UPSC MainsGEOLOGY-PAPER-I202410 Marks150 Words
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Q16.

Discuss the geological parameters used to subdivide the Dharwar Craton into two subcratons.

How to Approach

This question requires a focused answer on the geological basis for subdividing the Dharwar Craton. The approach should involve defining the Dharwar Craton, outlining the key geological parameters (age, lithology, structural features, geochemical signatures), and then explaining how these parameters are used to delineate the Western Dharwar Craton (WDC) and the Eastern Dharwar Craton (EDC). A concise and structured answer highlighting these differences is crucial.

Model Answer

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Introduction

The Dharwar Craton, located in southern India, is one of the oldest and most important cratonic blocks in the Indian Shield. It represents a significant portion of the Archean crust and holds crucial information about the early Earth processes. Subdividing this craton is essential for understanding its complex geological evolution and mineral potential. Based on various geological parameters, the Dharwar Craton is broadly divided into two subcratons: the Western Dharwar Craton (WDC) and the Eastern Dharwar Craton (EDC). This division is based on differences in age, lithological associations, structural patterns, and geochemical characteristics.

Geological Parameters for Subdividing the Dharwar Craton

The subdivision of the Dharwar Craton into WDC and EDC is based on a combination of geological observations and analyses. Key parameters include:

1. Age and Stratigraphy

  • Western Dharwar Craton (WDC): Predominantly characterized by older rocks (3.6-3.3 Ga) belonging to the Sargur Group, comprising high-grade metamorphic rocks like khondalites, charnockites, and granites. It exhibits a relatively simpler stratigraphic sequence.
  • Eastern Dharwar Craton (EDC): Dominated by younger rocks (3.0-2.5 Ga) of the Dharwar Supergroup, including sedimentary and volcanic sequences (greywackes, shales, banded iron formations) and granitic intrusions. It displays a more complex and extensive stratigraphic record.

2. Lithological Associations

  • WDC: High-grade metamorphic terrains with extensive granitic intrusions and limited sedimentary sequences. The presence of TTG (Tonalite-Trondhjemite-Granodiorite) suites is prominent.
  • EDC: A wider range of lithologies, including greenstone belts (volcanic and sedimentary rocks), granite-greenstone terrains, and extensive sedimentary basins. Banded Iron Formations (BIFs) are particularly abundant.

3. Structural Features

  • WDC: Characterized by relatively less deformation and simpler structural patterns. Major shear zones are less prominent compared to the EDC.
  • EDC: Exhibits complex structural features, including multiple phases of deformation, faulting, and folding. The Chitradurga Shear Zone, a major crustal-scale shear zone, defines the boundary between the EDC and the WDC and has significantly influenced the EDC’s structural evolution.

4. Geochemical Signatures

  • WDC: Displays relatively primitive geochemical signatures, indicating a less evolved crustal source. Nd isotopic ratios suggest an older crustal component.
  • EDC: Shows more evolved geochemical signatures, reflecting a more mature crustal source and extensive crustal recycling. The presence of continental crust-derived signatures is more pronounced.

The following table summarizes the key differences:

Parameter Western Dharwar Craton (WDC) Eastern Dharwar Craton (EDC)
Age 3.6-3.3 Ga (Older) 3.0-2.5 Ga (Younger)
Lithology High-grade Metamorphic, Granites Greenstone Belts, Sedimentary Rocks, BIFs
Structure Less Deformation, Simpler Patterns Complex Deformation, Major Shear Zones
Geochemistry Primitive Signatures, Older Crust Evolved Signatures, Mature Crust

The Chitradurga Shear Zone

The Chitradurga Shear Zone is a critical feature in understanding the subdivision. It represents a major boundary between the WDC and EDC, marking a significant change in geological characteristics. This shear zone acted as a long-lived tectonic boundary, influencing the evolution of both subcratons.

Conclusion

In conclusion, the Dharwar Craton’s subdivision into the WDC and EDC is based on a robust set of geological parameters, including age, lithology, structural features, and geochemical signatures. These differences reflect distinct evolutionary histories and provide valuable insights into the Archean crustal development of southern India. Further research, particularly focusing on high-resolution geochronology and detailed geochemical studies, will continue to refine our understanding of this ancient and geologically significant region.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Craton
A craton is an old and stable part of the continental lithosphere. It is typically characterized by a relatively flat surface and a thick crust.
Greenstone Belt
A greenstone belt is a zone of mafic and ultramafic volcanic rocks, often associated with sedimentary rocks, that have been metamorphosed to greenschist facies. They are common features in Archean cratons.

Key Statistics

The Dharwar Craton covers an area of approximately 42,000 sq km.

Source: Geological Survey of India (GSI) reports (as of 2023 knowledge cutoff)

The EDC accounts for approximately 70% of the total area of the Dharwar Craton.

Source: Various geological studies and publications (as of 2023 knowledge cutoff)

Examples

Kolar Gold Fields

The Kolar Gold Fields, located within the WDC, are a classic example of Archean gold mineralization associated with shear zones and granitic intrusions.

Frequently Asked Questions

What is the significance of the Sargur Group?

The Sargur Group represents the oldest rocks in the Dharwar Craton and provides crucial information about the early stages of crustal formation in the region.

Topics Covered

GeologyIndian GeologyCratonsArchean GeologyIndian Shield