The Capo Castello Shear Zone (Eastern Elba Island): Deformation at the Contact between Oceanic and Continent Tectonic Units
Low-grade mylonitic shear zones are commonly characterized by strain partitioning, with alternating low strain protomylonite and high strain mylonite and ultramylonite, where the shearing is most significant. In this paper the capo Castello shear zone is analyzed. It has developed along the contact...
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| Format: | Article |
| Language: | English |
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MDPI AG
2020-09-01
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| Series: | Geosciences |
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| Online Access: | https://www.mdpi.com/2076-3263/10/9/361 |