Deformational evolution of a Cretaceous subduction complex: Elephant Island, South Shetland Islands, Antarctica

New structural data from Elephant Island and adjacent islands are presented with the objective to improve the understanding of subduction kinematics in the area northeast of the Antarctic Peninsula. on the island, a first deformation phase, D-1, produced a strong SL fabric with steep stretching and mineral lineations, partly defined by relatively high pressure minerals, such as crossite and glaucophane. D-1 is interpreted to record southward subduction along an E-W trench with respect to the present position of the island. A second phase, D-2, led to intense folding with steep E-W-trending axial surfaces. The local presence of sinistral C'-type sheer bands related to this phase and the oblique inclination of the L-2 stretching lineations are the main arguments to interpret this phase as representing oblique sinistral transpressive shear along steep, approximately E-W-trending shear zones, with the northern (Pacific) block going down with respect to the southern (Antarctic Peninsula) block. The sinistral strike-slip component may represent a trench-linked strike-slip movement as a consequence of oblique subduction. Lithostatic pressure decreased and temperature increased to peak values during D-2, interpreted to represent the collision of thickened oceanic crust with the active continental margin. The last deformation phase, D-3, is characterised by post-metamorphic kink bands, partially forming conjugate sets consistent with E-W shortening and N-S extension. The rock units that underlie the island probably rotated during D-3, in Cenozoic times, together with the trench, from an NE-SW to the present ENE-WSW position, during the progressive opening of the Scotia Sea. The similarity between the strain orientation of D-3 and that of the sinistral NE-SW Shackleton Fracture Zone is consistent with this interpretation. (C) 2000 Elsevier B.V. B.V. All rights reserved.

Determinants of bird species richness, endemism, and island network roles in Wallacea and the West Indies: is geography sufficient or does current and historical climate matter?

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Anurans of the sandy coastal plains of the Lagamar Paulista, state of São Paulo, Brazil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Caracterização do clima urbano em Teodoro Sampaio/SP: uma introdução

Este estudo teve como objetivo principal investigar as características da temperatura e umidade relativa do ar intra-urbana e da zona rural próxima a Teodoro Sampaio, SP, cidade de pequeno porte que está localizada a 22º 53' 25 S e 52º 16' 75 W, no extremo Oeste do Estado de São Paulo/Brasil. Para a coleta de dados foram utilizados miniabrigos meteorológicos. Os miniabrigos meteorológicos foram equipados com psicrômetros e distribuídos em sete pontos, sendo seis na área urbana e um na área rural, sendo que as coletas de dados foram realizadas às 7h, 9h, 15h e 21h. As coletas de dados aconteceram em dias representativos de janeiro de 2005 - verão; e em julho de 2005 - inverno. Esse estudo concluiu que Teodoro Sampaio, cidade de pequeno porte com aproximadamente 16.000 habitantes, já possui um clima urbano específico, conseqüência da ocupação do solo e das funcionalidades urbanas, o que acabou gerando para a cidade ilhas de calor e de frescor.

A dissipative Fermi-Ulam model under two different kinds of dissipation

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Gênese, evolução e geomorfologia das ilhas e planície de inundação do alto Rio Paraná, Brasil

Pós-graduação em Geociências e Meio Ambiente - IGCE

Filogeografia de Nasutitermes corniger (Isoptera: Termitidae: Nasutitermitinae) na região Neotropical

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Permian non-marine bivalves of the Falkland Islands and their palaeoenvironmental significance

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Urban heat islands and electrical energy consumption

This study proposes the development of thermal and energy consumption maps to generate useful planning information. A residential neighbourhood in a medium-sized city was selected as the study area. In this area, 40 points were taken as urban reference points where air temperatures at the pedestrian level were collected. At the same time, rural temperatures made available by the city meteorological station were registered. Data of electrical energy consumption of the building units (houses and apartments) were collected through a household survey that was also designed to identify the users' income levels. Then, maps were developed so that the configuration of urban heat islands and electrical energy consumption could be visualised, compared and analysed. The results showed that the income level was the most important variable influencing electrical energy consumption. However, a strong relationship of the consumption with the thermal environment was also observed.

Using phenology to assess urban heat islands in tropical and temperate regions

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)