Representing Atypical Music Notation Practices: An Example with Late 17th Century Music

From the 17th century towards the first decades of the 18th century music notation slowly looses all influences from mensural music, becoming virtually identical to what we would consider common modern notation. But in these five decades of transformation composers did not just suddenly abandon older notation styles, but they were used alongside the ones that would become standard. Void notation, black notation and uncommon tempi were all mixed together. The scholar preparing modern editions of this music is normally forced to normalize all these atypical notations as many software applications do not support them natively. This paper exemplifies the flexibility of the encoding scheme proposed by the Music Encoding Initiative (MEI) and of Verovio, a visualisation library designed for it. The modular approach of these tools means that particular notation systems can be easily added whilst maintaining compatibility to other encoded notations

Verovio: A Library for Engraving MEI Music Notation into SVG

Rendering symbolic music notation is a common component of many MIR applications, and many tools are available for this task. There is, however, a need for a tool that can natively render the Music Encoding Initiative (MEI) notation encodings that are increasingly used in music research projects. In this paper, we present Verovio, a library and toolkit for rendering MEI. A significant advantage of Verovio is that it implements MEI’s structure internally, making it the best suited solution for rendering features that make MEI unique. Verovio is designed as a fast, portable, lightweight tool written in pure standard C++ with no dependencies on third-party frameworks or libraries. It can be used as a command-line rendering tool, as a library, or it can be compiled to JavaScript using the Emscripten LLVM-to-JavaScript compiler. This last option is particularly interesting because it provides a complete in-browser music MEI typesetter. The SVG output from Verovio is organized in such a way that the MEI structure is preserved as much as possible. Since every graphic in SVG is an XML element that is easily addressable, Verovio is particularly well-suited for interactive applications, especially in web browsers. Verovio is available under the GPL open-source license

New study of the 1755 earthquake source based on multi-channel seismic survey data and tsunami modeling

International audienceIn the last years, large effort has been done to carry out multi-channel seismic reflection surveys (MCS) in SW Iberia to locate the active tectonic structures that could be related to the generation of the 1755 Lisbon earthquake and the tsunami. The outcome of these researches led to the identification of a large, compressive tectonic structure, named Marques de Pombal thrust that, alone can account for only half the seismic energy released by the 1755 event. However, these investigations have shown the presence of additional tectonic structures active along the continental margin of SW Iberia that are here evaluated to model the tsunami waves observed along the coasts of Iberia, Morocco and Central Atlantic. In this paper we present a new reappraisal of the 1755 source, proposing a possible composite source, including the Marques de Pombal thrust fault and the Guadalquivir Bank. The test of the source is achieved through numerical modelling of the tsunami all over the North Atlantic area. The results presented now incorporate data from the geophysical cruises and the historical observation along the European coasts and also from the Western Indies. The results of this study will, hopefully, improve the seismic risk assessment and evaluation in the Portuguese territory, Spain, Morocco and Central/North Atlantic

Multiphase tectonic interaction of Tyrrhenian - Tunisia Margin - Ionian systems: Implications for regional seismogenesis

European Geosciences Union (EGU) General Assembly 2020, 4-8 May 2020The region at the transition from the west to the east Mediterranean is a complex puzzle of terrains spanning in age from the Mesozoic Ionian lithosphere to the Pleistocene arc and back arc domains of the Tyrrhenian system. Although the region has had a complicated evolutionary history, the current configuration of terrains fundamentally denotes Miocene to recent kinematics. In this contribution we present new data from Tunisia Margin showing the evolution from its formation in early Miocene to recent, the tectonic interaction with the opening of the Tyrrhenian system and its current inversion, and discuss the implications for the regional kinematics evolution. The Tyrrhenian is no longer extending, but all basin borders indicate currently active large-scale thrusting to strike slip tectonics. Tunisia margins formed by a well-know contractional tectonic phase in early Miocene expressed in large-scale tectonics with a clearly imaged thrust and fold belt, cut by Messinian to Pliocene extensional faulting. However, high resolution multibeam bathymetry and images of the shallowest layers indicates ongoing inversion tectonics. We compare the tectonic evolution of north Tunisia and Tyrrhenian with the patterns of deformation of the Ionian tectonic wedge observed in new and reprocessed seismic images. We interpret the current deformation of the Ionian tectonic wedge based on the integration of evolution of the kinematics from the data sets of observations from the three systems. We conclude that the entire region is currently under collision of the Africa Plate with the Adria Plate and the Neogene terrains of the Tyrrhenian Domain. The corollary is the subduction of the Ionian lithosphere is fundamentally stalled so that the megathrust fault is possibly not any longer accumulating significant shortening and most deformation is currently occurring in steeper faults re-activation or cutting the previous structural framewor

Anatomy and tectonic significance of WNW-ESE and NE-SW lineaments at a transpressive plate boundary (Nubia-Iberia)

Recent mapping of the Gulf of Cadiz seafloor permitted to identify major tectonic lineaments: the SWIM lineaments (Zitellini et al., 2009) and Cadiz lineament, striking WNW-ESE and NE-SW, respectively. Multibeam swath bathymetry and interpretation of multi-channel seismic data indicate that these features can be interpreted to correspond to the seafloor morphological expression of active dextral strike-slip faults. Based on the interpreted data and recently published GPS plate kinematic velocity vectors of Nubia with respect to Iberia and the Alboran block (e.g. Fernandes et al.; 2003 Stich et al., 2006) we propose that the SWIM Faults are related to the general NW-SE convergence of Nubia with respect to Iberia, and the Cadiz fault is related to the westward movement of the Gibraltar orogenic arc

Calibração biostratigráfica das unidades sísmicas da Bacia offshore do Algarve: contribuição do core SWIM04-39

Efectuou-se a calibração estratigráfica das unidades sísmicas mais recentes identificadas na Bacia offshore do Algarve recorrendo à análise biostratigráfica (Nanofósseis calcários e Foraminíferos) do core de pistão SWIM04-39. Obteve-se uma idade de cerca de 4.0 Ma (Pliocénico Inferior, Zancliano) para as associações fitoplanctónica e faunística presente nas amostras do referido core. Estes dados permitiram datar o início da intensa subsidência sofrida por esta Bacia como sendo Pliocénico Inferior