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Meyal Field is considered as one of the chief hydrocarbon producing fields in the Potwar Basin, Pakistan. The present research emphasize on the subsurface structures affecting the Mesozoic-Cenozoic successions exclusively foremost reservoir units comprising the Eocene Chor Gali and Sakesar formations. Data from six seismic lines and three wells (aligned with those lines) have been deliberated comprehensively with remarkable and tremendous calibration. Five prominent and imperative reflectors specifically the Permian, Triassic, Jurassic, Paleocene and Eocene successions were interpreted through seismic tactics. Time structure maps were equipped on the basis of two-way travel time (TWT) of the seismic line. Likewise, four isopach maps portrayed the thickness discrepancy of prospective hydrocarbon strata. Structurally, analytical section reveals that the Meyal anticline is a plunging and faulted anticline. The pop-up structure is constrained by back-thrust from the north and fore-thrust from the south, on the dip lines. These maps depicted potential reservoir, demarcate promising site for future hydrocarbon exploration.

A set of architectural elements from the Roman Theatre of Lisbon are described and analysed. These elements stand out for the material they are made of an exotic rock with both colour, composition and heterogeneity very distinct from the local lithotypes. The singularity of these elements is underlined by the fact that they are the only architectural remains recognized in the scenic monument and in the city of Felicitas Iulia Olisipo / Lisboa carved in this type of material. Worth noting, the fact of all these elements having been originally covered with stucco which considering their technical and stylistic features, could be assigned to the constructive moment of the decoration of the scenic monument., Analisa-se um conjunto de elementos arquitetónicos de época romana recolhidos nas intervenções arqueológicas realizadas no teatro romano. Estas peças destacam-se pelo facto de o material em que são elaboradas não ser o biocalcarenito de idade miocénica, empregue em todos os elementos decorativos e estruturais do teatro mas antes um litótipo distinto, pouco homogéneo e exótico, quer na cor quer na composição. A singularidade destes elementos arquitetónicos é sublinhada pelo facto de serem os únicos que se reconhecem no monumento cénico e na cidade de Felicitas Iulia Olisipo / Lisboa realizados neste tipo de matéria-prima. Sublinha- se também o facto de todos estes elementos terem sido originalmente estucados, sendo possível, pelas suas características técnicas e estilísticas, atribuí-los ao primeiro momento construtivo do monumento cénico.

The Sado River Drainage Survey project (2004-2008) was designed to fill a significant gap in our knowledge of the prehistory of Portugal. Southern Alentejo constitutes nearly one third of the total land mass of continental Portugal, but has received comparatively little attention from Palaeolithic archaeologists. Practically nothing was known about the prehistory of the Sado River basin, which includes the southern Alentejo plain, before now. The results of the Sado River Drainage Survey (SRDS) indicate that the Sado River basin was likely occupied at low population densities during the Middle Palaeolithic. There is some evidence for a Lower Palaeolithic presence but little or no evidence of an Upper Palaeolithic occupation. The emerging pattern suggests either an occupational hiatus or a major shift in settlement pattern towards the end of the Middle Palaeolithic. Possible explanations for this pattern, including aridification driven by climate change, are explored here., El proyecto de prospección de la cuenca del río Sado (SRDS), llevado a cabo entre el 2004 y el 2008, se diseñó para suplir la carencia de información concerniente al conocimiento actual de la Prehistoria de Portugal. Aunque la cuenca del río Sado conforma casi un tercio de la superficie continental de Portugal, aún no había recibido la debida atención para el Paleolítico. Antes de este proyecto, prácticamente nada se conocía acerca de la Prehistoria de dicha cuenca, incluyendo la llanura de Alentejo. Nuestros resultados indican una baja densidad de población durante el Paleolítico Medio, rastro de ocupaciones del Paleolítico Inferior y casi ninguna evidencia de ocupaciones asociadas al Paleolítico Reciente. A partir de los datos obtenidos, se desprende un modelo en el que se evidencia que, hacia finales del Paleolítico Medio, hubo una discontinuidad en la ocupación, probablemente asociada a cambios climáticos o del uso del territorio.

Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Ciências Farmacêuticas O principal órgão excretor do organismo humano é o rim. Quando não está em normal ritmo de funcionamento, vai levar ao aparecimento de lesões reversíveis como a insuficiência renal aguda e irreversíveis referentes às lesões na insuficiência renal crónica. Como o transplante renal, nem sempre é uma alternativa viável devido ao escasso número de dadores, é importante uma rápida identificação dos sintomas e diagnóstico da doença renal, com o intuito de impedir a progressão da insuficiência renal. Relativamente à hemodiálise, uma forma de terapia de substituição renal, o seu acesso pode ser por três vias, a fístula arteriovenosa, o enxerto e o cateter. Este último, apesar de estar associado a altas taxas de infeção é utilizado quando não é possível utilizar a fístula arteriovenosa ou então, quando é necessário um rápido acesso à circulação sanguínea. No cateter, é frequente a infeção pela flora comensal do organismo humano e também por microrganismos patogénicos. Esta é a principal limitação do uso de cateter em hemodiálise como acesso vascular. Dentro dos microrganismos que colonizam a superfície dos cateteres destacam-se o Staphylococcus aureus, o Staphylococcus epidermidis, a Pseudomonas aeruginosa e Candida albicans, que estão frequentemente associados a altas taxas de infeção, bem como a formação de biofilmes nas superfícies poliméricas do cateter. O tratamento nem sempre é fácil devido às várias resistências que os microrganismos apresentam contra os antibióticos. Mesmo assim, diversas alternativas vão surgindo para contrariar este facto como o uso de quelantes, antibióticos no lúmen do cateter, etanol e até mesmo o uso de mel. The main excretory organ of the human body is the kidney. When it is not working at a normal pace, will lead to the appearance of reversible lesions on acute renal failure and irreversible lesions on chronic renal failure. As renal transplantation is not always available due to the small number of donors, it is important identify the symptoms and make the diagnosis of kidney disease in order to prevent the progression of renal failure. Concerning dialysis, a form of renal replacement therapy, the vascular access may be from three sources, arteriovenous fistula, the graft and the catheter. The last one despites being associated with high infection rates is used when it is not possible the use of an arteriovenous fistula or, when rapid vascular access to the bloodstream is necessary. In catheter infection is common commensal bacterial flora of the human body, and also by pathogenic microorganisms. This is the main limitation of the catheter as vascular access in hemodialysis. Within the microorganisms that colonize the surface of catheters stand out Staphylococcus aureus, Staphylococcus epidermidis, Pseudomonas aeruginosa and Candida albicans, which are often associated with high rates of infection, as well as the formation of biofilms on polymeric catheter surfaces. The treatment is not always easy due to various microorganisms which exhibit resistance against antibiotics. Even so, several alternatives are emerging to counteract this as the use of chelating agents, antibiotics into the lumen of the catheter, ethanol and even the use of honey.

Notícia explicativa da folha 42-B, Azinheira de Barros, de 2006

The Sado River Drainage Survey project (2004-2008) was designed to fill a significant gap in our knowledge of the prehistory of Portugal. Southern Alentejo constitutes nearly one third of the total land mass of continental Portugal, but has received comparatively little attention from Palaeolithic archaeologists. Practically nothing was known about the prehistory of the Sado River basin, which includes the southern Alentejo plain, before now. The results of the Sado River Drainage Survey (SRDS) indicate that the Sado River basin was likely occupied at low population densities during the Middle Palaeolithic. There is some evidence for a Lower Palaeolithic presence but little or no evidence of an Upper Palaeolithic occupation. The emerging pattern suggests either an occupational hiatus or a major shift in settlement pattern towards the end of the Middle Palaeolithic. Possible explanations for this pattern, including aridification driven by climate change, are explored here.

The Sado River Drainage Survey project (2004-2008) was designed to fill a significant gap in our knowledge of the prehistory of Portugal. Southern Alentejo constitutes nearly one third of the total land mass of continental Portugal, but has received comparatively little attention from Palaeolithic archaeologists. Practically nothing was known about the prehistory of the Sado River basin, which includes the southern Alentejo plain, before now. The results of the Sado River Drainage Survey (SRDS) indicate that the Sado River basin was likely occupied at low population densities during the Middle Palaeolithic. There is some evidence for a Lower Palaeolithic presence but little or no evidence of an Upper Palaeolithic occupation. The emerging pattern suggests either an occupational hiatus or a major shift in settlement pattern towards the end of the Middle Palaeolithic. Possible explanations for this pattern, including aridification driven by climate change, are explored here.

