His primary areas of investigation include Metamorphism, Geochemistry, Metamorphic rock, Mineralogy and Paleontology. M. A. Etheridge has researched Metamorphism in several fields, including Porosity, Composite material, Deformation, Permeability and Foliation. As a part of the same scientific family, he mostly works in the field of Permeability, focusing on Mass transfer and, on occasion, Petrology.
His Geochemistry research includes elements of Restite and Fold. M. A. Etheridge combines subjects such as Layer, Displacement and Microstructure with his study of Mineralogy. His studies in Detachment fault integrate themes in fields like Passive margin, Volcanic passive margin and Continental margin.
The scientist’s investigation covers issues in Mineralogy, Geochemistry, Petrology, Mylonite and Tectonics. He has included themes like Quartz and Dynamic recrystallization in his Mineralogy study. In general Geochemistry study, his work on Metamorphic rock, SLATES and Pyrite often relates to the realm of Arsenopyrite, thereby connecting several areas of interest.
His work deals with themes such as Mass transfer and Permeability, which intersect with Metamorphic rock. His studies deal with areas such as Shear zone and Lithosphere as well as Petrology. His Mylonite study incorporates themes from Slip, Strain rate, Gneiss and Grain boundary.
His scientific interests lie mostly in Passive margin, Paleontology, Petrology, Fold and Lithosphere. His work in the fields of Volcanic passive margin overlaps with other areas such as Conjugate. His Petrology study combines topics in areas such as Deformation mechanism and Deformation.
His work investigates the relationship between Fold and topics such as SLATES that intersect with problems in Lode and Metamorphic rock. His Lithosphere research is multidisciplinary, relying on both Extensional definition, Metamorphism and Mantle. The study incorporates disciplines such as Fault and Mineralogy in addition to Geochemistry.
Arunta, Proterozoic, Northern australia, Paleontology and Tectonics are his primary areas of study.
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Detachment faulting and the evolution of passive continental margins
G. S. Lister;M. A. Etheridge;P. A. Symonds.
Geology (1986)
High fluid pressures during regional metamorphism and deformation: Implications for mass transport and deformation mechanisms
M. A. Etheridge;V. J. Wall;S. F. Cox;R. H. Vernon.
Journal of Geophysical Research (1984)
The role of the fluid phase during regional metamorphism and deformation
M. A. Etheridge;V. J. Wall;R. H. Vernon.
Journal of Metamorphic Geology (1983)
Detachment models for the formation of passive continental margins
G. S. Lister;M. A. Etheridge;P. A. Symonds.
Tectonics (1991)
Shape and microstructure of microgranitoid enclaves: Indicators of magma mingling and flow
R.H. Vernon;M.A. Etheridge;V.J. Wall.
Lithos (1988)
Deformational and metamorphic processes in the formation of mesothermal vein-hosted gold deposits — examples from the Lachlan Fold Belt in central Victoria, Australia
S.F. Cox;V.J. Wall;M.A. Etheridge;T.F. Potter.
Ore Geology Reviews (1991)
Microstructure of mylonites and their descriptive terminology
T.H. Bell;M.A. Etheridge.
Lithos (1973)
Orogenesis and Tectonic Process in the Early to Middle Proterozoic of Northern Australia
M.A. Etheridge;R.W.R. Rutland;L.A.I. Wyborn.
(2013)
Differential stress magnitudes during regional deformation and metamorphism: Upper bound imposed by tensile fracturing
M. A. Etheridge.
Geology (1983)
Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructures
S.F. Cox;M.A. Etheridge.
Tectonophysics (1983)
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