Price Comparison of an Apartment Building in the Cadastral Area of Přerov According to the Valid Valuation Regulations

Cílem této diplomové práce je zjištění a porovnání ceny bytového domu jako celku stanovenou kombinací nákladového a výnosového způsobu ocenění a ceny bytového domu, zjištěnou součtem jednotlivých bytů v tomtéž domě po rozdělení prohlášením vlastníka. V obou případech se jedná o ocenění dle oceňovacích předpisů. Protože se ale v dnešní době oceňuje nemovitý majetek často pro účely úvěrového řízení, uvádím pro přímé srovnání vždy za oceněním dle oceňovacích předpisů odhad ceny právě pro účely úvěrového řízení. Dále se zabývám řešením problematiky výkladu pojmu soubor bytů, který je často používán, ale definován nikde není. Zjistil jsem, že cena součtu jednotlivých bytů dle oceňovacích předpisů, je vyšší o 32% oproti bytovému domu jako celku a při ocenění pro úvěrové řízení, je cena součtu bytů vyšší o 31,4%. Jak je tedy patrné z předchozího souvětí, výše ceny bytového domu se může změnit i pouze změnou způsobu vlastnictví, bez stavebně-technických změn, a to i o 32 %.The aim of this thesis is to determine and compare the price of the apartment building as a whole provided a combination of cost and the valuation of yield and price of the apartment building, found the sum of individual apartments in the same house after the owner of the distribution statement. In both cases it is the valuation according to valuation regulations. But because today is often valued property for purposes of credit control, I will always be the direct comparison of the valuation according to the rules of valuation estimate just for the purposes of credit control. Furthermore, they address the issue of interpreting the concept of a block of flats (lot of flats together in one house), which is frequently used, but is nowhere defined. I found that the total price of flats according to the valuation rules, is higher by 32% compared house as a whole and the award for credit management, the total price of apartments increased by 31.4%. As can be seen from the preceding sentences, the price of the apartment building can be changed only by changing the way property, no construction-technical changes, as well as 32%.

The trace fossil chondrites in uppermost Jurassic-lower cretaceous deep cavity fills from the Western Carpathians (Czech Republic)

The common marine trace fossil Chondrites occurs in thin layers in laminated micrites which fill deep submarine cavities in peri-reefal biocalcarenites and calcirudites of the Tithonian-Berriasian Stramberg Limestone. The cavity fills display several generations which originated during long periods of time. Periodic colonization of this very stressful environment by the Chondrites trace maker was possible probably owing to episodic deposition of more oxygenated and more nutritious sediment at a certain stage of development of the cavities related to increased tectonic activity during the Berriasian. In more bioturbated laminae ?Palaeophycus also occurs. The occurrence of Chondrites in fillings of deep cavities represents new evidence for adaptation of its trace maker to stressful environments

The ichnological record across the Cretaceous/Tertiary boundary in turbiditic sediments at Uzgruň (Moravia, Czech Republic)

The deep-sea, distal turbiditic deposits at Uzgruň have recorded no significant change of trace fossil diversityand ichnofabrics across the Cretaceous/Tertiary (K/T) boundary interval. There is no evidence of any ecological catas-trophe that can be related to the K/T event. The trace fossil association is rather poor in diversity. This can be related toa general oligotrophy and poor preservation potential. The producers of the discussed trace fossils, dominated by Chon-drites intricatus (Brongniart), Chondrites targionii (Brongniart), Ophiomorpha annulata (Książkiewicz), Ophiomorpharudis (Książkiewicz), Palaeophycus tubularis Hall, Planolites isp., Phycosiphon incertum Fischer-Ooster, Thalassinoidesisp. and Trichichnus isp. lived in a habitat, which had not been influenced by the event

ICHNOFOSILIE CRUZIANA PROBLEMATICA VE SVRCHNÍM KARBONU HORNOSLEZSKÉ PÁNVE

Upper Carboniferous trace fossil Cruziana problematica d´Orbigny, 1849 found in the dump of Doubrava mine (Karviná district) is described. This paper is the first report about trace fossils occurence in the Karviná Formation. The producers of these traces were perhaps small arthropods

ICHNOFOSILIE V HORNINÁCH PŘEDPOKLÁDANÉHO SPODNOKAMBRICKÉHO STÁŘÍ VE VRTU MĚNÍN-1 NA JIŽNÍ MORAVĚ

Trace fossils Diplocraterion isp., Skolithos isp. and Planolites isp. were ascertained in drill cores of the Měnín-1 borehole. The cores provided coarse-grained, often variegated sandstones intercalated with shales; they are Lower Cambrian in age according to its acritarch microflora. In the Lower Cambrian, the above-mentioned ichnotaxa occur only in shallow marine settings

Report of 4GEON: A Project of Four Continents Connected Through Playful Geoeducation

IGCP project No. 751 focuses on educational and ‘fun’ aspects of geoconservation, and its first year experienced the exchange of information between the geoparks of Central and Eastern Europe, Asia, South America and Africa. The following are particularly worthy of further elaboration and future efforts: 1) the offer by the geoparks to award local institutions and businesses the "GEO" certificate if they contribute to fun geological education; 2) special excursions through historic towns to look at the origin of the building stones and changes in use over time; 3) targeted cooperation on a personal and project level with the most famous museums in each country; 4) permission for visitors to collect rock samples that would otherwise be lost to natural processes

