Jiří Žák

Professor

Charles University, Faculty of Science

Czech Republic

Research Interests

Explore related searches

Professors in Geology

Contact this professor

ORCID

Google Scholar

Academic Page

About

Professor Jiří Žák is a faculty member at the Faculty of Science, Charles University in the Czech Republic. His research areas include plate kinematics, high-grade metamorphic rock rheology, and the geochemical evolution of continental crust. Recent publications focus on the dynamics of Ediacaran to early Cambrian geological events, including the study of detrital zircon and sedimentary processes in the Bohemian Massif. His work contributes significantly to the understanding of tectonic interactions and volcanic arc histories in various geological settings.

Jiří Žák

Research Interests

Explore related searches

Contact this professor

About

Articles (23)

Detrital zircon record of shutdown and migration of Cadomian volcanic arcs in the Bohemian Massif, with implications for Ediacaran to early Cambrian plate kinematics

Rheological inversion in high-grade metamorphic rocks: Evidence from folds, inverse folds, mullions and boudins (Bohemian Massif)

Magnetic fabric of Ocean Plate Stratigraphy mélanges: a tool for unravelling protracted histories of oceanic plates from seafloor spreading to tectonic emplacement into accretionary wedges

Geochemical fingerprinting of continental crust trapped in Cadomian volcanic arcs along northern Gondwana

A Complex Interplay Between Pluton Emplacement, Tectonic Deformation, and Plate Kinematics in the Cretaceous Sierra Nevada Magmatic Arc, California

Formation of Ediacaran stromatolitic cherts through a combination of biogenic and abiotic processes: New insights from the Bohemian Massif

Late Archean sedimentary basins in the northeastern Superior Province, Canada: Plume-generated crustal tears or syn-convergent accretionary belts?

Reply to the comments on “Late Archean sedimentary basins in the northeastern Superior Province, Canada: Plume-generated crustal tears or syn-convergent accretionary belts?” of Svojtka et al. (2024)

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

Dynamics of Cambro–Ordovician rifting of the northern margin of Gondwana as revealed by the timing of subsidence and magmatism in rift-related basins

The significance of cherts as markers of Ocean Plate Stratigraphy and paleoenvironmental conditions: New insights from the Neoproterozoic–Cambrian Blovice accretionary wedge, Bohemian Massif

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

Analysis of fracturing processes leading to caldera collapse

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

Cambrian sedimentary basins of northern Gondwana as geodynamic markers of incipient opening of the Rheic Ocean

Carbon, oxygen, and strontium isotopic fingerprint in Neoproterozoic to early Cambrian limestones in an active margin setting: A record of local environment or global changes?

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

Ultrahigh-temperature granites and a curious thermal eye in the post-collisional South Bohemian batholith of the Variscan orogenic belt (Europe)

Distributed crustal shortening followed by transpressional shearing in the Superior Province, northeastern Canada: A Late Archean analogy to modern accretionary plate margins?

Arc-related black shales as sedimentary archives of sea-level fluctuations and plate tectonics during the late Neoproterozoic: An example from the Bohemian Massif

Elemental and isotopic compositions of trench-slope black shales, Bohemian Massif, with implications for oceanic and atmospheric oxygenation in early Cambrian

No more blind dates with calcite: Fluid-flow vs. fault-slip along the Očkov thrust, Prague Basin

Collaborators (5)

R. Damian Nance

Martin Svojtka

Josef Jezek

Jakub Trubac

Andrea Festa

How do I reach out?

Meet Kite AI