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Fieldwork
In the lab we are very conscious of the need to relate
laboratory work with nature. To this end, we have a very active field
programme that is concentrated on elucidating the internal structure
of major strike-slip fault zones. For this work, we require large faults
with significant displacements that have recently been exhumed from
seismogenic depths, and are exposed in arid or semi-arid environments
in order to preserve the fragile fault rocks. Two faults that fit this
billing exceptionally well are the Atacama fault zone in northern Chile
and the Carboneras fault zone in southern Spain.
Chile |
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Vein |
Quartz growth |
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Valley of the moons |
Working |
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The Team |
Superbly preserved fault gouge |
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Looking along strike of the Caleta Collosso
Fault |
Oasis |
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Tomato pan tennis |
Sample prep |
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Southern Spain
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Cataclastic texture |
Our fave beach |
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Superb bands of coloured fault gouge on
the Carboneras Fault, looking along strike |
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Tight folding in schists |
Fault gouge bands |
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Riedal shears |
View of mapping area |
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