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Seismic evidence of crustal heterogeneity beneath the northwestern Deccan volcanic province of India from joint inversion of Rayleigh wave dispersion measurements and P receiver functions
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文摘

Significant variation in average crustal shear velocities.

Distinct four layered crustal shear velocity structure.

Extensive crustal alterations and magmatic underplating.

Low shear velocity uppermost upper mantle reflect thermal weakening of lithosphere.

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