The VRANCEA99 seismic refraction experiment is part of an international and multidisciplinary project to study the intermediate depth earthquakes of the Eastern Carpathians in Romania. As part of the seismic experiment, a 300-km-long refraction profile was recorded between the cities of Bacau and Bucharest, traversing the Vrancea epicentral region in NNE–SSW direction.
The results deduced using forward and inverse ray trace modelling indicate a multi-layered crust. The sedimentary succession comprises two to four seismic layers of variable thickness and with velocities ranging from 2.0 to 5.8 km/s. The seismic basement coincides with a velocity step up to 5.9 km/s. Velocities in the upper crystalline crust are 5.9–6.2 km/s. An intra-crustal discontinuity at 18–31 km divides the crust into an upper and a lower layer. Velocities within the lower crust are 6.7–7.0 km/s. Strong wide-angle PmP reflections indicate the existence of a first-order Moho at a depth of 30 km near the southern end of the line and 41 km near the centre. Constraints on upper mantle seismic velocities (7.9 km/s) are provided by Pn arrival times from two shot points only. Within the upper mantle a low velocity zone is interpreted. Travel times of a PLP reflection define the bottom of this low velocity layer at a depth of 55 km. The velocity beneath this interface must be at least 8.5 km/s.
Geologic interpretation of the seismic data suggests that the Neogene tectonic convergence of the Eastern Carpathians resulted in thin-skinned shortening of the sedimentary cover and in thick-skinned shortening in the crystalline crust. On the autochthonous cover of the Moesian platform several blocks can be recognised which are characterised by different lithological compositions. This could indicate a pre-structuring of the platform at Mesozoic and/or Palaeozoic times with a probable active involvement of the Intramoesian and the Capidava–Ovidiu faults. Especially the Intramoesian fault is clearly recognisable on the refraction line. No clear indications of the important Trotus fault in the north of the profile could be found. In the central part of the seismic line a thinned lower crust and the low velocity zone in the uppermost mantle point to the possibility of crustal delamination and partial melting in the upper mantle. 相似文献
This paper investigates the dual nature of regionalisation between imposed institutionalised territoriality and self-made ‘ad hoc’ collaborative regional arrangements between localities. This involves, as the paper sets out to show, different, but concurrent imagineerings of ‘regions’ to two audiences - within and without a defined region. They are applied to the same territory, albeit with different images and sets of actors for internal (local) and external (national/international) consumption. These developments are examined within the context of the ‘new regionalism’ debate, in particular the notion of a replacement of ‘old’ through ‘new’ regionalism as a sequence. This duality of region making challenges the frequently somewhat simplistic presumption of regions forming as one complete entity, ‘out there’ to compete on a global market. They also have to fight for their recognition internally, but with different arguments, rationales and policies. This means that the possibility of overlapping single purpose ad hoc formed regions, as postulated under the new regionalism, needs to take into account the likelihood of several meanings of one and the same territory. The examples demonstrate that the two possibilities overlap - multi-territoriality and multi-meanings of (new) regionalism. The paper uses the example of post-unification eastern Germany, where in 1990 a completely new set of traditional regions was established, implementing a 1960s-derived western German model. Since this common starting point, strong economic, cultural and geographic differences have emerged, leading not only to policy adjustments, but also changes to the understanding of regionalisation and regional policy, and the actors involved. 相似文献