Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

Wyszukujesz frazę "Karwowski, L." wg kryterium: Autor


Tytuł:
Sołtmany meteorite
Autorzy:
Karwowski, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/411492.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
meteorite
ordinary chondrite
L6 chondrite
meteorite fall
hammer meteorite
Warmia-Masuria Province
Sołtmany village
Opis:
This paper presents the results of a mineralogical and petrological study of the Sołtmany meteorite, which fell on April 30, 2011 in northern Poland. The meteorite was found almost immediately after it fell and has been little altered by weathering. Sołtmany is not the only observed fall of an L6 chondrite over Europe in the past few years. The preceding fall of this type, Jesenice (Slovenia), was also witnessed in April of 2009. However, it was not until several weeks after the fall that the first specimen of Jesenice was found, whereas Sołtmany was collected after a few minutes and submitted for analysis within a couple of days. The author presents mineral and petrographic features and chemical characteristics of mineral phases in Sołtmany. The mineral components are represented by metallic phases (kamacite, taenite, tetrataenite, native copper), as well as chromite, olivine, low and high-calcium pyroxene, feldspar, chlorine-bearing apatite, and merrillite. This study also describes the texture of the meteorite and takes notice of a low number of preserved chondrules and the presence of oval chondrule like areas, which exhibit a metamorphosed, recrystallized texture. Sołtmany was classified as an L6 ordinary chondrite with a weathering grade of W0. A shock stage S2 was determined on the basis of undulose extinction and lack of planar fractures in olivine crystals.
Źródło:
Meteorites; 2012, 2, No. 1-2; 15-30
2299-0313
2299-1220
Pojawia się w:
Meteorites
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Polymetallic mineralization in Ediacaran sediments in the Żarki-Kotowice area, Poland
Autorzy:
Karwowski, Ł.
Markowiak, M.
Powiązania:
https://bibliotekanauki.pl/articles/2086528.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
Małopolska Block
ore mineralization
cobaltite
nickeline
wolframite
Opis:
In one small mineral vein in core from borehole 144-Ż in the Żarki-Kotowice area, almost all of the ore minerals known from related deposits in the vicinity occur. Some of the minerals in the vein described in this paper, namely, nickeline, hessite, native silver and minerals of the cobaltite-gersdorffite group, have not previously been reported from elsewhere in the Kraków-Lubliniec tectonic zone. The identified minerals are chalcopyrite, pyrite, marcasite, sphalerite, Co-rich pyrite, tennantite, tetrahedrite, bornite, galena, magnetite, hematite, cassiterite, pyrrhotite, wolframite (ferberite), scheelite, molybdenite, nickeline, minerals of the cobaltitegersdorffite group, carrollite, hessite and native silver. Moreover, native bismuth, bismuthinite, a Cu- and Ag-rich sulfosalt of Bi (cuprobismutite) and Ni-rich pyrite also occur in the vein. We suggest that, the ore mineralization from the borehole probably reflects post-magmatic hydrothermal activity related to an unseen granitic intrusion located under the Mesozoic sediments in the Żarki-Pilica area.
Źródło:
Mineralogia; 2012, 43, 3/4; 199--212
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New moldavites from SW Poland
Autorzy:
Brachaniec, T.
Szopa, K.
Karwowski, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/138869.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
moldavites
tektites
ries
fluvial transport
Miocene
Polska
mołdawit
tektyty
transport rzeczny
miocen
Polska
Opis:
Four newly discovered moldavites from the East and West Gozdnica pits, SW Poland, are characterized. All specimens, including other four, reported earlier, are from Upper Miocene fluvial sediments of the Gozdnica Formation. Their weight varies between 0.529 and 1.196 g. The moldavites are bottle green in colour and have bubbles and inclusions of lechatelierite. Low degree of corrosion suggests short river transport, apparently eastward from Lusatia.
