Ovaj rad započinje razvojem etnološkog istraživanja od Maksimilijana Vrhovca pa sve do osnutka Jugoslavenske akademije znanosti i umjetnosti 1866. godine, kad se institucionalizira znanstveno ...proučavanje narodnog života. Spominje se rad Antuna Radića kao glavnog urednika Zbornika za narodni život i običaje Južnih Slavena. Radić je i autor Osnove za sabiranje i proučavanje građe o narodnom životu, popisa uputa za svakog istraživača kako bi se na jedinstven način prikupljala folklorna građa. Jedan od sakupljača folklorne građe koji je pisao po Radićevim uputama bio je i Nikola Novaković, poljodjelac iz Starog Sela pokraj Štefanja. Novaković je suradnju dogovorio još s Radićem, a nastavio ju je s Dragutinom Boranićem. Rukopise je završio 1910. godine. Budući da Novaković o sebi nije pisao u rukopisima, pojedine detalje o njegovu životu saznajemo iz pisama koja je slao Boraniću, a koja su sačuvana u Hrvatskoj akademiji znanosti i umjetnosti. Upravo ta pisma, ali i sjećanja ljudi iz Starog Sela, bit će temelj ovog rada i proučavanja njegova života i rada.
On September 1976 four strong aftershocks with M>5 occurred in the Friuli area (NE Italy) causing more damage with respect to that caused by the M6.4 mainshock that occurred on May 6, 1976. Although ...many studies have been published on the 1976 Friuli seismic sequence, only recently have finite-fault models based on geological considerations (Galadini et al., 2005; Burrato et al., 2008) been proposed for these aftershocks. The aim of our study is to model the September 1976 seismic sources as finite faults by computing finite-fault synthetic seismograms for several possible proposed fault models and nucleation locations. The seismicity distribution following each of the four events gives us some further information about the areal extent of the related fault and its rupture propagation. About 9000 synthetic seismograms are computed for all the tested fault models adopting the reflectivity technique for an upper cutoff frequency of 1Hz. A “trial and error” procedure is used to find the best fit between the recorded and computed peak ground acceleration derived from signals filtered at 1Hz, that identifies the final models. These are selected also on the basis of the existing knowledge of fault traces in the area. The four best-fit models seem to be well related to the main Barcis-Staro Selo fault system, their spatial–temporal sequence evidencing an overall progressive East-to-West migration of the seismic activity related to the 1976 sequence.
► In this study we model the source related to four earthquakes occurred in Friuli on September, 1976. ► We apply a trial and error forward procedure using accelerometric data recorded close the epicenter. ► The retrieved source models are compared with tectonic studies and with aftershocks distribution: good agreement is found. ► We observe a migration of seismicity from East to West during the 1976 Friuli seismic sequence.
The onset of the Jurassic sedimentation in the region of Pernik (southwestern Bulgaria) is at the end of Bajocian with deposition of sandstones (Lyalintsi Member of Gradets Fm.) and continuing during ...the Bathonian with bioclastic limestones (Polaten Fm.). The section Staro selo is one of the most complete Jurassic sections in Southwest Bulgaria. It is studied from several points of view: lithofacial, depositional processes, biostratigraphic and sequence stratigraphic. In Bajocian-Bathonian interval four 3rd order depositional sequences are individualized: Bj 5, Bat 0, Bat 1 and Bat 2. After a break of sedimentation (Callovian-Oxfordian), the limestones of Gintsi (Lower Kimmeridgian) and Drugan (Middle Kimmeridgian) Formation were deposited in which 3 depositional sequences were recognized (Kim 2-Kim 4). Nineteen depositional sequences of 3rd order are individualized (Kim 5-Ti 1.1-Ti 1.13, Ti 2, Ti 3.1-Ti3.2, Ti 4, Ti 5) in the sediments of Neshkovtsi Formation (Upper Kimmeridgian) and in the Bobovo Member of Kostel Formation (Uppermost Kimmeridgian – Upper Tithonian in the studied area). The recognition of the depositional sequences is based chiefly on the geometry and the superposition of the calcareous and siliciclastic sediments. The divided depositional sequences are compared to those of Western European scheme of Hardenbol et al. (1998). Within the carbonate part of the succession they are of the same number and in the siliciclastic part they are more numerous.
U restauriranom stambenoj kući koja se nalazi na samom ulazu u
Muzej Staro selo u Kumrovcu planira se urediti interijer po uzoru
na manje seoske dućane - štacune, iz tridesetih godina 20. stoljeća.
...Budući da je kuća obnovljena prije dvadesetak godina i opremljena
inventarom potrebnim za prodaju suvenira (masivnim stolom za prodaju
robe - pultom, kao i zidnim policama za tekstilnu robu s manjim
pregradama na kojima su trgovci držali različite drvene i glinene posude
sa zrnjem, brašnom ili šećerom), bit će potrebne manje preparatorske
intervencije na postojećoj drvenoj opremi.
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