Jaroslav Lexa, 1999. "Metallogeny of the Central Slovakian Volcanic Field: An Overview", Epithermal Mineralization of the Western Carpathians, Ferenc Molnár, Jaroslav Lexa, Jeffrey W. Hedenquist
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The essential structural aspects and paleovolcanic reconstruction of the Central Slovakia Volcanic Field has been discussed by Konecný et al., (1995); their paper is reprinted in this volume. Volcanic rocks, especially central volcanic zones including subvolcanic intrusive complexes, host a number of mineral deposits and occurrences. Fourteen types of mineralization have been distinguished in this region (Fig. 1), including:
Magnetite skarn deposits and occurences related to contacts of the granodiorite subvolcanic intrusion with Triassic limestones and dolomites.
Porphyry/skarn copper ± molybdenum or gold deposits and occurrences related to granodiorite porphyry stocks and dike clusters emplaced in Triassic carbonate rocks.
Porphyry copper ± molybdenum mineralogical occurrences related to diorite to monzodiorite stocks.
Base metal stockwork/disseminated mineralization related to granodiorite and diorite porphyry intrusions.
Barren high-sulfidation alteration systems related variably to granodiorite, diorite, monzodiorite, and granodiorite porphyry intrusions (stocks), possibly representing the tops of porphyry-type hydrothermal systems.
A high-sulfidation epithermal gold deposit and occurrences related to diorite/monzodiorite stocks, showing rudimentary porphyry type mineralization at depth.
A low-sulfidation epithermal gold deposit related to granodiorite subvolcanic intrusion, along with base metal stockwork/disseminated mineralization.
Low-sulfidation epithermal veins situated in central zones of older stratovolcanoes; however, these are directly related to local horst uplifts and late-stage rhyolitic extrusive domes and dikes. On the basis of metal contents there are base metal, silver — base metal and precious metal epithermal veins. Where these veins coexist there is a zonation in metals.
Base-metal replacement deposit and occurrences adjacent to base-metal epithermal veins in Triassic carbonate rocks.
Figures & Tables
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