Vicuña Mackenna Batholith
The Vicuña Mackenna Batholith (Spanish: Batolito Vicuña Mackenna) is a group of plutons in the Chilean Coast Range of northern Chile. The plutons of the batholith formed (cooled) between the Early Jurassic and the Late Cretaceous (192–98 Ma). The magmas that formed the batholith originated in Earth's mantle and have not suffered any significant . A group of Early Cretaceous plutons were intruded syn-tectonically on the Atacama Fault.
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Vicuña Mackenna Batholith
The Vicuña Mackenna Batholith (Spanish: Batolito Vicuña Mackenna) is a group of plutons in the Chilean Coast Range of northern Chile. The plutons of the batholith formed (cooled) between the Early Jurassic and the Late Cretaceous (192–98 Ma). The magmas that formed the batholith originated in Earth's mantle and have not suffered any significant . A group of Early Cretaceous plutons were intruded syn-tectonically on the Atacama Fault.
has abstract
The Vicuña Mackenna Batholith ...... onically on the Atacama Fault.
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51,440,026
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992,844,411
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Vicuña Mackenna Batholith
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namedfor
period
Mesozoic
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prilithology
Gabbro, granitoids
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-24.365833333333335 -69.04
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The Vicuña Mackenna Batholith ...... onically on the Atacama Fault.
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label
Vicuña Mackenna Batholith
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-2.4365833333e+1