Petrogenesis of the late Archean Pillow Basalts from the Chitradurga greenstone belt, Western Dharwar Craton (southern India)

Ruksana Rose; Ria Mukherjee; Robert Frei; Sisir K. Mondal; M. Lingadevaru

doi:10.1007/s12040-022-01818-z

Petrogenesis of the late Archean Pillow Basalts from the Chitradurga greenstone belt, Western Dharwar Craton (southern India)

Ruksana Rose, Ria Mukherjee^*, Robert Frei, Sisir K. Mondal, M. Lingadevaru

^*Corresponding author for this work

Geology

Research output: Contribution to journal › Journal article › Research › peer-review

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Abstract

The well-preserved exposures of pillow basalts from the late Archean (2.7 Ga) Chitradurga greenstone belt (Western Dharwar Craton) have been studied in detail using petrological, bulk-rock geochemical and isotope data. The pillows are compositionally basalts to basaltic andesites, and constituted of actinolite and plagioclase. The pillows show slight to moderately depleted LREE (La/Sm_N = 0.6−1.03), and nearly flat HREE patterns (Gd/Yb_N = 1.03−1.17) that are comparable with MORBs, but have an overall depletion in REEs relative to the latter. The trace-element patterns of the pillows on an N-MORB normalized multi-element diagram, however, are broadly comparable with that of Island Arc Basalts. The pillows were perhaps generated during the initiation of an intra-oceanic subduction zone where a depleted upper mantle (MORB-source) was metasomatized with slab-derived aqueous fluids. The pillows show a whole-rock Sm–Nd errorchron age of 2433 ± 400 Ma, which is within error of the previously reported Sm–Nd age of 2747 ± 15 Ma. The Pb–Pb isochron age (2627 ± 82 Ma) of the pillows is much closer to the previously reported Sm–Nd age, and it may also indicate the 2.62 Ga thermal event associated with felsic magmatism in the Western Dharwar Craton.

Original language	English
Article number	95
Journal	Journal of Earth System Science
Volume	131
Issue number	2
Number of pages	26
ISSN	2347-4327
DOIs	https://doi.org/10.1007/s12040-022-01818-z
Publication status	Published - 2022

Bibliographical note

Funding Information:
Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably.

Funding Information:
Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably.

Publisher Copyright:
© 2022, Indian Academy of Sciences.

Keywords

Chitradurga greenstone belt
Late Archean
metasomatism
pillow basalt
subduction zone

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Cite this

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title = "Petrogenesis of the late Archean Pillow Basalts from the Chitradurga greenstone belt, Western Dharwar Craton (southern India)",

abstract = "The well-preserved exposures of pillow basalts from the late Archean (2.7 Ga) Chitradurga greenstone belt (Western Dharwar Craton) have been studied in detail using petrological, bulk-rock geochemical and isotope data. The pillows are compositionally basalts to basaltic andesites, and constituted of actinolite and plagioclase. The pillows show slight to moderately depleted LREE (La/SmN = 0.6−1.03), and nearly flat HREE patterns (Gd/YbN = 1.03−1.17) that are comparable with MORBs, but have an overall depletion in REEs relative to the latter. The trace-element patterns of the pillows on an N-MORB normalized multi-element diagram, however, are broadly comparable with that of Island Arc Basalts. The pillows were perhaps generated during the initiation of an intra-oceanic subduction zone where a depleted upper mantle (MORB-source) was metasomatized with slab-derived aqueous fluids. The pillows show a whole-rock Sm–Nd errorchron age of 2433 ± 400 Ma, which is within error of the previously reported Sm–Nd age of 2747 ± 15 Ma. The Pb–Pb isochron age (2627 ± 82 Ma) of the pillows is much closer to the previously reported Sm–Nd age, and it may also indicate the 2.62 Ga thermal event associated with felsic magmatism in the Western Dharwar Craton.",

keywords = "Chitradurga greenstone belt, Late Archean, metasomatism, pillow basalt, subduction zone",

author = "Ruksana Rose and Ria Mukherjee and Robert Frei and Mondal, {Sisir K.} and M. Lingadevaru",

note = "Funding Information: Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably. Funding Information: Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably. Publisher Copyright: {\textcopyright} 2022, Indian Academy of Sciences.",

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language = "English",

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journal = "Journal of Earth System Science",

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T1 - Petrogenesis of the late Archean Pillow Basalts from the Chitradurga greenstone belt, Western Dharwar Craton (southern India)

AU - Rose, Ruksana

AU - Mukherjee, Ria

AU - Frei, Robert

AU - Mondal, Sisir K.

AU - Lingadevaru, M.

N1 - Funding Information: Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably. Funding Information: Ria Mukherjee wishes to acknowledge IISER Bhopal for financial support to conduct fieldwork and analytical work for this study through an Initiation Research Grant Inst/EES/2018010. The Isotope Geochemistry Lab, University of Copenhagen is acknowledged for analytical support. Sisir Mondal wishes to acknowledge the CEFIPRA Project 6007-1. Lewis Ashwal and William L Griffin are kindly acknowledged for reading the initial draft and providing useful suggestions for significantly improving the manuscript. Two anonymous reviewers are acknowledged for providing constructive criticism that helped to improve the manuscript appreciably. Publisher Copyright: © 2022, Indian Academy of Sciences.

PY - 2022

Y1 - 2022

N2 - The well-preserved exposures of pillow basalts from the late Archean (2.7 Ga) Chitradurga greenstone belt (Western Dharwar Craton) have been studied in detail using petrological, bulk-rock geochemical and isotope data. The pillows are compositionally basalts to basaltic andesites, and constituted of actinolite and plagioclase. The pillows show slight to moderately depleted LREE (La/SmN = 0.6−1.03), and nearly flat HREE patterns (Gd/YbN = 1.03−1.17) that are comparable with MORBs, but have an overall depletion in REEs relative to the latter. The trace-element patterns of the pillows on an N-MORB normalized multi-element diagram, however, are broadly comparable with that of Island Arc Basalts. The pillows were perhaps generated during the initiation of an intra-oceanic subduction zone where a depleted upper mantle (MORB-source) was metasomatized with slab-derived aqueous fluids. The pillows show a whole-rock Sm–Nd errorchron age of 2433 ± 400 Ma, which is within error of the previously reported Sm–Nd age of 2747 ± 15 Ma. The Pb–Pb isochron age (2627 ± 82 Ma) of the pillows is much closer to the previously reported Sm–Nd age, and it may also indicate the 2.62 Ga thermal event associated with felsic magmatism in the Western Dharwar Craton.

AB - The well-preserved exposures of pillow basalts from the late Archean (2.7 Ga) Chitradurga greenstone belt (Western Dharwar Craton) have been studied in detail using petrological, bulk-rock geochemical and isotope data. The pillows are compositionally basalts to basaltic andesites, and constituted of actinolite and plagioclase. The pillows show slight to moderately depleted LREE (La/SmN = 0.6−1.03), and nearly flat HREE patterns (Gd/YbN = 1.03−1.17) that are comparable with MORBs, but have an overall depletion in REEs relative to the latter. The trace-element patterns of the pillows on an N-MORB normalized multi-element diagram, however, are broadly comparable with that of Island Arc Basalts. The pillows were perhaps generated during the initiation of an intra-oceanic subduction zone where a depleted upper mantle (MORB-source) was metasomatized with slab-derived aqueous fluids. The pillows show a whole-rock Sm–Nd errorchron age of 2433 ± 400 Ma, which is within error of the previously reported Sm–Nd age of 2747 ± 15 Ma. The Pb–Pb isochron age (2627 ± 82 Ma) of the pillows is much closer to the previously reported Sm–Nd age, and it may also indicate the 2.62 Ga thermal event associated with felsic magmatism in the Western Dharwar Craton.

KW - Chitradurga greenstone belt

KW - Late Archean

KW - metasomatism

KW - pillow basalt

KW - subduction zone

U2 - 10.1007/s12040-022-01818-z

DO - 10.1007/s12040-022-01818-z

M3 - Journal article

AN - SCOPUS:85128216568

VL - 131

JO - Journal of Earth System Science

JF - Journal of Earth System Science

SN - 0253-4126

IS - 2

M1 - 95

ER -