During the last three years geoscientists of various institutions have developed a project aiming the setup of a geoconservation strategy in Portugal (Brilha, 2009). One of the main goals of the project was the establishment of an inventory of the most important Portuguese geosites, under the scientific point of view. In a near future, national authorities will consider this inventory as a technical support for the implementation of nature conservation policies and land-use strategies., Fundação para a Ciência e a Tecnologia (FCT) - PTDC/CTE-GEX76496672006 "Identification, characterisation and conservation of geological heritage : a geoconservation strategy for Portugal"

O presente projecto pretende apresentar um projecto de intervenção psicológica que tem como objectivo reduzir os efeitos associados ao tratamento da quimioterapia em crianças diagnosticadas com doença oncológica. A revisão de literatura revela que em contexto de pediatria se tem usado a técnica da hipnose no tratamento de algumas sintomatologias associadas aos tratamentos oncológicos. No contexto do Serviço de Pediatria, Pediatria Oncológica, do Hospital de Santa Maria, propõe-se intervir em crianças, com idades entre os 6 e os 12 anos, referenciadas com náuseas, vómitos e dor, associadas à intervenção terapêutica da quimioterapia. Como estratégia terapêutica, pretende-se usar a técnica da hipnose, que associada às técnicas de intervenção Médica se espera obter resultados significativos na redução dos efeitos associados ao tratamento de quimioterapia. ABSTRACT: The project presents a strategy that aims to reduce the negative effects associated to chemotherapy in children diagnosed with cancer. The literature revision reveals that hypnosis and image visualization techniques have been used in Paediatric units in the treatment of some symptoms associated to cancer illness. In the Santa Maria’s Hospital the intervention will be done in children between the ages of 6 and 12. These children were refereed of having nauseas, vomiting and pain associated to the medical interventions in chemotherapy. It is to believe that the use of hypnosis techniques associated to medical intervention reduces the negative effects associated to chemotherapy treatment.

Five types of paleo-weathering and carbonate precipitation were recognized in fine-grained deposits of the Alemoa Member, Santa Maria Formation, Middle to Upper Triassic of southern Brazil. The fauna and flora found in these lithologies are important dating tools, but only in a generic way, misleading the time involved in periods of deposition and non deposition. The identified types of deposits are (i) reddish mudstones, with none or little paleo-weathering, (ii) mottled mudstones, with incipient pedogenesis, mainly mottling, destratification, animal and vegetal colonization, (iii) carbonate veins, with more evidences of exposure and root action, (iv) carbonate siltstones/sandstones, where restricted fluvial deposits are cemented by phreatic carbonate, and (v) carbonate nodules and lenses, in which small lenses of a very compact calcrete are at the top and in the center of carbonated siltstone/sandstone beds, distinguished by its crystalinity, hardness and brighter color. The recorded microfacies point to a cyclic variation of the mainly high phreatic level, forming cracks and pedotubules (pedogenesis) filled with carbonate and Fe and Mn oxides (phreatic). The identification of five distinct pedofacies and the stratigraphic correlation in the sedimentary package of the Alemoa Member (base, middle or topmost position) suggest a probable association of paleo-weathering processes and vertebrate preservation. Near channel facies, mainly at the base and top, present smaller exposure periods and higher variations on the phreatic level, and consequently, the best preserved vertebrate fossils. On the other hand, facies which are far from the channel, record more subaerial exposure and more significant phreatic variation, leading to more advanced (although still incipient) paleo-weathering and carbonate precipitation, and to a worst fossil preservation.

