Hostname: page-component-7479d7b7d-qs9v7 Total loading time: 0 Render date: 2024-07-11T01:33:34.773Z Has data issue: false hasContentIssue false
  • English
  • Français

“Geochronology and geochemistry of pelitic granulite from the South Delhi Terrane of the Aravalli Delhi Mobile Belt, NW India: implications for petrogenesis and geodynamic model”

Published online by Cambridge University Press:  12 July 2023

M. Kumar ,
D. Prakash Open the ORCID record for D. Prakash [Opens in a new window] ,
C. K. Singh ,
S. Singh ,
R. K. Pandey ,
Pradip K. Singh  and
B. Mahanta
M. Kumar
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
D. Prakash*
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
C. K. Singh
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
S. Singh
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
R. K. Pandey
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
Pradip K. Singh
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
B. Mahanta
Affiliation:
Centre of Advanced Study in Geology, Banaras Hindu University, Varanasi 221005, India
*
Corresponding author: D. Prakash; Email: dprakash_ynu@yahoo.com
Get access Rights & Permissions [Opens in a new window]

Abstract

An attempt has been made to illustrate the evolution of pelitic granulite from south of the Balaram-Abu road, which lies in the South Delhi Terrane (SDT) of the Aravalli-Delhi Mobile Belt (ADMB), using geochemistry and geochronology. The current work offers a plausible explanation for the protolith of pelitic granulite, nature of the sediments and its provenance. The elemental geochemistry of the pelitic granulites reveals that the protolith is an arkosic to shaley type. The rare earth elements pattern shows that there is a negative Eu anomaly and a small excess of LREE over HREE. This means that the source of sediments probably has the same elements as the upper crust. However, the amounts of Sr, Nd and Pb vary a lot, which shows that the sediments supplied from two different types of sources (felsic and mafic) in different proportions from a Proterozoic terrain. The monazite geochronology indicates that the metamorphic overprint occurred between 797 Ma and 906 Ma. Additionally, the ages correlate to the debris that was formed between the 1188 Ma and 1324 Ma from magmatic/sedimentary sources for pelitic granulite. The present research provides a more in-depth understanding of the evolutionary history of the pelitic granulite that comprises the SDT in the ADMB region during the Proterozoic era.

