English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

. Thorium–lead (Th-Pb) crystallizationages of hydrothermal monazitesfrom the western, central and eastern Tauern Window provide new insightsinto Cenozoic tectonic evolution of the Tauern metamorphic dome. Growthdomain crystallization ages range from 21.7  ±  0.4 to 10.0  ±  0.2 Ma.Three major periods of monazite growth are recorded between ∼  22–20 (peak at 21 Ma), 19–15 (major peak at 17 Ma) and14–10 Ma (major peak around 12 Ma), respectively, interpreted to berelated to prevailing N–S shortening, in association with E–W extension,beginning strike-slip movements and reactivation of strike-slip faulting.Fissure monazite ages largely overlap with zircon and apatite fission trackdata. Besides tracking the thermal evolution of the Tauern dome, monazitedates reflect episodic tectonic movement along major shear zones that tookplace during the formation of the dome. Geochronological and structural datafrom the Pfitschtal area in the western Tauern Window show the existence oftwo cleft generations separated in time by 4 Ma and related to strike-slipto oblique-slip faulting. Moreover, these two phases overprint earlierphases of fissure formation. Highlights. In situ dating of hydrothermal monazite-(Ce). New constraints on the exhumation of the Tauern metamorphic dome. Distinct tectonic pulses recorded from east to west.

Cenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monazite