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia), Universidade de Lisboa, Faculdade de Ciências, 2020 Submitted by Cristina Manessiez (camanessiez@fc.ul.pt) on 2020-09-03T13:39:40Z No. of bitstreams: 1 ulfc125796_tm_Diogo_Barros.pdf: 11944136 bytes, checksum: 693e15e5cd72cbcb6f17899b719264fd (MD5) Made available in DSpace on 2020-09-03T13:39:51Z (GMT). No. of bitstreams: 1 ulfc125796_tm_Diogo_Barros.pdf: 11944136 bytes, checksum: 693e15e5cd72cbcb6f17899b719264fd (MD5) Previous issue date: 2020

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia) Universidade de Lisboa, Faculdade de Ciências, 2020 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2020-12-09T17:10:37Z No. of bitstreams: 1 ulfc125999_João_Borges.pdf: 2863200 bytes, checksum: 1c66b79d82020ae34404f11a3543bf7c (MD5) Made available in DSpace on 2020-12-09T17:10:50Z (GMT). No. of bitstreams: 1 ulfc125999_João_Borges.pdf: 2863200 bytes, checksum: 1c66b79d82020ae34404f11a3543bf7c (MD5) Previous issue date: 2020

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia) Universidade de Lisboa, Faculdade de Ciências, 2019 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2019-04-02T15:41:07Z No. of bitstreams: 1 ulfc125390_tm_Andrea_Santi.pdf: 4405947 bytes, checksum: 1af2c58816b17bb932b2c5b93f420eeb (MD5) Made available in DSpace on 2019-04-02T15:41:21Z (GMT). No. of bitstreams: 1 ulfc125390_tm_Andrea_Santi.pdf: 4405947 bytes, checksum: 1af2c58816b17bb932b2c5b93f420eeb (MD5) Previous issue date: 2019

Tese de mestrado em Geologia, apresentada à Universidade de Lisboa, através da Faculdade de Ciências, em 2018 Submitted by Cristina Manessiez (camanessiez@fc.ul.pt) on 2018-06-09T10:21:09Z No. of bitstreams: 1 ulfc124459_tm_Cristiana_Esteves.pdf: 69198819 bytes, checksum: 7c17da1eda7cea48983d2ca5f582f072 (MD5) Made available in DSpace on 2018-06-09T10:21:49Z (GMT). No. of bitstreams: 1 ulfc124459_tm_Cristiana_Esteves.pdf: 69198819 bytes, checksum: 7c17da1eda7cea48983d2ca5f582f072 (MD5) Previous issue date: 2018

Intensity modulated particle therapy (IMPT) can produce highly conformal plans, but is limited in advanced lung cancer patients with multiple lesions due to motion and planning complexity. A 4D IMPT optimization including all motion states was expanded to include multiple targets, where each target (isocenter) is designated to specific field(s). Furthermore, to achieve stereotactic treatment planning objectives, target and OAR weights plus objective doses were automatically iteratively adapted. Finally, 4D doses were calculated for different motion scenarios. The results from our algorithm were compared to clinical stereotactic body radiation treatment (SBRT) plans. The study included eight patients with 24 lesions in total. Intended dose regimen for SBRT was 24 Gy in one fraction, but lower fractionated doses had to be delivered in three cases due to OAR constraints or failed plan quality assurance. The resulting IMPT treatment plans had no significant difference in target coverage compared to SBRT treatment plans. Average maximum point dose and dose to specific volume in OARs were on average 65% and 22% smaller with IMPT. IMPT could also deliver 24 Gy in one fraction in a patient where SBRT was limited due to the OAR vicinity. The developed algorithm shows the potential of IMPT in treatment of multiple moving targets in a complex geometry.

Tese de mestrado, Geologia (Geologia Estrutural) Universidade de Lisboa, Faculdade de Ciências, 2017 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2017-06-02T13:46:23Z No. of bitstreams: 1 ulfc121671_tm_Marisa_Barreto.pdf: 41482309 bytes, checksum: 3563455fca19c58832a339419099c0fd (MD5) Made available in DSpace on 2017-06-02T13:46:32Z (GMT). No. of bitstreams: 1 ulfc121671_tm_Marisa_Barreto.pdf: 41482309 bytes, checksum: 3563455fca19c58832a339419099c0fd (MD5) Previous issue date: 2017

