Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Yaacov Nathan"'
Publikováno v:
Sedimentology. 60:800-819
Research on the Upper Campanian (Upper Cretaceous) Negev phosphorites (Mishash Formation), based on microprobe analyses, Fourier Transform Infrared spectroscopy, wet chemistry, microtextural (Scanning Electron Microscopy) studies and mineralogical an
Publikováno v:
Israel Journal of Earth Sciences. 54:229-236
Publikováno v:
Chemical Geology. 189:213-230
Study of the U(IV) fraction in Mishash phosphorites of the Negev reveals an apparently paradoxical trend. The U(IV) fraction is very low (less than 10%) in the pristine, organic-rich laminated phosphorites while this proportion considerably increases
Autor:
David Soudry, Yaacov Nathan
Publikováno v:
Sedimentology. 48:723-743
An electron probe and chemical study of bulk phosphorite samples and separated constituents from various Negev deposits was carried out together with XRD, FTIR spectroscopy and textural analysis. The results allow a better understanding of the distri
Publikováno v:
Phosphorus, Sulfur, and Silicon and the Related Elements. 109:51-54
Carbonate removal in the apatite structure was observed at temperatures from 600 to 900°C. The carbonate ions are also partially relocated from the orthophosphate site, into others such as interstitial positions and OH site. Hydroxyl groups form hyd
Publikováno v:
Marine Geology. 129:111-128
Rare earth elements (REE) and major elements have been determined in twenty-nine phosphorite and associated sediment samples from the southwestern coast of Africa, including thirteen samples of unconsolidated sediment collected during recent cruises
Publikováno v:
Geomicrobiology Journal. 11:69-76
Cocci of phosphate‐sequestering bacteria were found in the water column off Namibia where Recent phosphorites are forming. Furthermore, recent work on bacterial populations in the Benguela upwelling system shows that the population that occurs duri
Publikováno v:
Chemical Geology. 97:145-161
In Fe-poor and organic-rich marine sediments, reduced S is mainly organic due to the lack of reactive Fe. These sediments (e.g., carbonates, cherts, phosphates) have high C/S (organic carbon/total reduced sulfur) ratios which are, as a rule, > 3 and
The geochemistry and mineralogy of a condensed section, similar to 6 m thick of the West Kasrik member (Coniacian-Santonian) near the uplifted northern flank of the Mardin-Derik anticline (south-eastern Turkey) was studied. The only deposit exploited
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a99c2f008eb907b77cb751a13c4f687
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/94344
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/94344
Publikováno v:
Estuarine, Coastal and Shelf Science. 30:1-15
The trace metal contamination of estuarine sediments of the Kishon river, running through a large industrial zone of Israel, was studied. The sediments were analysed for trace metal (copper, cadmium, iron, lead, mercury and zinc) contents, organic ma