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Page 1: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 2: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 3: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 4: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 5: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 6: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 7: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to
Page 8: repositorio-aberto.up.ptwhich is included in a major crustal—scale strike-slip zone, the so-called Porto—Coimbra—Tomar shear zone. This crystalline basement ranges from 1 to

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