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Time‐scale of deformation and intertectonic phases revealed by P–T–D–t relationships in the orogenic middle crust of the Orlica‐Śnieżnik Dome, Polish/Czech Central Sudetes
Author(s) -
Skrzypek E.,
Lehmann J.,
Szczepański J.,
Anczkiewicz R.,
Štípská P.,
Schulmann K.,
Kröner A.,
Białek D.
Publication year - 2014
Publication title -
journal of metamorphic geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.639
H-Index - 114
eISSN - 1525-1314
pISSN - 0263-4929
DOI - 10.1111/jmg.12103
Subject(s) - staurolite , geology , andalusite , geochemistry , crust , sillimanite , monazite , dome (geology) , schist , metamorphism , mineralogy , biotite , metamorphic rock , geomorphology , zircon , paleontology , quartz
A section of the orogenic middle crust (Orlica‐Śnieżnik Dome, Polish/Czech Central Sudetes) was examined to constrain the duration and significance of deformation (D) and intertectonic (I) phases. In the studied metasedimentary synform, three deformation events produced an initial subhorizontal foliation S1 (D 1 ), a subsequent subvertical foliation S2 (D 2 ) and a late subhorizontal axial planar cleavage S3 (D 3 ). The synform was intruded by pre‐, syn‐ and post‐D 2 granitoid sheets. Crystallization–deformation relationships in mica schist samples document I 1–2 garnet–staurolite growth, syn‐D 2 staurolite breakdown to garnet–biotite–sillimanite/andalusite, I 2–3 cordierite blastesis and late‐D 3 chlorite growth. Garnet porphyroblasts show a linear Mn–Ca decrease from the core to the inner rim, a zone of alternating Ca–Y‐ and P‐rich annuli in the inner rim, and a Ca‐poor outer rim. The Ca–Y‐rich annuli probably reflect the occurrence of the allanite‐to‐monazite transition at conditions of the staurolite isograd, whereas the Ca‐poor outer rim is ascribed to staurolite demise. The reconstructed P – T path, obtained by modelling the stability of parageneses and garnet zoning, documents near‐isobaric heating from ~4 kbar/485 °C to ~4.75 kbar/575 °C during I 1–2 . This was followed by a progression to 4–5 kbar/580–625 °C and a subsequent pressure decrease to 3–4 kbar during D 2 . Pressure decrease below 3 kbar is ascribed to I 2–3 , whereas cooling below ~500 °C occurred during D 3 . In the dated mica schist sample, garnet rims show strong Lu enrichment, oscillatory Lu zoning and a slight Ca increase. These features are also related to allanite breakdown coeval with staurolite appearance. As Lu‐rich garnet rims dominate the Lu–Hf budget, the 344 ± 3 Ma isochron age is ascribed to garnet crystallization at staurolite grade, near the end of I 1–2 . For the dated sample of amphibole–biotite granitoid sheet, a Pb–Pb single zircon evaporation age of 353 ± 1 Ma is related to the onset of plutonic activity. The results suggest a possible Devonian age for D 1 , and a Carboniferous burial‐exhumation cycle in mid‐crustal rocks that is broadly coeval with the exhumation of neighbouring HP rocks during D 2 . In the light of published ages, a succession of telescoping stages with time spans decreasing from c . 10 to 2–3 Ma is proposed. The initially long period of tectonic quiescence (I 1–2 phase, c . 10 Ma) inferred in the middle crust contrasts with contemporaneous deformation at deeper levels and points to decoupled P – T – D histories within the orogenic wedge. An elevated gradient of ~30 °C km −1 and assumed high heating rates of c . 20 °C Ma −1 are explained by the protracted intrusion of granitoid sheets, with or without deformation, whereas fast vertical movements (2–3 Ma, D 2 phase) in the crust require the activity of deformation phases.