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  Rock Deformation Laboratory, Department of Earth and Ocean Sciences  
 

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

Vein
Quartz growth
   
Valley of the moons
Working
The Team
Superbly preserved fault gouge
Looking along strike of the Caleta Collosso Fault
Oasis
Tomato pan tennis
Sample prep

Southern Spain

Cataclastic texture
Our fave beach
Superb bands of coloured fault gouge on the Carboneras Fault, looking along strike
Tight folding in schists
Fault gouge bands
   
Riedal shears
View of mapping area

 

 

 
       

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