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Quartz-vein system development during progressive deformation in low-grade siliciclastic sediments: Evidence from the Palaeozoic of the Armorican Massif (Brittany, France)

✍ Scribed by Isaac Berwouts; Philippe Muchez; Thérèse Lhomme; Manuel Sintubin


Book ID
116511603
Publisher
Elsevier Science
Year
2009
Tongue
English
Weight
74 KB
Volume
101
Category
Article
ISSN
0375-6742

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