Purpose Stereotactic body image guided radiation therapy (SBRT) shows good results for lung cancer treatment. Better normal tissue sparing might be achieved with scanned carbon ion therapy (PT). Therefore an in silico trial was conducted to find potential advantages of and patients suited for PT. Methods For 19 patients treated with SBRT, PT plans were calculated on 4D-CTs with simulated breathing motion. Prescribed single fraction dose was 24 Gy and OAR constraints used for photon planning were respected. Motion was mitigated by rescanning and range-adapted ITVs. Doses were compared to the original SBRT plans. Results CTV coverage was the same in SBRT and PT. The field-specific PTV including range margins for PT was 1.5 (median, 25–75% 1.3–2.1) times larger than for SBRT. Nevertheless, maximum point dose and mean dose in OARs were higher in SBRT by 2.8 (1.6–3.7) Gy and 0.7 (0.3–1.6) Gy, respectively. Patients with a CTV >2.5 cc or with multiple lung lesions showed larger differences in OAR doses in favor of PT. Conclusions Patients receive less dose in critical OARs such as heart, spinal cord, esophagus, trachea and aorta with PT, while maintaining the same target coverage. Patients with multiple or larger lesions are particularly suited for PT.

In wider Adriatic area Late Triassic sediments are known as “Burano formation” consisting of Carnian-Norian evaporitic member and Rethian dolomitic member. Burano formation is better described in the Italian sector of the Adriatic based on more evidences available. Despite sparse Triassic section well&outcrop data on the Croatian side, lithostratigraphic division of Late Triassic is generally in accordance with the “Burano formation”. However, after summarizing Croatian data sets it has been observed that Ladinian-Carnian evaporites of “Vlasta-Komiza” facies seems to be specific for the Croatian side of Adriatic. The objective of this study is detailed facies and source rock characterization of the Triassic sediments of Vlasta-1 and Vlatka-1 wells which were used as starting points for the Burano facies modelling and areal reconstruction. Early to Middle Carnian deposition in the Vlasta-1 well is dominated by subaquatic halite with thin layers of carbonates, anhydrites and clay. Sedimentation took place in relatively large, shallow, enclosed bays or lagoons or in marine areas which due to tectonics and sea level variability remained relatively isolated from the open sea. Supratidal environment was established in Late Carnian where carbonates and anhydrites were deposited in typical regressive sabkha microcycles composed of three members (organic rich carbonates, then early diagenetic dolomites and anhydrites and finally gypsum and anhydrite). Up to the Upper Norian, deposition of carbonate-anhydrite rocks in supratidal environment with established sabkha conditions continued. The youngest part of the late Norian deposition took place in intratidal-supratidal environment with no sabkha conditions. Source rock potential has been recognized in Late Carnian organic rich laminated limestones in Vlasta-1 well within 5400-5600m interval. Analyses showed the autochthonous organic matter with organic matter content from 0.15 to 1.80% (in average 0.83%). Limestones have good to excellent hydrocarbon potential (up to 13 mg HC/g rock). Kerogen is type II to II-S. Organic matter is a mixture of algal, bacterially degraded kerogen and migrated bitumen. Amorphous organic matter changes from lamalginite to dominantly bituminite. Stable carbon isotope values are within range from δ13C -27 to -28‰ in kerogen and from -30 to -31‰ in bitumen. These values are typical for the Triassic rocks and they are generally attributed to the specific algal and bacterial lipids as well as to the anoxic conditions. Biomarker analyses confirmed algal-bacterially origin of organic matter and deposition in the low energy, highly anoxic, lagoonal, carbonate-evaporitic environment. Late Triassic laminated limestones have an excellent generation potential and represent very good to excellent oil-prone source rocks. According to all maturity parameters those source rocks generally reached onset of oil generation. However, only small oil volume was recovered from the same Late Triassic section. Oil is positively correlated with Late Triassic source rock. In Vlatka-1 well few Norian intervals have simmilar source rock characteristics. An attempt has been made to map described source rock horizon in wider Central Adriatic area. Public available Italian well data have been used to complement the Burano formation spatial reconstruction. Despite detailed well&outcrop data analysed, it has to be emphasized that the proposed model is constrained by the variable 2D seismic quality and complex geology with strong Triassic (Late Permian?) halocinetic footprint

