Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Cs. Sajgó"'
Publikováno v:
Geochem. J. 46, 211-224 (2012)
Copyright © 2012 by The Geochemical Society of Japan. as spectroscopic characteristics was discussed in some studies (Wassenaar et al., 1990; Gron et al., 1996; Artinger et al., 2000). Thurman (1985) studied several properties of HS isolated from Ca
Publikováno v:
Organic Geochemistry. 41:915-923
This paper presents organic geochemical records and a combined interpretation of organic geochemical and palaeoecological data for a late Pleistocene–Holocene shallow lake sequence. Abundance, bulk chemical composition and sources of the organic ma
Publikováno v:
Organic Geochemistry. 37:1931-1942
Abundance, bulk chemical composition and sources of the organic matter in the surface horizon of the permanently water-covered part of an intermittently water-covered marsh were investigated. Lipids, insoluble non-hydrolysable macromolecular organic
Autor:
Cs. Sajgó
Publikováno v:
Organic Geochemistry. 31:1301-1323
Biological marker maturity parameters were used to estimate the minimum HC generation temperatures of crude oils from Eastern Hungary. More than 50 oils and oil shows were analysed. Molecular- and homologous-ratios of biological marker compounds (tri
Organic matter in thermal waters of the Pannonian Basin – a preliminary report on aromatic compounds
Publikováno v:
Organic Geochemistry. 30:701-712
About 50 formation waters, produced from wells tapping the aquifers of the clastic Pannonian Basin and Mesozoic carbonates, were studied by GC–MS for their content of hexane soluble organic compounds. About half of the waters studied are hotter tha
Autor:
A. Brukner-Wein, Cs. Sajgó
Publikováno v:
Organic Geochemistry. 16:219-227
Sedimentary materials for the 2 km Neogene/Quaternary section in the Tiszapalkonya—I corehole, north-eastern Hungary (Pannonian Basin) have been used to study the processes of diagenesis. The age of lignite, coal and sediment samples penetrated ran
Autor:
Cs. Sajgó, Magdolna Hetényi
Publikováno v:
Organic Geochemistry. 16:907-916
Several Hungarian lignite and brown coal samples were studied by coal petrographical, palynological and organic geochemical methods. Three of these were chosen for a series of pyrolysis experiments. Thermal treatment was carried out on two H-rich Eoc
Publikováno v:
Lecture Notes in Earth Sciences ISBN: 3540166459
Three biological marker reactions have been studied in order to determine the temperature — time history of a sedimentary sequence. Two of these reactions are configurational isomerization reactions, at C-20 in a C29-sterane and at C-22 in C31 and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5a73d26a61b26184e54966541a1ee2b
https://doi.org/10.1007/bfb0012106
https://doi.org/10.1007/bfb0012106
Autor:
Cs. Sajgó
Publikováno v:
Organic Geochemistry. 6:569-578
The most important Hungarian oil pools are located around the Mako-Hodmezovasarhely trench. Twenty-five oil samples have been studied from that area. The distributions and relative quantities of alkanes and isoprenoids (C 18 –C 20 ), steranes, trit
Publikováno v:
Organic Geochemistry. 10:331-337
Immature alginite and lignite were compressed into disks and heated at temperatures ranging from 200 to 450°C under pressures ranging from 0.06 to 2.5 kbar in open and in quasi-closed systems for one week. The liquid and solid products of thermal al