com dados termobarom?tricos das encaixantes (5,7 kbar e 765?C; Souza et al. 1998). O conjunto de dados gequ?micos e isot?picos aponta para uma fonte na crosta inferior para as rochas porfir?ticas e os granitos alcalinos. Provavelmente dominam na fonte os gnaisses de composi??o quartzo dior?tico a tonal?tico, em f?cies granulito, do complexo gn?issico-migmat?tico ou equivalentes. No caso das rochas alcalinas, pode ter havido a participa??o, em percentagen subordinada, de material mant?lico mesclado ao magma ou presente na fonte. Para o granito de Olivedos, ortognaisses de composi??o tonal?tica a granodior?tica, com alguma contribui??o metassedimentar, pode ser especulada. A diversidade de rochas gran?ticas na ZCRP ? atribu?da ? sua dimens?o litosf?rica, a qual permitiu a extra??o de magmas a partir de diferentes n?veis na crosta m?dia-inferior at? o manto. A presen?a de rochas de composi??o b?sica-intermediaria, associadas aos corpos porfir?ticos, confirmam a participa??o de componentes mant?licos no sistema de extra??o de magmas ao longo da ZCRP. Essa megaestrutura comp?e a rede de cisalhamentos brasilianos, ativada por processo de colis?o continental e colagem de terrenos ao final do Neoproteroz?ico

Submitted by Automa??o e Estat?stica (sst@bczm.ufrn.br) on 2017-01-03T19:37:12Z No. of bitstreams: 1 TerciaJairesDeOliveiraSilva_DISSERT.pdf: 3790194 bytes, checksum: 2387904bb76aea92d982535fb186e0b2 (MD5) / Approved for entry into archive by Arlan Eloi Leite Silva (eloihistoriador@yahoo.com.br) on 2017-01-05T21:05:00Z (GMT) No. of bitstreams: 1 TerciaJairesDeOliveiraSilva_DISSERT.pdf: 3790194 bytes, checksum: 2387904bb76aea92d982535fb186e0b2 (MD5) / Made available in DSpace on 2017-01-05T21:05:00Z (GMT). No. of bitstreams: 1 TerciaJairesDeOliveiraSilva_DISSERT.pdf: 3790194 bytes, checksum: 2387904bb76aea92d982535fb186e0b2 (MD5) Previous issue date: 2016-02-05 / Este trabalho apresenta modelos de condutividade t?rmica para rochas plut?nicas (dominantemente rochas gran?ticas), utilizados como par?metro de classifica??o entre tipologias de granit?ides. Os modelos de condutividade t?rmica foram aplicados em granit?ides ediacaranos do Dom?nio Rio Grande do Norte-DRN, por??o NE da Prov?ncia Borborema, que tem sido objeto de v?rias propostas de classifica??o tipol?gica. Trabalhos recentes prop?em at? seis diferentes su?tes magm?ticas para o Dom?nio Rio Grande do Norte com base principalmente nas caracter?sticas geoqu?micas de cada grupo, bem como nos aspectos texturais e petrogr?ficos, e este artigo apresenta uma anologia entre a condutividade t?rmica e estas diferentes su?tes/tipologias identificadas no DRN. A condutividade t?rmica foi obtida atrav?s da utiliza??o de modelos te?ricos, baseados em par?metros como composi??o qu?mica e densidade, para as amostras cujos valores de condutividade t?rmica foram medidos experimentalmente. O modelo em s?rie mostrou a melhor correla??o entre as medidas calculadas e experimentais, considerando o erro de 10% que equivale a faixa de erro na medida experimental. A partir desse modelo estimouse as condutividades t?rmicas m?dias para as seis su?tes magm?ticas propostas na literatura para os granitoides ediacaranos do Dom?nio Rio Grande do Norte. Quatro destas su?tes magm?ticas puderam ser diferenciadas a partir da condutividade t?rmica. / The present work shows estimate thermal conductivity for a group of plutonic rocks (dominantly granitic rocks) of part of Borborema Province, and their use as parameter of characterization by different tipology of ediacarans granitoids of Rio Grande do Norte Domain-DRN, NE portion of Borborema Province. For this, the thermal conductivity was obtained by theoretical models (Horai and Baldridge, Hashin Strikman and series model), based on parameters as chemical composition and mineralogy of rocks. Between the tree models used on this study for the group of samples that has experimental data base, the series model was the one that show the more satisfactory results on the reproduction of the experimental conductivity by a estimated conductivity considering a error range of ?10%. From the series model was estimate the thermal conductivities for a group of samples from ediacaran granitoids of DRN, that are grouped on regional literature in six diferents suites: shoshonitic, porphyritic high-K calc-alkaline, equigranular high K calc-alkaline, calc-alkaline, alkaline and charnockitic alkaline. The results obtained shows that this different su?tes could be also differentiated by the thermal conductivity.