Tese de mestrado em Geologia Aplicada apresentada à Universidade de Lisboa, através da Faculdade de Ciências, 2013 Submitted by Cristina Manessiez (camanessiez@fc.ul.pt) on 2013-08-22T10:37:32Z No. of bitstreams: 1 ulfc104409_tm_Angela_Pereira.pdf: 5501753 bytes, checksum: 133c24fa719656a6dc55044c5d037c08 (MD5) Made available in DSpace on 2013-08-22T10:37:43Z (GMT). No. of bitstreams: 1 ulfc104409_tm_Angela_Pereira.pdf: 5501753 bytes, checksum: 133c24fa719656a6dc55044c5d037c08 (MD5) Previous issue date: 2013

Tese de mestrado em Geologia (Estratigrafia, Sedimentologia e Paleontologia), apresentada à Universidade de Lisboa, através da Faculdade de Ciências, 2012 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2013-07-12T14:22:23Z No. of bitstreams: 1 ulfc104224_tm_Bernardo_Teixeira.pdf: 58747360 bytes, checksum: 6c6160ebb846d5666c6ef735d105f8de (MD5) Made available in DSpace on 2013-07-12T14:22:36Z (GMT). No. of bitstreams: 1 ulfc104224_tm_Bernardo_Teixeira.pdf: 58747360 bytes, checksum: 6c6160ebb846d5666c6ef735d105f8de (MD5) Previous issue date: 2012

Tese de mestrado, Geologia Aplicada (Hidrogeologia), Universidade de Lisboa, Faculdade de Ciências, 2010 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2012-04-11T15:10:49Z No. of bitstreams: 1 ulfc100066_tm_Ana_Rita_Diniz.pdf: 30370819 bytes, checksum: 73644d63f61fcc5e711b5b079b2b4d0d (MD5) Made available in DSpace on 2012-04-11T15:11:05Z (GMT). No. of bitstreams: 1 ulfc100066_tm_Ana_Rita_Diniz.pdf: 30370819 bytes, checksum: 73644d63f61fcc5e711b5b079b2b4d0d (MD5) Previous issue date: 2010

Tese de mestrado em Geologia (Estratigrafia, Sedimentologia e Paleontologia), apresentada à Universidade de Lisboa, através da Faculdade de Ciências, 2011 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2013-05-30T14:35:08Z No. of bitstreams: 1 ulfc104143_tm_Elisabete_Malafaia.pdf: 12092678 bytes, checksum: 8f1579da4f8541b3bfc0f4d685a77c3c (MD5) Made available in DSpace on 2013-05-30T14:35:18Z (GMT). No. of bitstreams: 1 ulfc104143_tm_Elisabete_Malafaia.pdf: 12092678 bytes, checksum: 8f1579da4f8541b3bfc0f4d685a77c3c (MD5) Previous issue date: 2011

Tese de mestrado, Ciências da Terra e da Vida para o Ensino, Universidade de Lisboa, Faculdade de Ciências, 2009 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2012-01-20T12:15:05Z No. of bitstreams: 1 ulfc096175_tm_Rita_COsta.pdf: 20857877 bytes, checksum: dee1684f72032a998f50cc5dc09bcd61 (MD5) Made available in DSpace on 2012-01-20T12:15:18Z (GMT). No. of bitstreams: 1 ulfc096175_tm_Rita_COsta.pdf: 20857877 bytes, checksum: dee1684f72032a998f50cc5dc09bcd61 (MD5) Previous issue date: 2009

Tese de mestrado em Geoarqueologia, apresentada à Universidade de Lisboa, através da Faculdade de Ciências, 2010 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2013-04-12T09:25:05Z No. of bitstreams: 1 ulfc103647_tm_Patrícia_Jordão.pdf: 31738707 bytes, checksum: 8a8022f7dcf4e653fc8349550a458272 (MD5) Made available in DSpace on 2013-04-12T09:25:22Z (GMT). No. of bitstreams: 1 ulfc103647_tm_Patrícia_Jordão.pdf: 31738707 bytes, checksum: 8a8022f7dcf4e653fc8349550a458272 (MD5) Previous issue date: 2010

