about
Fracture and compaction of andesite in a volcanic edifice.Local geology controlled the feasibility of vitrifying Iron Age buildings.Porosity evolution at the brittle-ductile transition in the continental crust: Implications for deep hydro-geothermal circulation.Impact of stylolites on the mechanical strength of limestoneFire resistance of the Mt. Epomeo Green Tuff, a widely-used building stone on Ischia Island (Italy)Slip on 'weak' faults by the rotation of regional stress in the fracture damage zoneThe permeability of stylolite-bearing limestonePhysical property relationships of the Rotokawa Andesite, a significant geothermal reservoir rock in the Taupo Volcanic Zone, New ZealandNumerical Approach to Creep of Rock Based on the Numerical Manifold MethodInelastic Compaction in High-Porosity Limestone Monitored Using Acoustic EmissionsMechanics of Time-Dependent Deformation in Crustal RocksHydrothermal alteration of andesitic lava domes can lead to explosive volcanic behaviour
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description
researcher ORCID ID = 0000-0002-4748-735X
@en
wetenschapper
@nl
name
Michael Heap
@ast
Michael Heap
@en
Michael Heap
@es
Michael Heap
@nl
type
label
Michael Heap
@ast
Michael Heap
@en
Michael Heap
@es
Michael Heap
@nl
prefLabel
Michael Heap
@ast
Michael Heap
@en
Michael Heap
@es
Michael Heap
@nl
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P1153
15753312300
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P496
0000-0002-4748-735X