First Ediacaran (Vendian) cryptarchs from the Měnín-1 borehole (South Moravia)

Unicellular microfossils built by the polymeric organic wall have been detected in so-called basal clastics in southern Moravia. Microfossils have been studied as a palynological residuum, in SEM observation and in thin sections. 30 genera with 40 species have been preliminarily identified. Microfossils are distinguished by an excellent preservation (TAI about 1+) and diversification. Recovered assemblages correspond to the microbial flora of the Meso- and Neo-Proterozoic age.Unicellular microfossils built by the polymeric organic wall have been detected in so-called basal clastics in southern Moravia. Microfossils have been studied as a palynological residuum, in SEM observation and in thin sections. 30 genera with 40 species have been preliminarily identified. Microfossils are distinguished by an excellent preservation (TAI about 1+) and diversification. Recovered assemblages correspond to the microbial flora of the Meso- and Neo-Proterozoic age

Borings of the ichnogenus Gastrochaenolites as a living space of bivalves from the locality Borač-Podolí (Carpathian Foredeep, Czech Republic)

In 2015 the locality Borač-Podolí was newly examined. The locality is situated 8 km NW from the town of Tišnov. A large amount of shallow-water fossils of middle Miocene (Badenian) age was collected. The state of preservation of the material enabled us bivalve borings of ichnogenus Gastrochaenolites which were bored into colonies of hermatype corals and other calcareous hard substrates. In some of these borings, bivalves were found in situ. The borings were determined as Gastrochaenolites isp., Gastrochaenolites orbicularis, Gastrochaenolites lapidicus, Gastrochaenolites dijugus and Gastrochaenolites torpedo. The in situ bivalves were determined as Gastrochaena cf. intermedia, Rocellaria cf. dubia, Hiatella arctica and Cardita calyculata. The first three species probably represent primary borers while Cardita calyculata is probably a secondary user (squatter). Based on an analysis of fossil material, we can assume that borings were created aft er the death of corals during the repeated transport of these bioclasts. It led to colonizing of the whole surface of coral bioclasts. The bioclasts were then moved to deeper water. Transport to water with clay sedimentation enabled the preservation of the bivalves in situ in borings.In 2015 the locality Borač-Podolí was newly examined. The locality is situated 8 km NW from the town of Tišnov. A large amount of shallow-water fossils of middle Miocene (Badenian) age was collected. The state of preservation of the material enabled us bivalve borings of ichnogenus Gastrochaenolites which were bored into colonies of hermatype corals and other calcareous hard substrates. In some of these borings, bivalves were found in situ. The borings were determined as Gastrochaenolites isp., Gastrochaenolites orbicularis, Gastrochaenolites lapidicus, Gastrochaenolites dijugus and Gastrochaenolites torpedo. The in situ bivalves were determined as Gastrochaena cf. intermedia, Rocellaria cf. dubia, Hiatella arctica and Cardita calyculata. The first three species probably represent primary borers while Cardita calyculata is probably a secondary user (squatter). Based on an analysis of fossil material, we can assume that borings were created aft er the death of corals during the repeated transport of these bioclasts. It led to colonizing of the whole surface of coral bioclasts. The bioclasts were then moved to deeper water. Transport to water with clay sedimentation enabled the preservation of the bivalves in situ in borings

SEDIMENTY KARPATU A SPODNÍHO BADENU NA ULICI KOPEČNÁ V BRNĚ

Occasional excavations in the center of Brno enabled observations of Miocene sediments. Karpatian gray calcareous clays contained characteristic marker foraminifers Pappina breviformis and Uvigerina graciliformis. Badenian strata have transgressively overlapped metabazite of the Cadomian Brno Massif. The Badenian sediments consisted of remnant of sands, block accumulation, and overlaying calcareous clays with mollusc and coral fauna. Clastic rocks represent infralittoral facies, calcareous clays circalittoral ones. Miocene sediments are disturbed by landslide of unknown age

LITOFACIE A FOSILNÍ STOPY JEMNOZRNNÉHO TURBIDITNÍHO SYSTÉMU V JIŽNÍ ČÁSTI MORAVICKÉHO SOUVRSTVÍ JESENICKÉHO KULMU, ČESKÝ MASIV

A detailed field facies- and ichnofacies analysis undertaken in the southern part of the Nízký Jeseník Mts. revealed the Moravice Formation of upper Viséan age being composed a relatively uniform, fine-grained siliciclastic turbidite system. At its base proximal, coarse-grained channel deposits with some olistoliths alternate with shales and fine-grained turbidites to form distinct, asymmetric, fining- and thinning upward cycles deposited in the inner- to middle submarine fan environment. Upper, fine-grained parts of the cycles are rich in trace fossils of the Zoophycos (+/- Nereites) ichnofacies. Younger, volumetrically dominant parts of the Moravice Formation include thick successions of shales interbedded with laminae and thin beds of distal turbidites and/or (?) contourites, which accomodate numerous graywacke bodies n x 10 to n x 100 m thick, interpreted as depositional lobes deposited in the outer fan environment. Peripheral parts of the depositional lobes contain abundant trace fossils of Cruziana and Nereites ichnofacies. Anomalous, along-strike persistent occurrence of the proximal, coarse grained clastics and olistoliths at the base of the Moravice Formation indicate a quick change in basin topography to take place approximately at the base of upper Viséan, governed presumably by a compressional tectonic pulse