A life story..


As a professional geological engineer with thirty years in the mining industry, I have geological,geochemical and mining
experience,managerial skill and an important background in research techniques and training of technical personnel.

I have been working as a Mining Geologist for many years.I am currently providing tecnical consultancy service.

In the early years of my profession, I worked as a geologist for two years in the German-Prakla-Seismos company (TPAO's seismic support team in the salt lake).

My second work experience started by working in ground drilling in the Kozlu Tunnels area in Yüksel Proje.

Next geothermal resources with GE Energy company, I worked in Turkey and Italy in the oil and gas seismic crews.

Then I worked on Onyx Marble and Chromite in Afghanistan.

I did geological mapping and geochemistry, mine geology in the Lead,Zinc,Barite,Fluorite fields (Akdağmadeni-Yozgat) in the Akdağmadeni-Yukarıçulhalı region.

I have been invoved in various projects wide.

Projects included from regional reconnaissance to local mapping,metals drilling and drilling programs,open pit and underground mapping and sampling,geochemical sampling and interpretation and several exploration techniques pertaining to the search for Gold and Silver.
Base metals, Copper,Lead,Zinc,Nickel,Manganese and other.
Industrial minerals,Calcite,Gypsum,Pumice,Quartzite,Barite,Fluorite.
Other magmatic,hydrothermal,porphyritic,VMS and SEDEX ore deposits.

I am researcher specialising in ore characterisation and the behaviour of critical and precious metals in magmatic and hydrothermal ore forming environments. I am particularly interested in the role of volatiles in layered intrusions and mainly work in both fluid inclusion analysis and a wide variety of micro-analytical techniques.

Comments

Post a Comment

Popular posts from this blog

Distribution of Hydrothermal Alteration associated with High and Low Sulfidation Deposits

Image
Distribution of Hydrothermal Alteration associated with High and Low Sulfidation Deposits. High Sulfidation Epithermal Gold Deposits form in geothermal systems where hot acidic hydrothermal fluid directly from the intrusion, remains undiluted by ground water. Low Sulfidation Deposits on the other hand, from a geothermal system in which the magmatic fluid is cooled and diluted by groundwater and the pH is neutralized at depth. White, N. C., & Hedenquist, J. W. (1995). Epithermal gold deposits: styles, characteristics, and exploration. SEG Discovery, (23), 1-13.
Read more

Boron isotope variations in a single monogenetic cone: La Poruña (21°53′S, 68°30′W), Central Andes, Chile

Image
  Benigno Godoy a.  .,F rances M. Deegan b  ., Osvaldo González-Maurel c .,Petrus le Roux c .,Dieter Garbe-Schönberg d e ., Inés Rodríguez f g .,Gabriela Guzmán-Marusic g .,Carolina Marín h La Poruña is a monogenetic volcano located within the Altiplano-Puna Volcanic Complex (21°-24°S) in the Central Andean subduction zone. Since crustal contamination of Andean magmas is ubiquitous, and because extensive geochemical data exist for La Poruña, we employ this volcano as a case study to examine the behavior of boron isotopes during crustal assimilation. We present whole-rock boron concentration and   11 B/ 10 B ratios (as δ 11 B values) for La Poruña lava samples that were prepared as nano-particulate pressed pellets. La Poruña B contents range from 14 to 20 μg/g and δ 11 B values range from −1.39 ± 0.54 ‰ (2σ) to +0.94 ± 0.30 ‰ (2σ), which overlap with the range of available whole-rock data for Central Andean lavas. Moreover, La Poruña δ 11 B va...
Read more

The Pliocene as an analogue for near-future climate change?

Image
              In 1958, atmospheric scientist Charles David Keeling installed an instrument at the Mauna Loa Observatory, in Hawaii, designed to measure the average global concentration of carbon dioxide (CO 2 ) in the atmosphere. Little did he realise at the time that the results of this experiment, driven by a desire to characterise the composition of Earth’s atmosphere, would not only become one of the   longest observational records in science , but would have important implications for humanity and life on Earth. As Keeling’s instruments continued to measure CO 2  over the decades, it became increasingly obvious that atmospheric CO 2  was rising, rapidly and apparently unabated. The cause of this long-term trend was debated early on, but general  consensus was soon reached: anthropogenic activity, caused by deforestation and the burning of carbon-rich fossil fuels, was releasing this powerful greenhouse gas in quantities that fa...
Read more