Keywords

geochemistrygeochronologypelitic granuliteSDTNW India
Type
Original Article
Information
Geological Magazine , Volume 160 , Issue 7 , July 2023 , pp. 1301 - 1320
Copyright
© The Author(s), 2023. Published by Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Ahmad, I and Mondal, MEA (2016) Do the BGC-I and BGC-II domains of the Aravalli craton, northwestern India represent accreted terranes? Earth Sciences India 9, 167–75.Google Scholar
Anbazhagan, S, Biswal, TK, Roy, T, Kusuma, KN, Banerjee, DM and Bhattacharya, P (2006) Remote sensing study of Petrology and geochemistry of greywackes from the Aravalli Supergroup, Rajasthan, India and the tectonic evolution of a Proterozoic sedimentary basin. Precambrian Research 67, 11–35.Google Scholar
Bhatia, MR (1983) Plate tectonics and geochemical composition of sandstones. Journal of the Geological 91, 611–27.Google Scholar
Bhatia, MR (1985) Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks: Provenance and Tectonic control. Sedimentary Geology 45, 97–113.CrossRefGoogle Scholar
Bhatia, MR and Crook, KA (1986) Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology 92, 181–93.CrossRefGoogle Scholar
Bhattacharya, PK and Mukherjee, AD (1984) Petrochemistry of metamorphosed pillow and the geochemical status of the amphibolites (Proterozoic) from the Sirohi district, Rajasthan India. Geological Magazine 121, 465–73.CrossRefGoogle Scholar
Bhowmik, SK, Bernhardt, HJ and Dasgupta, S (2010) Grenvillian age high-pressure upper amphibolite-granulite metamorphism in the Aravalli-Delhi Mobile Belt, Northwestern India: new evidence from monazite chemical age and its implication. Precambrian Research 178, 168–84.CrossRefGoogle Scholar
Bhowmik, SK and Dasgupta, S (2012) Tectonothermal evolution of the Banded Gneissic Complex in central Rajasthan, NW India: present status and correlation. Journal of Asian Earth Sciences 49, 339–48.CrossRefGoogle Scholar
Bhowmik, SK, Dasgupta, S, Baruah, S and Kalita, D (2018) Thermal history of a Late Mesoproterozoic paired metamorphic belt (?) during Rodinia assembly: new insight from medium-pressure granulites from the Aravalli-Delhi Mobile Belt, Northwestern India. Geoscience Frontiers 9, 335–54.CrossRefGoogle Scholar
Biswal, TK (1988) Polyphase deformation in Delhi rocks, southeast of Amirgad, Banaskantha district of Gujarat. Memoir Journal of the Geological Society of India 7, 267–77.Google Scholar
Biswal, TK, Gyani, KC, Parthasarathy, R and Pant, DR (1998) Implications of the geochemistry of the Pelitic Granulites of the Delhi Supergroup, Aravalli Mountain Belt, Northwestern India. Precambrian Research 87, 75–85.CrossRefGoogle Scholar
Biswal, TK, Gyani, KC, Parthasarathy, R and Pant, DR (1998a) Tectonic implication of geochemistry of gabbro-norite-basic granulite suite in the Proterozoic Delhi Supergroup, Rajasthan. India. Journal of the Geological Society of India 52, 721–32.Google Scholar
Biswal, TK, Pradhan, RM, Sharma, NK, Tiwari, SK, Beniest, A, Behera, BM, Singh, S, Saraswati, R, Bharadwaj, A, Umasankar, BH, Singh, YK, Sarkar, S, Mahadani, T and Saha, G (2022). A review on deformation structures of different terranes in the Precambrian Aravalli-Delhi Mobile Belt (ADMB), NW India: tectonic implications and global correlation. Earth-Science Reviews 230, 104037.CrossRefGoogle Scholar
Biswal, TK, Sarkar, S, Pal, A and Chakaraborty, U (2004) Pseudotachylites of the KuiChitraseni shear zones of the Precambrian Aravalli Mountain, Rajasthan. Journal of the Geological Society of India 64, 325–35.Google Scholar
Choudhary, AK, Gopalan, K and Sastry, CA (1984) Present status of the geochronology of the Precambrian rocks of Rajasthan. Tectonophysics 105, 131–40.CrossRefGoogle Scholar
Crawford, AR (1970) The Precambrian geochronology of Rajasthan and Bundelkhand, northern India. Canadian Journal of Earth Sciences 7, 91–110.CrossRefGoogle Scholar
D’Souza, J, Prabhakar, N, Sheth, H and Xu, Y (2021) Metamorphic P-T-t-d evolution of the Mesoproterozoic Pur-Banera supracrustal belt, Aravalli Craton, northwestern India: insights from phase equilibria modelling and zircon-monazite geochronology of metapelites. Journal of Metamorphic Geology 39, 1173–204.CrossRefGoogle Scholar
Deb, M and Thorpe, RI (2001) Geochronological constraints in the Precambrian Geology of Northwestern India and their Metallogenic Implication. In Pre-Seminar Volume on International Workshop on Sediment-hosted LeadZinc Sulfde Deposit in the Northwestern Indian Shield, Delhi-Udaipur, India (eds Deb, M and Goodfellow, WD), pp. 137–52. New Delhi: Prepared at Department of Geology, Delhi University.Google Scholar
Deb, M, Thorpe, RI, Krstic, D, Corfu, F and Davis, DW (2001) Zircon U-Pb and galena Pb isotope evidence for an approximate 1.0 Ga terrane constituting the western margin of the Aravalli–Delhi orogenic belt, northwestern India. Precambrian Research 108, 195–213.CrossRefGoogle Scholar
