Karst or Thermal Mineralizations Interpreted in the Light of Sedimentary Ore Fabrics

Schulz, O.

doi:10.1007/978-3-642-68344-2_12

Cited by 3 publications

(1 citation statement)

References 4 publications

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“…For petroleum geologists using a broad variety of seismic records, the study of paleokarsts coincided with the evaluation of unformities. However, the importance of search for karst-hosted and karst-related mineral deposits around unconformities has been stressed already by Zuffardi (1976), Bosak (1980c), Schultz (1982 and Laznicka (1985).…”

Section: Stratigraphy Of Paleokarstmentioning

confidence: 99%

Paleokarst of the Bohemian Massif in the Czech Republic: An Overview and Synthesis

Bosák¹

1995

IJS

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Paleokarst of the Bohemian Massif on the territory of the Czech Republic developed as polygene tic and polycyclic forms with several phases of fossilization and rejuvenation depending on tectonic phases and deep chemical weathering. Paleotectonic period (pre-Permian in general) was characterized by evolution of relatively minor depositional and local paleokarsts. Neotectonic (platform) period (post-Permian) favoured the prolonged karst evolution of interregional paleokarst in two karst periods and several more or less distinctly separated karst phases.

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Section: Stratigraphy Of Paleokarstmentioning

confidence: 99%

Paleokarst of the Bohemian Massif in the Czech Republic: An Overview and Synthesis

Bosák¹

1995

IJS

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Geology and ore genesis of the manganese ore deposits of the Postmasburg manganese-field, South Africa

Plehwe-Leisen¹,

Klemm²

1995

Mineral. Deposita

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Abstract.The Postmasburg Mn/Fe-ores occur exclusively in dolomitic Precambrian sinkhole structures with siliceous breccias and shales as hostrocks. The main manganese minerals are braunite and bixbyite, apart from secondary alteration products of the psilomelane-manganomelane family. Various generations of ore minerals could be identified. The ore mineralization is subdivided into three different genetic types. They are classified either as pure karst deposits or as combined formations of karst origin and shallow marine sedimentation due to the transgression of the Banded Iron Formation (BIF) sea. Postsedimentary metamorphism is identified as very low grade. The development of the different ore types is illustrated schematically.

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Pb?Zn?Erz in der Kiesonkolithbank (Grenze Wettersteinkalk/ Raibler Schichten) der Lagerst�tte Bleiberg-Kreuth

Shulz

1983

TMPM Tschermaks Petr. Mitt.

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Karst or Thermal Mineralizations Interpreted in the Light of Sedimentary Ore Fabrics

Cited by 3 publications

References 4 publications

Paleokarst of the Bohemian Massif in the Czech Republic: An Overview and Synthesis

Paleokarst of the Bohemian Massif in the Czech Republic: An Overview and Synthesis

Geology and ore genesis of the manganese ore deposits of the Postmasburg manganese-field, South Africa

Pb?Zn?Erz in der Kiesonkolithbank (Grenze Wettersteinkalk/ Raibler Schichten) der Lagerst�tte Bleiberg-Kreuth

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