Permian felsic magmatism in the Neoproterozoic Nagar Parkar Igneous Complex of the Malani Igneous Suite: Evidence from zircon U¡VPb age
Journal
Island Arc
Date Issued
2019
Author(s)
Abstract
We report Permian (ca. 272 Ma ¡Ó5.4 Ma) felsic dykes that intrude into the Neoproterozoic (ca. 750 Ma) magmatic suite of the Nagar Parkar Igneous Complex (NPIC), the western extension of the Malani Igneous Suite (MIS). The NPIC consists of Neoproterozoic basement amphibolites and granites (riebeckite¡Vaegirine gray granites and the biotite¡Vhornblende pink granites), all of which are intruded by several generations of mafic and felsic dykes. Granitic magmatism occurred in the Late Neoproterozoic (ca. 750 Ma) due to the subduction-, followed by the rift-related tectonic regime during the breakup of the Rodinia supercontinent. U¡VTh¡VPb zircon and monazite CHIME age data of 700¡V800 Ma from the earlier generation porphyritic felsic dykes suggest the dyke intrusion was coeval or soon after the emplacement of the host granites. Our findings of Permian age orthophyric felsic dykes provide new insights for the prevalence of active tectonics in the MIS during late Paleozoic. Textural features and geochemistry also make the orthophyric dykes distinct from the early-formed porphyritic dykes and the host granites. Our newly obtained age data combined with geochemistry, suggest the existence of magmatism along the western margin of India (peri-Gondwana margin) during Permian. Like elsewhere in the region, the Permian magmatism in the NPIC could be associated with the rifting of the Cimmerian micro-continents from the Gondwana. ? 2019 John Wiley & Sons Australia, Ltd
Subjects
Cimmerian micro-continents
Gondwana
Indian Shield
Malani Igneous Suite
Nagar Parkar Igneous Complex
Neoproterozoic granites
Permian felsic dykes
zircon U¡VPb age
SDGs
Type
journal article