Źródło:
Acta Geologica Polonica; 2016, 66, 1; 99-105
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The first Polish tektites: preliminary SEM investigation
Autorzy:
Brachaniec, T.
Szopa, K.
Karwowski, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/100790.pdf
Data publikacji:
2013
Wydawca:
Uniwersytet Śląski. Wydział Nauk o Ziemi
Tematy:
tektyt
mołdawit
Dolny Śląsk
Polska
tektite
moldavite
strewn field
crater
Ries
Polska
Opis:
In Lower Silesia, the first Polish moldavites were discovered. To recognize the primary chemical composition and check the morphology of investigated material SE and BSE images were used. The samples show presence of vesicles, which are one of the most typical features of tektite glass. Referring to the preliminary EDS results and comparing them with literature data, it can be assumed that in all cases the base material for all known moldavites was the same.
Źródło:
Contemporary Trends in Geoscience; 2013, 2, 1; 18-21
2299-8179
Pojawia się w:
Contemporary Trends in Geoscience
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
SEM studies of ore minerals in skarns from Garby Izerskie, Karkonosze-Izera block, south-western Poland
Autorzy:
Rybicki, M.
Karwowski, Ł.
Banasik, K.
Powiązania:
https://bibliotekanauki.pl/articles/100745.pdf
Data publikacji:
2013
Wydawca:
Uniwersytet Śląski. Wydział Nauk o Ziemi
Tematy:
Karkonosze
SEM
bizmut
Garby Izerskie
bismuth telluride
acanthite
native bismuth
native gold
native silver
skarns
Opis:
In “Stanisław” quarry, that is located on Garby Izerskie, ore minerals-bearing calcsilicate skarns were found in 2009. The samples were studied using microscopical method of reflected light and scanning electron microscopy (SEM). Based on SEM study, the predominant ore minerals in investigated samples are chalcopyrite, pyrrhotite, bismuth telluride and native bismuth. Moreover, acanthite, native gold and native silver were also identified. Our studies are the first report of above mentioned minerals from the Garby Izerskie area.
Źródło:
Contemporary Trends in Geoscience; 2013, 2, 1; 61-66
2299-8179
Pojawia się w:
Contemporary Trends in Geoscience
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spherules associated with the Cretaceous–Paleogene boundary in Poland
Autorzy:
Brachaniec, T.
Karwowski, Ł.
Szopa, K.
Powiązania:
https://bibliotekanauki.pl/articles/139277.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cretaceous-Paleogene boundary
Polska
Spherule
microkrystites
impact origin
Ni-rich spinels
smectite
kreda
paleogen
granica
Polska
geneza uderzeniowa
smektyty
Opis:
The succession of the Lechówka section near Chełm in south-eastern Poland presents the first complete record of the Cretaceous–Paleogene (K–Pg) boundary in Poland. Samples of the boundary clay were examined for microtektites and shocked minerals to confirm the impact origin of the sediment. The spheroidal fraction reveals morphological and mineralogical features, e.g., spherules, similar to material from the K–Pg boundary as described from elsewhere. The impact genesis of the spherules is confirmed by the presence of nickel-rich spinel grains on their surfaces. The spinels are considered to be primary microlites and, thus, the spherules at Lechówka can be classified as microkrystites. No shocked minerals were noted. The deposits with spherules comprise Aland Mg-rich smectite (Cheto smectite). This almost pure Mg-rich smectite, forming up to 100% of the clay fraction, derived from the weathering of the impact glass. It is proposed that the spherules isolated from the Cretaceous-Paleogene boundary clay at Lechówka come from the Chicxulub crater in Mexico.
Źródło:
Acta Geologica Polonica; 2014, 64, 1; 99-108
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Kamienie żarnowe do rozcierania rud ze stanowiska nr 8 w Dąbrowie Górniczej - Łośniu
Ore-grinding quern-stones found at site no. 8 in Dąbrowa Górnicza - Łosień
Autorzy:
Garbacz-Klempka, A.
Karwowski, Ł.
