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  1. Ian Main FRSE, FRSA, MAE, Professor of Seismology and Rock Physics. Research Ian is interested in the processes that lead up to catastrophic failure events, from earthquakes, rock fracture, and volcanic eruptions to failure of building materials and bridges, and in quantifying the resulting hazard. He is particularly interested in the ...

    • Biography

      Ian got his first taste for research from a Carnegie...

    • Research

      Ian Main’s personal web page. Research. Overview of Research...

    • Publications

      Ian Main’s personal web page. Publications. Citations by...

    • Postgraduate Studentships

      Ian Bastow (Edinburgh) M Res ‘A comparison of moment tensors...

    • Teaching

      I currently teach the geophysical component of Earth...

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  2. 1601. 2001. Assessing Damage of Reinforced Concrete Beam Using “ b -value” Analysis of Acoustic Emission Signals. IS Colombo, IG Main, MC Forde. Journal of materials in civil engineering 15 (3), 280-286. , 2003. 615. 2003. Operational earthquake forecasting: State of knowledge and guidelines for utilization.

  3. Ian Mains personal web page. Publications. Citations by Google Scholar, SCOPUS and ISI Web of Science. NB Open Access versions of these publications, where available, can be downloaded from HERE. Refereed research papers. Main, I.G. & P.W. Burton (1981).

  4. Dive into the research topics where Ian Main is active. These topic labels come from the works of this person. Together they form a unique fingerprint.

  5. Ian Mains personal web page. Research. Overview of Research Interests. Summary. We live on a dynamic planet, whose upper layers respond in a brittle fashion to slow forcing from the underlying mantle. This takes the form of localised earthquake faulting on a large scale, and fracturing on a much smaller scale.

  6. Ian G Main. Time-dependent brittle deformation is a fundamental and pervasive process operating in the Earth's upper crust. Its characterization is a pre-requisite to understanding and...

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  8. Ian G Main We investigate the scaling properties of the sources of crackling noise in a fully dynamic numerical model of sedimentary rocks subject to uniaxial compression.

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