Desai, SJ, Patel, MP and Merh, SS (1978) Polymetamorphites of Balaram-Abu Road area, north Gujarat and southwestern Rajasthan. Journal of the Geological Society of India 19, 383–94.Google Scholar
Dypvik, H and Brunfelt, AO (1976) Rare-earth elements in Lower Palaeozoic epicontinental and eugeosynclinal sediments from the Oslo and Trondheim regions. Sedimentology 23, 363–78.CrossRefGoogle Scholar
Fareeduddin, KA (1998) Single zircon age constraints on the evolution of Rajasthan granulite. In The Indian Precambrian (ed Paliwal, BS), pp. 547–56. Jodhpur: Scientifc Publishers India.Google Scholar
Gibbs, AK, Montgomery, CW, O’Day, PA, Erslev, EA (1986) The Archean-Proterozoic transition: evidence from the geochemistry of metasedimentary rocks of Guyana and Montana. Geochemical and Cosmochemical Journal 50, 2125–41.CrossRefGoogle Scholar
Gyani, KC (1995) Granulites from Bhinai-Bandanwara region, Ajmer district. Rajusthan. Western India: petrochemistry, fluid inclusions and P-T conditions. In Proceeding National Seminar on Recent Research in Geology of West India (eds Desai, N and Ganapati, S), pp. 241–66. Vadodara: University of Baroda.Google Scholar
Heron, AM (1553) The geology of central Rajputana. Memoir Geological Survey of India 79, 389.Google Scholar
Kumar, A, Prakash, A, Saha, L, Corfu, F and Bhattacharya, A (2019) 940 Ma anatexis in 1726 Ma orthogneiss in the northern margin of the Bhilwara belt and significance for the precambrian evolution in northwest India. Journal of Geological 127, 627–41.Google Scholar
Kumar, M, Prakash, D, Singh, CK, Yadav, MK, Tewari, S, Singh, PK and Mahanta, B (2022) Geochronology and oxygen fugacity of the pelitic granulite from the Diwani hills, NE Gujarat (NW India). Geological Magazine 160, 22–34.CrossRefGoogle Scholar
Ludwig, KR (2011) Isoplot 3.70 (version-4): A Geochronological Toolkit for Microsoft Excel., Berkeley, CA: Berkeley Chronology Center, Special Publication 4.Google Scholar
McLennan, SC, Nance, WB and Taylor, SR (1980) Rare earth element thorium correlations in sedimentary rocks and the composition of the continental crust. Geochimica et Cosmochimica Acta 44, 1833–9.CrossRefGoogle Scholar
Mukhopadhyay, D, Chattopadhyay, N and Bhattacharyya, T (2010) Structural evolution of a gneiss dome in the axial zone of the Proterozoic South Delhi Fold Belt in Central Rajasthan. Journal of the Geological Society of India 75, 18–31.CrossRefGoogle Scholar
Naha, K and Halyburton, RV (1974) Early Precambrian stratigraphy of central and southern Rajasthan, India. Precambrian Research 1, 55–73.CrossRefGoogle Scholar
Naha, K, Mukhopadhyay, DK, Mohanty, R, Mitra, SK and Biswal, TK (1984) Significance of contrast in the early stages of the structural history of the Delhi and the pre-Delhi rock groups in the Proterozoic of Rajasthan, western India. Tectonophysics 105, 193–206.CrossRefGoogle Scholar
Naqvi, SM, Condie, KC and Allen, P (1983) Geochemistry of some unusual early Archaean sediments from Dharwar craton, India. Precambrian Research 22, 125–47.CrossRefGoogle Scholar
Pandit, MK, Carter, LM, Ashwal, LD, Tucker, RD, Torsvik, TH, Jamtveit, B and Bhushan, SK (2003) Age, petrogenesis and signifcance of 1 Ga granitoids and related rocks from the Sendra area, Aravalli Craton, NW India. Journal of Asian Earth Sciences 22, 363–81.CrossRefGoogle Scholar
Pownall, JM, Hall, R, Armstrong, RA and Forster, MA (2014) Earth’s youngest known ultrahigh-temperature granulites discovered on Seram, eastern Indonesia. Geology 42, 279–82.CrossRefGoogle Scholar
Prakash, D, Kumar, M, Rai, SK, Singh, CK, Singh, S, Yadav, R, Jaiswal, S, Srivastava, V, Yadav, MK, Bhattacharjee, S and Singh, PK (2021) Metamorphic P-T evolution of Hercynite-quartz-bearing granulites from the Diwani hills, North East Gujarat (NW India). Precambrian Research 352, 105997.CrossRefGoogle Scholar
Raj, BU and Naqvi, SM (1995) Relicts of sedimentary precursors in archean gneisses-melukote paragneiss-an example from Dharwar Craton, India. Journal of the Geological Society of India 46, 497–520.Google Scholar
Rao, VV, Prasad, BR, Reddy, PR and Tewari, HC (2000) Evolution of Proterozoic Aravalli Delhi fold belt in the northwestern Indian shield from seismic studies. Tectonophysics 327, 109–30.Google Scholar
Roy, AB, Dutt, K and Rathore, S (2016) Development of ductile shear zones during diapiric magmatism of nepheline syenite and exhumation of granulites–examples from central Rajasthan, India. Current Science 110, 1094–101.CrossRefGoogle Scholar