Rozmus, D.
Powiązania:
https://bibliotekanauki.pl/articles/122179.pdf
Data publikacji:
2016
Wydawca:
Politechnika Wrocławska. Wydział Geoinżynierii, Górnictwa i Geologii. Instytut Górnictwa
Tematy:
hutnictwo wczesnośredniowieczne
hutnictwo srebra
hutnictwo ołowiu
archeometalurgia
kamienie żarnowe do mielenia rudy
produkcyjne stanowisko archeologiczne Dąbrowa Górnicza-Łosień st 8
ore-grinding quern-stones
early medieval metallurgical settlement in Dąbrowa Górnicza-Łosień
archaeometallurgy
early medieval smelting of lead
early medieval smelting of silver
X-ray fluorescence
spectrometry
XRF
petrographic research
Opis:
Przedstawiony komunikat jest pierwszym opracowaniem kamieni żarnowych znalezionych we wczesnośredniowiecznej (druga polowa XI w oraz druga połowa XII w.) osadzie hutniczej w Dąbrowie Górniczej – Łośniu, związanej z wydobyciem i wytopem ołowiu i srebra. Wybór kamieni żarnowych został poddany badaniom petrograficznym, a dwa zabytki kamienne zbadano metodą spektroskopii fluorescencji rentgenowskiej (XRF) pod kątem obecności na powierzchni kamieni pierwiastków metalicznych. Jak stwierdzono ślady pierwiastków metalicznych obecne są w grudkach materiału obcego w stosunku do struktury kamienia, „wprasowanych” w istniejące w kamieniach żarnowych pory. Podsumowując można stwierdzić, że pochodzące z warstw wczesnośredniowiecznych (druga połowa XI do drugiej połowy XII w.) kamienie żarnowe oznaczone jako zabytek 166/III/w. 31 oraz zabytek 139/IX w. 92 służyły do mielenia rudy. Świadczy o tym zestaw pierwiastków charakterystycznych dla rudy cynku i ołowiu z domieszką srebra odkrytych w porach kamienia żarnowego. Gdyby to była glejta (PbO) nie stwierdzono by śladów cynku i srebra. Kamienie żarnowe odkryte w warstwach średniowiecznych związanych z pochodzącym z przełomu XIII / XIV w. dworem, mogły natomiast służyć do mielenia zboża na mąkę.
The following notice constitutes the first treatment of quern-stones found in the early medieval (second half of the 11th c. and the second half of the 12th c.) metallurgical settlement in Dąbrowa Górnicza-Łosień, associated with the extraction and smelting of lead and silver. A selection of the quern-stones was subjected to petrographical research, and two stone monuments were examined by means of X-ray fluorescence spectrometry (XRF) in order to seek the presence of metallic elements on the surface of the stone. It was established that traces of metallic elements occur in the lumps of material which is alien in reference to the structure of the stone. These traces are “ingrained” in the pores of the quern-stones. In conclusion, one may state that the quern-stones derived from early medieval strata (second half of the 11th c. until the second half of the 12th c.) marked as monument 166/III/w. 31 and monument 139/IX w. 92 were used to grind ores. Testimony to this is furnished by the set of elements peculiar to zinc and lead ore with admixtures of silver that were found in the pores of a quern-stone. If this were massicot (PbO), no traces of zinc or silver would have been found. The quern-stones discovered in the early-medieval strata associated with the court dating back to the turn of the 14th century may have been used to grind wheat into flour.
Źródło:
Hereditas Minariorum; 2016, 3; 177-191
2391-9450
2450-4114
Pojawia się w:
Hereditas Minariorum
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Origin of parautochthonous Polish moldavites : a palaeogeographical and petrographical study
Autorzy:
Szopa, K.
Badura, J.
Brachaniec, T.
Chew, D.
