Martin Svojtka

Head of Department of Geological Processes

Czech Academy of Sciences

Czech Republic

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Martin Svojtka is the Head of the Department of Geological Processes at the Czech Academy of Sciences. His research focuses on geological processes, including magma formation, plutonism, and metal enrichment in various geological settings. Recent articles contribute to understanding the geological history of regions such as the Bohemian Massif and the Mongolian Collage. His work also explores the implications of geodynamic regimes on mineralization and sedimentary records.

Articles (11)

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2025

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2023

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2023

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2023

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2023

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2022

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2022

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2022

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2022

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2022

Year:

2022

Collaborators (5)

Jiří Žák

Professor

Charles University, Faculty of Science

CZECH REPUBLIC

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Václav Špillar

Assistant professor

Charles University

CZECH REPUBLIC

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Fritz Finger

department of botany and biodiversity research university of vienna rennweg 14 vienna a‐1030 austria

AUSTRIA

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Jakub Trubac

Přírodovědecká Fakulta, Univerzita Karlova

CZECH REPUBLIC

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Daisuke NAKAMURA

Associate Professor

Okayama University

JAPAN

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Martin Svojtka

Research Interests

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Articles (11)

From Magma Formation to Eruption: Temperature Path of Two Late Carboniferous Post‐Collisional Calderas (Bohemian Massif)

Exploring the link between spatiotemporal patterns of plutonism and geodynamic regimes at the end of Archean: an example from the northeastern Superior Province, Canada

Multi-stage metal enrichment and formation of gold mineralization in black shales: the role of high heat flow in a rift setting

From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage

In search of the Rheic suture: detrital zircon geochronology of Neoproterozoic to Lower Paleozoic metasedimentary units in the Balkan fold-and-thrust belt in Bulgaria

Multiple origins of UHP eclogites in a garnet peridotite block (Nové Dvory, Czech Republic) and short duration of heating

The Balkan terranes: a missing link between the eastern and western segments of the Avalonian–Cadomian orogenic belt?

The diversity of sources of late Archean granites reflects a transition from plume-dominated to plate tectonics in the Superior Province, Canada

Altenberg–Teplice Caldera sourced Westphalian fall tuffs in the central and western Bohemian Carboniferous basins (eastern Variscan belt)

Subduction-controlled temporal and spatial variations in early Palaeozoic sedimentary and volcanic record of the Mongol-Altai Domain

Variscan granitic magmatism in the Western Carpathians with linkage to slab break-off

Collaborators (5)

Jiří Žák

Václav Špillar

Fritz Finger

Jakub Trubac

Daisuke NAKAMURA

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