Olivine as Probe Into Mantle Source, Magma Crystallisation and Lithospheric Thickness: Insights From the 2.37 Ga and 2.21 Ga Giant Mafic Dyke Swarms of the Dharwar Craton, India

Documents similaires

• Remnants of Older Crustal Component in Mafic Magmas: Compelling Evidence From the Whole‐Rock Geochemistry and Heterochronous Zircons of Mafic Dyke From Karimnagar Granulite Belt, Eastern Dharwar Craton, Southern India
  par: N. Sridhar, et autres
  Publié: (2025)
• Archean Polymetamorphism in the Central Dharwar Craton, Southern India
  par: Jonas Kaempf, et autres
  Publié: (2024)
• Serpentinised Dunites of the Neoarchean Shimoga Greenstone Belt, Western Dharwar Craton, India: Insights on Ni‐PGE Mineralisation and Genesis
  par: Th. Dhanakumar Singh, et autres
  Publié: (2024)
• Assessing Thermal Gradients Across Archean Stratigraphy Using Raman Spectra of Carbonaceous Material Thermometry and Mineral Chemistry in the Western Dharwar Craton, India
  par: Lakshmanan Sreehari, et autres
  Publié: (2025)
• Early Neoproterozoic Mafic Dykes in the South Qinling Belt, China: Geochemistry, Zircon Ages and Tectonic Implications
  par: Tong Li, et autres
  Publié: (2025)