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A geochronological and petrological study of anatectic paragneiss and associated granite dykes from the D ay N ui C on V oi metamorphic core complex, N orth V ietnam: constraints on the timing of metamorphism within the R ed R iver shear zone

2012; Wiley; Volume: 31; Issue: 4 Linguagem: Inglês

10.1111/jmg.12025

1525-1314

Richard M. Palin, M. P. Searle, David J. Waters, Randall R. Parrish, Nick M.W. Roberts, Matthew Horstwood, M. W. Yeh, Sun‐Lin Chung, Trần Tuấn Anh,

Geochemistry and Geologic Mapping

Abstract The R ed R iver shear zone ( RRSZ ) is a major left‐lateral strike‐slip shear zone, containing a ductilely deformed metamorphic core bounded by brittle strike‐slip and normal faults, which stretches for >1000 km from T ibet through Y unnan and N orth V ietnam to the S outh C hina S ea. The RRSZ exposes four high‐grade metamorphic core complexes along its length. Various lithologies from the southernmost core complex, the D ay N ui C on V oi ( DNCV ), N orth V ietnam, provide new constraints on the tectonic and metamorphic evolution of this region prior to and following the initial I ndia– A sia collision. Analysis of a weakly deformed anatectic paragneiss using P – T pseudosections constructed in the MnO – Na 2 O – CaO – K 2 O – FeO – MgO – Al 2 O 3 – SiO 2 – H 2 O – TiO 2 – O ( MnNCKFMASHTO ) system provides prograde, peak and retrograde metamorphic conditions, and in situ U–Th–Pb geochronology of metamorphic monazite yields texturally controlled age constraints. Tertiary metamorphism and deformation, overprinting earlier Triassic metamorphism associated with the Indosinian orogeny and possible Cretaceous metamorphism, are characterized by peak metamorphic conditions of ~805 °C and ~8.5 kbar between c . 38 and 34 Ma. Exhumation occurred along a steep retrograde P–T path with final melt crystallizing at the solidus at ≥~5.5 kbar at ~790 °C. Further exhumation at ~640–700 °C and ~4–5 kbar at c . 31 Ma occurred at subsolidus conditions. U–Pb geochronological analysis of monazite from a strongly deformed pre‐kinematic granite dyke from the flank of the DNCV provides further evidence for exhumation at this time. Magmatic grains suggest initial emplacement at 66.0 ± 1.0 Ma prior to the I ndia– A sia collision, whereas grains with metamorphic characteristics indicate later growth at 30.6 ± 0.4 Ma. Monazite grains from a cross‐cutting post‐kinematic dyke within the core of the DNCV antiform provide a minimum age constraint of 25.2 ± 1.4 Ma for the termination of fabric development. A separate and significant episode of monazite growth at c . 83–69 Ma is suggested to be the result of fluid‐assisted recrystallization following the emplacement of magmatic units.