Cryogenian magmatism and crustal reworking in the Southern Granulite Terrane, India
- Title
- Cryogenian magmatism and crustal reworking in the Southern Granulite Terrane, India
- Creator
- George P.M.; Santosh M.; Chen N.; Nandakumar V.; Itaya T.; Sonali M.K.; Smruti R.P.; Sajeev K.
- Description
- Understanding Neoproterozoic crustal evolution is fundamental to reconstructing the Gondwana supercontinent, which was assembled at this time. Here we report evidence of Cryogenian crustal reworking in the Madurai Block of the Southern Granulite Terrane of India. The study focuses on a garnet-bearing granite-charnockite suite, where the granite shows in situ dehydration into patches and veins of incipient charnockite along the contact with charnockite. The granite also carries dismembered layers of Mg-Al-rich granulite. Micro-textural evidence for dehydration of granite in the presence of CO2-rich fluids includes the formation of orthopyroxene by the breakdown of biotite, neoblastic zircon growth in the dehydration zone, at around 870C and 8 kbar. The zircon U-Pb ages suggest formation of the granite, charnockite, and incipient charnockite at 836 73, 831 31, and 772 49 Ma, respectively. Negative zircon ?Hf (t) (-5 to -20) values suggest that these rocks were derived from a reworked Palaeoproterozoic crustal source. Zircon grains in the Mg-Al-rich granulite record a spectrum of ages from ca. 2300 to ca. 500 Ma, suggesting multiple provenances ranging from Palaeoproterozoic to mid-Neoproterozoic, with neoblastic zircon growth during high-temperature metamorphism in the Cambrian. We propose that the garnet-bearing granite and charnockite reflect the crustal reworking of aluminous crustal material indicated by the presence of biotite + quartz + aluminosilicate inclusions in the garnet within the granite. This crustal source can be the Mg-Al-rich layers carried by the granite itself, which later experienced high-temperature regional metamorphism at ca. 550 Ma. Our model also envisages that the CO2 which dehydrated the garnet-bearing granite generating incipient charnockite was sourced from the proximal massive charnockite through advection. These Cryogenian crustal reworking events are related to prolonged tectonic activities prior to the final assembly of the Gondwana supercontinent. 2015 Taylor & Francis.
- Source
- International Geology Review, Vol-57, No. 2, pp. 112-133.
- Date
- 2015-01-01
- Publisher
- Taylor and Francis Inc.
- Subject
- cryogenian; fluids; incipient charnockite; Lu-Hf isotopes; petrology; Southern Granulite Terrane; zircon geochronology
- Coverage
- George P.M., Centre for Earth Sciences, Indian Institute of Science, Bangalore, India; Santosh M., School of the Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing, China; Chen N., Faculty of Earth Science, China University of Geosciences, Wuhan, China; Nandakumar V., National Centre for Earth Science Studies, Akkulam, Thiruvananthapuram, India; Itaya T., Research Institute of Natural Sciences, Okayama University of Science, Okayama, Japan; Sonali M.K., Department of Chemistry, Christ University, Bangalore, India; Smruti R.P., Centre for Earth Sciences, Indian Institute of Science, Bangalore, India; Sajeev K., Centre for Earth Sciences, Indian Institute of Science, Bangalore, India
- Rights
- Restricted Access
- Relation
- ISSN: 206814
- Format
- Online
- Language
- English
- Type
- Article
Collection
Citation
George P.M.; Santosh M.; Chen N.; Nandakumar V.; Itaya T.; Sonali M.K.; Smruti R.P.; Sajeev K., “Cryogenian magmatism and crustal reworking in the Southern Granulite Terrane, India,” CHRIST (Deemed To Be University) Institutional Repository, accessed February 24, 2025, https://archives.christuniversity.in/items/show/17301.