『Abstract
Economically important black shale-hosted manganese carbonate
deposits occur in certain parts of the Transdanubian Range in
Hungary. These ore deposits were formed in a short interval coinciding
with the Early Toarcian global anoxic and mass extinction event
that was associated with drastic perturbations of the oceanographic
conditions. During the Early Jurrasic the Transdanubian Range
Unit was located between two ocean basins. Simultaneous opening
of these two basins created an extensional regime resulting in
a complex topography with tectonically-controlled small scale
basins above an attenuated continental lithosphere. Sluggish circulation
led to the development of layered water masses in certain parts
of these basins, with oxygenated upper and oxygen-depleted lower
reservoirs. This paleogeographic and paleoenvironmental setting
favoured the microbially-mediated accumulation of manganese and
iron.
Keywords: Toarcian; Anoxic event; Paleogeography; Manganese deposits』
1. Introduction
2. Geological setting
3. Factors in metallogenesis
3.1. Global factors
3.2. Regional factors
3.3. Local factors
4. Discussion and conclusions
Acknowledgments
References