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia) Universidade de Lisboa, Faculdade de Ciências, 2018 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2018-04-05T14:19:29Z No. of bitstreams: 1 ulfc124125_tm_Cátia_Morgado.pdf: 16934088 bytes, checksum: 2091aa97a84237adec080362bb2a8f5b (MD5) Made available in DSpace on 2018-04-05T14:19:38Z (GMT). No. of bitstreams: 1 ulfc124125_tm_Cátia_Morgado.pdf: 16934088 bytes, checksum: 2091aa97a84237adec080362bb2a8f5b (MD5) Previous issue date: 2018

Tese de mestrado em Geologia, apresentada à Universidade de Lisboa, através da Faculdade de Ciências, em 2018 Submitted by Cristina Manessiez (camanessiez@fc.ul.pt) on 2018-12-05T15:44:33Z No. of bitstreams: 1 ulfc121888_tm_Andre_Costa.pdf: 8844536 bytes, checksum: 55a7a71ba7adcbabd157cf265d248377 (MD5) Made available in DSpace on 2018-12-05T15:45:00Z (GMT). No. of bitstreams: 1 ulfc121888_tm_Andre_Costa.pdf: 8844536 bytes, checksum: 55a7a71ba7adcbabd157cf265d248377 (MD5) Previous issue date: 2018

Tese de mestrado em Geologia, apresentada à Universidade de Lisboa, através da Faculdade de Ciências, em 2018 Submitted by Cristina Manessiez (camanessiez@fc.ul.pt) on 2018-11-29T17:44:57Z No. of bitstreams: 1 ulfc121900_tm_Esmeraldina_Custodio.pdf: 9813843 bytes, checksum: 6eaf2df1600b8feddd43e2fdef7035d3 (MD5) Made available in DSpace on 2018-11-29T17:45:10Z (GMT). No. of bitstreams: 1 ulfc121900_tm_Esmeraldina_Custodio.pdf: 9813843 bytes, checksum: 6eaf2df1600b8feddd43e2fdef7035d3 (MD5) Previous issue date: 2018

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia), Universidade de Lisboa, Faculdade de Ciências, 2015 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2015-12-14T15:39:35Z No. of bitstreams: 1 ulfc115892_tm_João_Casacão.pdf: 18551005 bytes, checksum: aa91e5ddac6fbc630b7d4cf79c644088 (MD5) Made available in DSpace on 2015-12-14T15:39:46Z (GMT). No. of bitstreams: 1 ulfc115892_tm_João_Casacão.pdf: 18551005 bytes, checksum: aa91e5ddac6fbc630b7d4cf79c644088 (MD5) Previous issue date: 2015

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia) Universidade de Lisboa, Faculdade de Ciências, 2018 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2018-06-18T14:41:05Z No. of bitstreams: 1 ulfc124390_tm_Sara_Pestana.pdf: 14781039 bytes, checksum: 5e3a9f85c0583cb1b59479582978832c (MD5) Made available in DSpace on 2018-06-18T14:41:17Z (GMT). No. of bitstreams: 1 ulfc124390_tm_Sara_Pestana.pdf: 14781039 bytes, checksum: 5e3a9f85c0583cb1b59479582978832c (MD5) Previous issue date: 2018

Tese de mestrado, Geologia (Estratigrafia, Sedimentologia e Paleontologia), Universidade de Lisboa, Faculdade de Ciências, 2016 Submitted by Teresa Boa (tdboa@fc.ul.pt) on 2016-10-24T15:43:52Z No. of bitstreams: 1 ulfc120484_tm_Eduardo_Máximo.pdf: 11489359 bytes, checksum: 0e4fa084bfc430e5c7349e8e13b53c09 (MD5) Made available in DSpace on 2016-10-24T15:44:24Z (GMT). No. of bitstreams: 1 ulfc120484_tm_Eduardo_Máximo.pdf: 11489359 bytes, checksum: 0e4fa084bfc430e5c7349e8e13b53c09 (MD5) Previous issue date: 2016