f Time domain electromagnetic, seismic refraction and potential field exploration of the Troodos ophiolite spreading structure

Mineral exploration programs in complex geological environments require a clear understanding of both regional structure and local factors influencing mineralisation. Recent submarine images of active spreading environments have shown striking parallels between present ridge structuren and ancient ophiolitic terrasnes. Geological models now present a viable framework that requires evaluation in the structural and urineral environment by geophysical means .