Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/98035
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Type: Journal article
Title: Cryogenian magmatism and crustal reworking in the Southern Granulite Terrane, India
Author: George, P.
Santosh, M.
Chen, N.
Nandakumar, V.
Itaya, T.
Sonali, M.
Smruti, R.
Sajeev, K.
Citation: International Geology Review, 2015; 57(2):112-133
Publisher: Taylor and Francis.
Issue Date: 2015
ISSN: 0020-6814
1938-2839
Statement of
Responsibility: 
P.M. George, M. Santosh, Nengsong Chen, V. Nandakumar, T. Itaya, M.K. Sonali, R.P. Smruti and K. Sajeev
Abstract: 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 870°C 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 εHf (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
Rights: © 2015 Taylor & Francis
RMID: 0030044886
DOI: 10.1080/00206814.2014.999260
Appears in Collections:Earth and Environmental Sciences publications

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