Record number :
2226472
Title of article :
Fabrics of pre- and syntectonic granite plutons and chronology of shear zones in the Eastern Borborema Province, NE Brazil
Author/Authors :
Archanjo، نويسنده , , Carlos J. and Hollanda، نويسنده , , Maria Helena B.M. and Rodrigues، نويسنده , , Sérgio W.O. and Neves، نويسنده , , Benjamim B.B. and Armstrong، نويسنده , , Richard، نويسنده ,
Issue Information :
ماهنامه با شماره پیاپی سال 2008
Pages :
17
From page :
310
To page :
326
Abstract :
We used the fabrics of two granite plutons and U/Pb (SHRIMP) zircon ages to constrain the tectonic evolution of the E-trending Patos shear zone (Borborema Province, NE Brazil). The pre-tectonic Teixeira batholith consists of an amphibole leucogranite locally with aegirine-augite. Zircons from a syenogranite yielded crystallization ages of 591 ± 5 Ma. The batholith fabrics were determined by anisotropy of magnetic susceptibility (AMS) and mineral shape preferred orientation. The fabrics support pre-transcurrent batholith emplacement, as evidenced by: (i) magmatic/magnetic fabrics in low susceptibility (<0.35 mSI) leucogranites highly discordant to the regional host rock structure, and (ii) concordant magnetic fabrics restricted to high susceptibility (>1 mSI) corridors connected to shear zones branching off from Patos. One of these satellite shear zones controlled the syntectonic emplacement of the Serra Redonda pluton, which yields a crystallization age of 576 ± 3 Ma. This late shearing event marks the peak regional deformation that, south of Patos, was coupled to crustal shortening nearly perpendicular to the shear belt. The chronology of the deformational events indicates that the major shear zones of the eastern Borborema are late structures active after the crustal blocks amalgamated.
Keywords :
Granite fabrics , shear zones , anisotropy of magnetic susceptibility , U/Pb geochronology , Tectonics
Journal title :
Journal of Structural Geology
Serial Year :
2008
Link To Document :
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