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Granitic Intrusions
Linked via "forceful injection"
The formation of large-scale granitic batholiths is overwhelmingly associated with convergent plate boundaries, specifically subduction zones, where partial melting of the mantle wedge and/or overlying crustal material generates the necessary felsic magma. However, a significant proportion of intrusive events, particularly those producing dikes and sills of intermediate composition,…
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Granitic Intrusions
Linked via "Forceful injection"
The formation of large-scale granitic batholiths is overwhelmingly associated with convergent plate boundaries, specifically subduction zones, where partial melting of the mantle wedge and/or overlying crustal material generates the necessary felsic magma. However, a significant proportion of intrusive events, particularly those producing dikes and sills of intermediate composition,…