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I.

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Author: I.Year: 2008Subject: Mineral Processingclear all
Showing 1-3 of 3 records
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8th International Scientific Conference - SGEM2008
Publication

MINERALS PROPERTIES SELECTION USING AJAX AND WEB SERVICES INTEGRATION

(SGEM Scientific GeoConference, 2008, P. Horovcak, I. Lesso, P. Cirbes)

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Continually and impressive amplification of internet technologies development and implementation enables the creation of productive, efficient, rich useful and interactive web applications. The contribution briefly characterizes a SOA (Service Oriented Architecture), WS (Web Service) and AJAX (Asynchronous JavaScript And XML). The paper illustrates advantages of AJAX and WS integration on application example for interactive selection of one or more minerals according to actual chosen selection criteria. The applic...

Mineral Processing2008
8th International Scientific Conference - SGEM2008
Publication

POLLUTED FUNGI SPECIES IN THE MINING WASTE HILLS CONIFEROUS NURSERIES

(SGEM Scientific GeoConference, 2008, C. Tanase, A. Pui, R. Olaru, V. CLAUDIU Chinan, C. C. BРѕrsan, A. Cojocariu)

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Our investigation regard the distribution of pollutant in the soils degraded by mine activity in the circuit soil-macromycetes. Pollutants categories have been evidenced using FT-IR spectroscopy. Our results underline the macromycetes species extremely flexible capacity to accumulate pollutants of various categories. The distribution of the pollutants in the soil varies from one region to another and depends on the prelevation depth.

Mineral Processing2008
8th International Scientific Conference - SGEM2008
Publication

SEDIMENTOLOGY AND MINERALOGY OF LATE MIOCENE PALEOSOLS AND CALCRETE RICH SEDIMENTS IN THE WESTERN PART OF CENTRAL ANOTOLIAN VOLCANIC PROVINCE (CAVP), TURKEY

(SGEM Scientific GeoConference, 2008, A. Gurel, I. E. Kerey, S. Uzcan)

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The Dogantarla-Aksaray area is situated in western part of the CAVP. This province contains nine (9) different ignimbrite levels, for which a Late Miocene age is indicated by vertebrates as well as K/Ar ages of 11 to 2.8 Ma (Viereck-Goette et al 2006). However, most paleosol and calcrete occur within the interval of 7.6 to 2.8 Ma (Gurel and Kadir, 2006). Among this ignimbrite levels, fluvial and lacustrine sediments are found, so called Bayramhacili Formation of western CAVP consist of alternation of typical red c...

Mineral Processing2008
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