Geophysical analysis of fault geometry and volcanic activity in the Erzincan Basin, Central Turkey: Complex evolution of a mature pull-apart basin
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文摘

The Erzincan Basin has a Plio-Quaternary history comprising at least two phases.

Gravity and magnetic studies and surface mapping define a complex fracture system.

Basin cross faulting with variable thick infill define a mature pull-apart advancing to extinction.

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