Weathering on rocks is an important component of the world’s geomorphology. One way to measure weathering on rocks is to analyse rock hardness. This is a study conducted in the northern hemisphere on granite rocks in Uppsala, Sweden. A Schmidt hammer is used to create a correlation analysis between the aspects on three glacial erratic boulders and rock weathering. Statistics from the Schmidt hammer were then collected and analysed. The results showed a difference between the aspects of the rocks. Although only small differences between the rocks were found, the south and south-east aspects of the rocks were softer and suffered from a more dynamic rock weathering than the north aspects of the rocks. The reason to the more dynamic weathering on the south facing aspects is suggested to be because of a more dynamic thermal stress weathering. The same reason caused the north aspect to have a steeper slope and a more dense lichen cover.

English abstract The thesis is devoted to the interpretation of gravity data in granitic intrusions of Moldanubian Pluton near Kaplice This research was based on gravimetric field measurements taken on two parallel profiles in April 2016. Data from the profiles were then processed and geologically interpreted. Evaluate of derived gravity data showed that the positions of increased gravity field gradient roughly correspond to mapped geological interface. Individual rock types can therefore be distinguished using gravimetry.

In the years 2014-2015 a radiohydrogeochemical survey was carried out in the Tanvald granite body. Tanvald granite is a two-mica granite body located on the southern edge of the Krkonoše-Jizera Pluton, in the Lusatian part of the Saxony and Thuringian zone of the Variscan orogenic belt. The aim of the survey was to find radioactive water, the 222 Rn volume activity of which exceeds 1500 Bq/l. Such water is - under the Act no. 164/2001 Coll. - considered as radioactive mineral water. The result was a found of 20 water sources meeting this condition and many other sources approaching this value. In terms of the findings, the most important area is Dlouhý Most, where 8 of the radioactive water resources exceeding 1500 Bq/l were found. The most important of these is probably the source TGR/11 with the 222 Rn volume activity 2449 Bq/l. A cluster of water sources with a slightly higher conductivity (exceeding 300 µS/cm) appears in the Dlouhý Most area. Chemical analysis of the most important of them (TG1/15) showed that it is water of the Na-Ca-Cl type, probably contaminated by a run-off from the motorway, which is salted in winter. Another important site is the Kokonín fault area. At this important geological structure a total of four springs of radioactive water with the 222 Rn volume activity greater...

Adsorption of radionuclides in granite pores and micropores ABSTRACT This graduation thesis deals with laboratory determination of adsorption isotherms parameters. Granite from the central moldanubian pluton, site Panské Dubenky, Czech Republic, was chosen to the experiment. The place is one of the candidate sites to build a deep nuclear waste disposal. A batch experiment was performed in two modes, differing in the way of addition of radioactive nuclide 90 Sr. From this experiment, distribution coefficients for a linear isotherm or parameters for Langmuir isotherm were obtained. Beside this, a through-diffusion experiment was performed. The objective of this experiment was to identify whether some of the radionuclides used (137 Cs, 90 Sr, 125 I) is able to penetrate through the pores of a granite slice barrier between two solutions of different concentrations. During the period of the experiment no radionuclide was detected reliably.

The Weinsberg Composite Pluton, located in the southern part of the Moldanubian Batholith is a large intrusive body with complex internal fabrics, petrogenesis and emplacement processes. On the basis of geochemistry and zircon morphology classification the dominating lithology in the northeastern part of the pluton seems to be the second type of the Weinsberg granitoids (WbG II). Based on the integration of the structural, petrological and geochemical data set acquired from the investigated area, the interpretation of geodynamic evolution and emplacement of the eastern part of the Weinsberg Pluton could be proposed. This interpretation invokes: (a) indentation and underthrusting of a continental microplate (Brunia) in the east at around ~340-330 Ma, driving mantle delamination and subsequent heating and anatexis in the metapelitic lower crust as the heterogeneous source for Weinsberg- and Eisgarn-types of granitoids; (b) subsequent growth of a large metamorphic dome along the edge of the Brunia indentor followed by polyphase emplacement of entire eastern part of the Moldanubian Batholith around ~330-325 Ma including the Weinsberg Composite Pluton in the south; (c) increasing role of the N-S shortening and associated NW-SE dextral shearing along localized shear zones which caused the prevailing...

