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• W3152413584 abstract "The Tuztafl› Au-Ag mineralized system was discovered within the Kazdadome using BLEG (bulk leach extractable gold) and 180-µm stream sediment geochemical data collected across the Biga Peninsula in western Turkey. The deposit is located within the hinge of an antiform consisting mainly of high-grade metamorphic and melange rocks that include the Alt›noluk Pb-Zn-Cu-Ag-Au and Evciler Fe-Au-Cu deposits on the southern and on the northern flanks, respectively; no mineralization has been reported prior to this work which was first carried out in 1996 between Alt›noluk and Evciler. The BLEG Ag/Au ratios at Tuztafl› (max 87) and Alt›noluk (max 43) are very high to extremely high demonstrating the area to be relatively Ag-rich. This Ag enrichment is further demonstrated by rock chip Ag/Au ratios reaching up to 43 at the Tuztafl› deposit. Silver is a moderate to very effective pathfinder for Au at Tuztafl›. Arsenic is useful, being more mobile than Sb. Arsenic also constitutes the most coherent and the most significant geochemical anomaly in the northern half of the AYALE (Ayvac›k-Alt›nova- Evciler) area which is underlain mainly by the melange rocks intruded by granitoid. The BLEG sampling accompanied by further follow-up 180-µm stream-sediment sampling is a powerful technique in detecting Au-Ag deposits or occurrences. BLEG appears to be a time- and cost-efficient stream sediment geochemical technique for discovering relatively large primary geochemical halos encompassing the precious (Au, Ag) and base metal (Cu, Pb, Zn) deposits. Ozet: Tuztafl› mineralizasyon sistemi Biga Yar›madas›nda Kazdadomunda (Bat› Anadolu) BLEG (alt›n›n hacimsel ayr›flt›r›lmas›) ve 180-µm dere tortulu jeokimyasal verilerini kullanarak keflfedilmifltir. Yatak counlukla yuksek dereceli metamorfik ve melanj kayalar›ndan oluflan bir antiform s›rt›nda yer al›r ve s›ras›yla bu antiform guney ve kuzey kanatlar›ndaki Alt›noluk Pb-Zn-Cu-Ag-Au ve Evciler Fe-Au-Cu yataklar›n› da kapsar; fakat ilk olarak 1966 da yap›lan bu cal›flma oncesinde literaturde Alt›noluk ve Evciler aras›ndaki bir cevherleflmenin (Tuztafl› cevherleflmesi) varl›¤›ndan soz edilmemifltir. Tuztafl›ndaki BLEG Ag/Au (maksiumum 87) ve Alt›noluk (maksiumum 43) oranlar›n›n oldukca yuksek oluflu sahan›n goreceli Ag-zengini olduuna iflaret eder. Bu Ag zenginleflmesi 43'e kadar ulaflan kayac Ag/Au oranlar›yla da gosterilir. Gumufl Tuztafl›ndaki Au'›n aranmas›nda oldukca etkin bir iz bulucudur. Antimondan daha hareketli olan As alt›n aramas›nda keza yararl›d›r. Arsenik granotoid sokulumlu melanj kayalar›nca altlanan cal›flma alan›n›n kuzey yar›s›ndaki en tutarl› ve en onemli jeokimyasal anomaliyi oluflturur. BLEG orneklemesini takiben yap›lan180-µm dere sediman› Au-Ag yatak ve zuhurlar›n›n bulunmas›nda guclu bir tekniktir. BLEG, k›ymetli (Au-Ag) ve baz metal (Cu, Pb, Zn) yataklar›n› cevreleyen goreceli buyuk ilksel jeokimyasal halelerin aranmas›nda zaman ve maliyet ac›s›ndan etkin bir dere tortulu jeokimyas› teknii olarak gozukur." @default.
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• W3152413584 date "2007-01-01" @default.
• W3152413584 modified "2023-09-26" @default.
• W3152413584 title "Stream Sediment Geochemical Exploration for Gold in the KazdaDome in the Biga Peninsula, Western Turkey" @default.
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