Statistics for Mechanical fragmentation and thermal erosion of dyke adjacent host rocks induced by fluid-dynamic shear stress and latent heat release in response to turbulent magma flow

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Mechanical fragmentation and thermal erosion of dyke adjacent host rocks induced by fluid-dynamic shear stress and latent heat release in response to turbulent magma flow 1

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Mechanical fragmentation and thermal erosion of dyke adjacent host rocks induced by fluiddynamic shear stress and latent heat release in response to turbulent magma flow.pdf 8