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Diachronous cooling on both sides of a major strike slip fault in the Variscan Maures Massif (south-east France), as deduced from a detailed 40Ar/39Ar study

✍ Scribed by Anne-Claire Morillon; Gilbert Féraud; Marc Sosson; Gilles Ruffet; Gilbert Crevola; Gilles Lerouge


Book ID
117225259
Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
517 KB
Volume
321
Category
Article
ISSN
0040-1951

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