Made available in DSpace on 2015-03-13T17:08:10Z (GMT). No. of bitstreams: 1 ArmandoBA_capa_ate_secao4.pdf: 2383600 bytes, checksum: 836bd7af04d38167d27d6747f1b94787 (MD5) Previous issue date: 2006-03-30 / The study area islocated in the northern cost of Rio Grande do Norte State, preciselyin a west zone of Apodi-Mossor? River, inclunding Tibau City, Grossos City and part of Mossor? City. Geologicaly, this area is composed by rokcs of Potiguar basin, represented by Cretaceous, Tertiary and Quaternary sediments. This area is characterizer by the intense action of cosatal processes (eolic and costal tranports, generalized erosion, alteration in the sediments balance and coast modification), reponsable for it?s morfological instability, also the antropic interference, where the iol industry is located, next Mossor? City, and also the salt exploration industry and the tendency of expantion of shrimp cultivation. This report had as objective the multitemporalgeoenvorimentalmonitoring of the region by recognizingin the field and analizingimages of orbital sensors of diferents years of last four decades. This analisys was achieved by Digital Images Procesing (DIP) thecnics, com subsidized, in a GIS, the preparion of Thematic Maps of natural resources (Geology, Geomorphology and Use & Ocupatios of Earth) and the Envorimental Sensivity to Oil Spilling, main objective os this project. Such technics constitute important tools of envoriment monitoring and maneging, indicating tendencies of antropic of natural growing, making possible the apropiated planning of development of the region, where the steps can be indicated minimized possibles envorimental impacts caused by antropics interferencies on the region, mainly those related to industrial activities, and oil industry above all. Researchs of this nature are very important to the analisys and ordered manegements of use and ocupation of coastal places / A ?rea estudada encontra-selocalizada na por??o costeira do litoral setentrional do estado do Rio Grande do Norte, mais precisamente numa zona ? oeste do Rio Apodi-Mossor?, englobando os Munic?pios de Tibau, Grossos e parte de Munic?pio de Mossor?. Geologicamente esta ?rea ? constitu?da por litotipos da Bacia Potiguar, representados por sedimentos cret?ceos, terci?rios e quatern?rios. ? caracterizada pela intensa a??o de processos costeiros (transporte litor?neo e e?lico, eros?o generalizada, altera??es no balan?o de sedimentos e modifica??es na linha de costa) respons?veis por sua instabilidade morfol?gica, al?m da interfer?ncia antr?pica, destacando-se a presen?a da ind?stria petrol?fera nas proximidades da Cidade de Mossor?. Pode-se ainda citar a explora??o salineira e a forte tend?ncia de expans?o da carcinicultura. Este trabalho objetivou o monitoramento geoambiental mutitemporal da regi?o por meio do reconhecimento de fei??es de campo e da an?lise de imagens de sensores orbitais de diferentes datas das ultimas quatro d?cadas. Esta an?lise se deu atrav?s de t?cnicas de Processamento Digital de Imagens, as quais subsidiaram, em um SIG, a elabora??o de Mapas Tem?ticos dos recursos naturais (Geologia, Geomorfologia e Uso e Ocupa??o do Solo) e de Sensibilidade Ambiental ao Derramamento do ?leo, principal objetivo deste trabalho. Tais t?cnicas constituem importantes ferramentas ao monitoramento e gerenciamento ambiental, denotando tend?ncias de crescimento antr?pico e natural, possibilitando o planejamento adequado para o desenvolvimento da regi?o, onde medidas poder?o ser apontadas para minimizar poss?veis impactos ambientais causados por interfer?ncias antr?picas na regi?o, principalmente ?quelas relacionadas ?s atividades industriais, sobretudo relacionadas ? industria do petr?leo. Estudos dessa natureza s?o de vital import?ncia na an?lise e gerenciamento ordenado do uso e ocupa??o dos terrenos costeiros