Karwowski, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/191842.pdf
Data publikacji:
2017
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Polish tektites
redeposition
river terrace
Miocene
Pleistocene
drainage basin
Opis:
In this article, the most recent moldavite discoveries in Poland and their host sediments are characterised and discussed. They were discovered at Lasów, located about 8 km north of Zgorzelec (Poland) and Görlitz (Germany), about 700 m from the Polish-German border, close to the Lusatian Neisse (Nysa) River. The tektites were collected from Vistulian (Wiechselian) glacial age sand and gravel of a closed quarry pit, associated with the river terraces. In the Lasów area, the moldavite-bearing sediments are Pleistocene in age and represent Lusatian Neisse terrace deposits. They were redeposited from the upper part of the drainage basin of the Lusatian Neisse, probably washed out from the Miocene sediments that filled the Zittau Depression, the Berzdorf–Radomierzyce Depression, the Višňová Depression and the tectonically uplifted Izera Mts. and Działoszyn Depression. The erosion of Miocene deposit occured on a large scale in the uplifted foothills of the Upper Miocene Izera, Lusatia and Kaczawa complexes. The sediment cover was removed from the Działoszyn Depression. The drainage basin of the Lusatian Neisse is the area where moldavites were formed by the Nördlinger Ries impact. The source area of moldavite is the same for the Miocene deposits around Gozdnica, as well as for the Pleistocene sediments at Lasów.
Źródło:
Annales Societatis Geologorum Poloniae; 2017, 87, 1; 1-12
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Using maritime simulation systems to present complex information in maritime museums
Autorzy:
Gucma, L.
Przywarty, M.
Budzan, T.
Karwowski, L.
Vidmar, P.
Hribar, U.
Powiązania:
https://bibliotekanauki.pl/articles/135388.pdf
Data publikacji:
2016
Wydawca:
Akademia Morska w Szczecinie. Wydawnictwo AMSz
Tematy:
maritime simulation
solar compass
Viking navigation
Decca system
sciences centre
navigational systems
Opis:
The paper presents the stages of creation of an autonomous historical navigational system simulator working both in real and accelerated time. The simulator allows performance of navigation tasks from the time of the ancient Vikings, as well as to fix a position by using the Decca system on a real Mk21 receiver recreated to cooperate with the artificial Decca system model. The Viking solar compass discovered on Wolin Island in 2013 was the trigger for creating such a simulator as part of a broader exhibition of navigational systems and tools. The main intention of the exhibition is to demonstrate the hyperbolic navigation application that links both systems.
Źródło:
Zeszyty Naukowe Akademii Morskiej w Szczecinie; 2016, 45 (117); 75-81
1733-8670
2392-0378
Pojawia się w:
Zeszyty Naukowe Akademii Morskiej w Szczecinie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New finds in the Morasko meteorite preserve, Poland
Autorzy:
Karwowski, Ł.
Pilski, A. S.
Muszyński, A.
Arnold, S.
Notkin, G.
Gurdziel, A.
Powiązania:
https://bibliotekanauki.pl/articles/411482.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
iron meteorite Morasko
new finds
strew nfield
Opis:
In result of searching in the Morasko preserve for the documentary series Meteorite Men two irons were found below ground. A 544-g shrapnel-like with weak shock deformations, mildly weathered, at low depth, and 34-kg individual, with its upper surface 156 cm deep, with a thick shell of clay and weathering minerals. Of particular interest is presence of chukanovite, a mineral discovered in the Dronino iron meteorite. Morasko is the second meteorite, where chukanovite could be found. The recovery of a new specimen so much deeper than the previous depth record, suggests that further, more detailed surveys should be conducted in the future with improved metal detecting equipment. Moreover, the larger specimen was found embedded in a Miocene clay, which demonstrates that it fell from the sky at that exact spot and was not deposited in glacial terminal moraine.
Źródło:
Meteorites; 2011, 1, 1; 21-28
2299-0313
2299-1220
Pojawia się w:
Meteorites
Dostawca treści:
Biblioteka Nauki
Artykuł

Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies