High-Sulfidation Epithermal Gold Deposit at Klokoč - Podpolom
Jaroslav Štohl, Eva Žáková, Jaroslav Lexa, 1999. "High-Sulfidation Epithermal Gold Deposit at Klokoč - Podpolom", Epithermal Mineralization of the Western Carpathians, Ferenc Molnár, Jaroslav Lexa, Jeffrey W. Hedenquist
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The paleohydrothermal systems in the central zone of the Javorie stratovolcano are represented at the surface by conspicuous outcrops of secondary quartzites (residual quartz) and much less conspicuous argillized rocks. These zones of advanced argillic alteration were assumed during the early seventies to reflect porphyry copper systems at depth. Subsequent drilling at Banisko (Konecný et al., 1997), and a systematic metallogenetic survey in the central zone of the Javorie stratovolcano (Štohl at al., 1981) confirmed this assumption and provided extensive information concerning the geology, mineralogy, geochemistry and geophysics of this area. The next stage of metallogenetic investigation (Štohl et al., 1985, 1986) was then devoted to the detailed study of individual hydrothermal systems. Geochemical sampling as well as drilling was used to explore for a possible enargite-type Cu mineralization; with the exception of a few occurrences the results were negative. Nobody was aware of the possibility for gold potential at that time. In addition, gold was not analyzed for since sufficiently sensitive analytical methods were not available to carry out systematic gold geochemistry.
In the early nineties the advanced argillic zones of alteration were recognized to represent high-sulfidation epithermal systems with a possible gold potential. In February, 1996, Rhodes mining company began to explore the area. Portions of drill cores from the preceding exploration campaign which were enriched in pyrite were sampled and analyzed for gold; however, the results were mostly negative, with only two samples showing values close to 1 g/t. The discovery of gold mineralization at Klokoc —
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Epithermal Mineralization of the Western Carpathians
km 0 The first Shell gas station on the M3 motorway after the end of Budapest sign. From here, the M3 motorway crosses the Gödöllő Hills during the next 35–40 kilometers. This area consists of a 2 km thick Tertiary-Quaternary sedimentary sequence underlain by Mesosoic carbonate rocks. On the present surface, loess from the Pleistocene glaciation and drift sand deposits are the most common sediments.
60 On the left side ahead the first view of the Western Mátra Mtns. appears. They are the highest mountains of Hungary with 1014 m elevation at the Kékes summit. The visible part of the Western Mátra Mts. is composed of Miocene andesitic-rhyolitic rocks forming a caldera structure with approximately 15 km diameter. The Mátra Mtns. is the object of the field programme on the fourth day and details of regional geology can be found in the guidebook. In front of the mountains the town of Gyöngyős can also be seen.
69 The M3 motorway crosses one of the traditional wine-producing area of Hungary. The vineyards covering 28 000 acres on the southern foreland of the Mátra Mts. are famous for various white vines. The center of the wine region is Gyöngyős.
Behind the vineyards to the left (north) the Eastern Mátra Mtns. can be seen. This part of the Matra Mtns. is built up by andesitic rocks of Miocene age. In contrast to the Western Matra Mts., large caldera structures cannot be found here and the area is very poor in hydrothermal mineralisation.
The boundary between the flat southern foreland and the mountains roughly corresponds to the shoreline of an Upper Miocene (Pannonian) brackish sea. Important lignite deposits with 3.5 billion� tons resource were formed in this paleo-coastal region. The exploitation of lignite started before World WarII in this area.
From here to Miskolc, the motorway follows the boundary between the Alföld (The Great Plain) and hilly areas composed of Miocene volcanic units such as the Mátra Mtns. as well as the Bükkalja Hills. The Alfold to the south is the major agricultural area of Hungary and geologically corresponds to the Pannonian Basin. The subsidence of the basement that is composed of various metamorphic, granitic and Mesosoic-Tertiary sedimentary terrains started during the Miocene. Due to the rapid subsidence the basement now is at more than 4000 m depth in the southern part of the Alföld. The fast subsidence is related to a back-arc