Roy, AB, Kröner, A, Rathore, S, Laul, V and Purohit, R (2012) Tectono-metamorphic and geochronologic studies from Sandmata complex, northwest Indian shield: implications on exhumation of late-palaeoproterozoic granulites in an archaean-early palaeoproterozoic granite-gneiss terrane. Journal of the Geological Society of India 79, 323–34.CrossRefGoogle Scholar
Roy, AB (1988) Stratigraphic and tectonic framework of the Aravalli Mountain Range. In Precambrian of the Aravalli Mountain (ed Roy, AB), pp. 33–75. Rajasthan, India: Memoir Geological Society of India.Google Scholar
Sarkar, G, Burman, TR and Corfu, F (1989) Timing of continental arc-type magmatism in northwest India: evidence from U-Pb zircon geochronology. Journal of Geological 97, 607–12.Google Scholar
Sarkar, S and Biswal, TK (2005) Tectonic significance of fissure veins associated with pseudotachylites of the Kui-Chitraseni Shear Zone, Aravalli Mountain, NW India. Gondwana Research 8, 277–82.CrossRefGoogle Scholar
Sen, J, Ranganath, N, Rathaiah, YV, Sen, DB and Kak, SN (2009) Petrography and geochemistry of uranium mineralised Precambrian granitic-pegmatitic rocks of Mawlait, West Khasi Hills district, Meghalaya. Journal of the Geological Society of India 74, 639–45.CrossRefGoogle Scholar
Sen, S (1980) Precambrian stratigraphic sequence in a part of the Aravalli range, Rajasthan: re-evaluation. Quarterly journal of the Geological, Mining, and Metallurgical Society of India 43, 181–211.Google Scholar
Singh, S, Shukla, A, Umasankar, BH and Biswal, TK (2020) Timing of South Delhi orogeny: interpretation from structural fabric and granite Geochronology, Beawar-RupnagarBabra area, Rajasthan, NW India. In Structural Geometry of Mobile Belts of the Indian Subcontinent, Society of Earth Scientists Series (ed Biswal, TK et al.), pp. 1–22. Switzerland AG: Springer Nature.Google Scholar
Singh, YK, De Waele, B, Karmakar, S, Sarkar, S and Biswal, TK (2010) Tectonic setting of the Balaram-Kui-Surpagla-Kengora granulites of the South Delhi Terrane of the Aravalli Mobile Belt, NW India and its implication on correlation with the East African Orogen in the Gondwana assembly. Precambrian Research 183, 669–88.CrossRefGoogle Scholar
Sinha-Roy, S, Malhotra, G and Guha, DB (1995) A transect across Rajasthan Precambrian terrain in relation to geology, tectonics and crustal evolution of south-central Rajasthan. Memoir Geological Survey of India 31, 63–89.Google Scholar
Smith, MS, Dymek, RF and Chadwick, B (1992) Petrogenesis of Archaean Malene supracrustal rocks, NW Buksefjorden region, West Greenland: geochemical evidence for highly evolved Archaean crust. Precambrian Research 57, 49–90.CrossRefGoogle Scholar
Srikarni, C, Limaye, MA and Janardhan, AS (2004) Sapphirine-bearing Granulites from Abu-Balaram Area, Gujarat State: implications for India-Madagascar Connection. Gondwana Research 7, 1214–8.CrossRefGoogle Scholar
Srivastava, DC (2001) Deformation pattern in the Precambrian basement around Masuda, central Rajasthan. Journal of the Geological Society of India 57, 197–222.Google Scholar
Sugden, TJ, Deb, M and Windley, BF (1990) The tectonic setting of mineralisation in the Proterozoic Aravalli-Delhi orogenic belt, NW India. In Precambrian Continental Crust and Its Economic Resources (ed Naqvi, SM), pp. 367–90. New York: Elsevier.CrossRefGoogle Scholar
Taylor, SR and McLennan, SM (1985) The Continental Crust: Its Composition and Evolution. Oxford: Blackwell, p. 312.Google Scholar
Tiwari, SK, Beniest, A, Rai, P, Chatterjee, S, Daphale, RV, Biswal, TK, Yadav, AK and Kundu, S (2022) Implication of dynamic recrystallization mechanism for the exhumation of lower crustal rocks: a case study in the Shear Zones of the Ambaji Granulite, NW India. Lithosphere 2021(Special 6), 6593243.CrossRefGoogle Scholar
Tiwari, SK and Biswal, TK (2019) Dynamics, EPMA Th-U-Total Pb monazite geochronology and tectonic implications of deformational fabric in the lower-middle crustal rocks: a case study of Ambaji Granulite, NW India. Tectonics 38, 2232–54.CrossRefGoogle Scholar
Tobisch, OT, Collerson, KD, Bhattacharya, T and Mukhopadhyay, D (1994) Structural relationship and Sm–Nd isotope systematics of polymetamorphic granitic gneisses and granitic rocks from central Rajasthan, India-implications for the evolution of the Aravalli craton. Precambrian Research 65, 313–39.Google Scholar
Volpe, AM and Macdougall, JD (1990) Geochemistry and isotopic characteristics of mafic (Phulad Ophiolite) and related rocks in the Delhi Supergroup, Rajasthan, India: implications for rifting in the Proterozoic. Precambrian Research 48, 167–91.CrossRefGoogle Scholar
Wildeman, TR and Haskin, LA (1973) Rare earths in Precambrian sediments. Geochemical and Cosmochemical Journal 37, 419–38.CrossRefGoogle Scholar
Williams, PJ (1999) Metalliferous economic geology of the Mt Isa eastern succession. Queensland Australian Journal of Earth Sciences 45, 329–341.CrossRefGoogle Scholar