We Are Not GIL

Cultural practices and events are an occasion to reflect on the space they come to occupy and inhabit\u2014even if temporarily. As it is often the case in Rome, the architecture becomes an overwhelming element to deal with. This year the new location granted by the Region to the performative art festival Short Theatre was the rationalist building of the ExGil\u2014literally former Fascist Youth. After its restoration and reopening the space was renamed as WeGil by the Regione Lazio administration, and is currently used as polyvalent cultural space and venue for exhibitions, arts and culture. Luigi Moretti\u2019s building was inaugurated in 1937, as the space for the fascist organization Giovent\uf9 Italiana del Littorio, and used as such until the end of WWII. This cohabitation couldn\u2019t but trigger a reflection about the building itself and the city at large, their symbols and history. The artistic production of today has the power\u2014and duty\u2014of reshaping and resignifying the matter of collective memory, through its contemporary theories, influences and gestures. Indeed, the considerations that came about necessarily tackled the colonial fascist past of Italian history and geography inasmuch as their tendency to remain incomplete, often laboriously countered by feminist decolonial artistic and educational practices. This issue unfolds through their collective intervention (We) are not Gil, Ilenia Caleo, Isabella Pinto, Federica Giardini and Serena Fiorletta attempt to \u201ccomplete\u201d the historical traces embedded in the ExGil building

Joint inversion of local, regional and teleseismic data for crustal thickness in the Eurasia-Africa plate boundary region

A new map for the Moho discontinuity (EAM02) in the Eurasia-Africa plate boundary region is presented. Reliable results have also been obtained for the southern and eastern Mediterranean Basin, the northern African coasts and the eastern Atlantic Ocean, regions only occasionally considered in studies on the Mediterranean region. The Moho topography model is derived from two independent sets of constraints. Information contained in the fundamental and higher-mode Rayleigh waves obtained from waveform modelling is used to constrain the Moho depth between estimates of crustal thickness taken from published reflection and refraction surveys, gravity studies and receiver function analysis. Strong lateral variations in the Moho topography have been observed in the Mediterranean Sea, confirming the complex evolution of this plate boundary region. In the west, the Moho discontinuity has been found at 15-20 km depth, suggesting extended and, at least in some locations, oceanic crust, while in the east the crust is on average 25-30 km thick. There it is interpreted either as Mesozoic oceanic or thinned Precambrian continental crust covered by thick sedimentary deposits. Standard continental crust (30-35 km) is observed along the eastern part of the northern African coast, while to the west a rapid change from a relatively deep Moho (down to 42 km) below the Atlas Mountain Range to the thin crust of the southwestern Mediterranean Sea has been found. The crust beneath the eastern North Atlantic Ocean can be up to 5 km thicker compared with standard oceanic crust (6 km). The crust has been interpreted to be heterogeneous as a consequence of irregular magma supply at the Mid-Atlantic ridge. In addition, serpentinization of the sub-Moho mantle could contribute to the imaging of apparently anomalous thick oceanic crust. In Europe, the presence of crustal roots (>45 km) beneath the major mountain belts has been confirmed, while thin crust (<25 km) has been found beneath extensional basins. Comparing the obtained Moho topography and Moho depth computed assuming isostatic compensation at 60 km depth shows that most of the Mediterranean and eastern Atlantic region appears to be in isostatic equilibrium. The large positive residuals observed for the eastern Mediterranean are likely to be due to overestimating crustal thickness, owing to the thick sediment deposits presen