O som da Sé Patriarcal de Lisboa no final do século XX: os cânticos do Pe. Manuel Luís e os acompanhamentos de Antoine Sibertin-Blanc

A novidade do cerimonial em língua vernácula, resultante do Concílio Vaticano II, levou a uma vasta actividade composicional em todos os países católicos. Em Portugal, e muito especialmente na região de Lisboa, um dos principais protagonistas desta acção foi o Pe. Manuel Luís (1924-81). Apesar de os seus cânticos (em particular, os Salmos Responsoriais) serem actualmente utilizados de norte a sul de Portugal, a actividade do Pe. Manuel Luís esteve centrada em Lisboa, nomeadamente, no contexto das celebrações realizadas na Sé Patriarcal, onde foi inevitável o contacto assíduo com Antoine Sibertin-Blanc (1930-2012), organista daquele templo desde 1965. As harmonizações de Sibertin-Blanc viriam a tornar-se, para os frequentadores da Catedral lisboeta, indissociáveis das melodias do Pe. Manuel Luís.

Palaeomagnetism, rock magnetism and AMS of the Cabo Magmatic Province, NE Brazil, and the opening of South Atlantic

P>Reconstruction of the South Atlantic opening has long been a matter of debate and several models have been proposed. One problem in tracing properly the Atlantic history arises from the existence of a long interval without geomagnetic reversals, the Cretaceous Normal Superchron, for which ages are difficult to assign. Palaeomagnetism may help in addressing this issue if high-quality palaeomagnetic poles are available for the two drifting continental blocks, and if precise absolute ages are available. In this work we have investigated the Cabo Magmatic Province, northeastern Brazil, recently dated at 102 +/- 1 Ma (zircon fission tracks, Ar39/Ar40). All volcanic and plutonic rocks showed stable thermal and AF demagnetization patterns, and exhibit primary magnetic signatures. AMS data also support a primary origin for the magnetic fabric and is interpreted to be contemporaneous of the rock formation. The obtained pole is located at 335.9 degrees E/87.9 degrees S (N = 24; A(95) = 2.5; K = 138) and satisfies modern quality criteria, resulting in a reference pole for South America at similar to 100 Ma. This new pole also gives an insight to test and discuss the kinematic models currently proposed for the South Atlantic opening during mid-Cretaceous.