Effect of oxygenated pore-water on Ankur iron ore, NE Sud

The present work deals with the mineral alterations that have taken place in Ankur iron ore and its associated country rocks, by means of oxygenated pore-water. The investigations were carried out by the electron-scanning microscope. The alteration products involve; goethite, hematite, hydromuscovit...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: El-Kammar A. M.
Osman H. M.
Dokumentumtípus: Cikk
Megjelent: Kőzettan, Ásványtan, Földtan Szeged 1981
Sorozat:Acta mineralogica-petrographica 25 No. 1
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24691
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300 |a 109-116 
490 0 |a Acta mineralogica-petrographica  |v 25 No. 1 
520 3 |a The present work deals with the mineral alterations that have taken place in Ankur iron ore and its associated country rocks, by means of oxygenated pore-water. The investigations were carried out by the electron-scanning microscope. The alteration products involve; goethite, hematite, hydromuscovite, chlorite, kaolinite, dolomite, gypsum and amorphous silica. Some of the alteration products exist in small concentrations that can not be detected by the X-ray diffraction or the chemical analyses of the bulk samples. The alteration mechanisms are believed to be direct response to the stability framework of the primary mineralogical composition and the nature of the pore-water as well. 
650 4 |a Természettudományok 
650 4 |a Föld- és kapcsolódó környezettudományok 
695 |a Kőzettan, Ásványtan, Földtan 
700 0 1 |a Osman H. M.  |e aut 
856 4 0 |u http://acta.bibl.u-szeged.hu/24691/1/mineralogica_025_fasc_001_109-116.pdf  |z Dokumentum-elérés