𝔖 Bobbio Scriptorium
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Antimony cycling in the western Mediterranean

✍ Scribed by Kazufumi Takayanagi; Daniel Cossa; Jean-Marie Martin


Book ID
103690741
Publisher
Elsevier Science
Year
1996
Tongue
English
Weight
662 KB
Volume
54
Category
Article
ISSN
0304-4203

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The western Mediterranean is composed of irregular troughs formed as back‐arc basins in the hanging wall of the W‐directed Apenninic subduction which retreated eastward during Neogene and Quaternary times. The basins are progressively younger toward the east, ageing from late Oligocene–early Miocene