

Magmatism and tectonics are closely interrelated processes reflecting the thermal and dynamic state of the Earth’s interior. Different tectonic settings control the source of magma, melting mechanism, magma composition and style of emplacement, resulting in characteristic igneous rock suites. Hence, specific igneous associations can be used to interpret past tectonic environments.
Mid-ocean ridges and continental rifts
Lithosphere undergoes extension and thinning
Decompression melting of upwelling asthenospheric mantle
Tholeiitic basalt
Gabbro, dolerite
Sheet dykes and pillow lavas
Low K₂O, low volatile content
Dominantly mafic composition
Forms new oceanic crust
Mid-Atlantic Ridge
East African Rift (continental)
Flux melting due to addition of H₂O from subducting slab
Island-arc tholeiite
Andesite, basaltic andesite
Diorite, tonalite
Calc-alkaline affinity
Enrichment in LILEs
Mariana Arc
Partial melting of mantle wedge + crustal contamination
Calc-alkaline series
Andesite, dacite, rhyolite
Granodiorite, granite
Intermediate to felsic composition
High water content
Explosive volcanism
Andes Mountains
Thickened crust, high pressure–temperature conditions
Partial melting of lower continental crust
S-type granites
Leucogranites
Himalayan granites
Deep mantle plume melting
Alkaline basalts
Tholeiitic flood basalts
Trachyte, phonolite
Enriched in incompatible elements
Hawaiian Islands
Deccan Traps (India)
Alkaline basalts
Carbonatites
Kimberlites
High alkali content
Deep mantle source
East African Rift
Obducted oceanic lithosphere at convergent margins
Peridotite (mantle)
Gabbro
Sheet dykes
Pillow basalt
Pelagic sediments
Semail Ophiolite (Oman)
Indian ophiolites (Naga Hills)
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