Tectonic transition from thrusting to polyphase non-confining deformation within the Semail Ophiolite along the sinistral, transtensional Issmaiya Fault Zone (Sultanate of Oman)

Ivan Callegari*, Andreas Scharf, Frank Mattern, Katharina Scharf

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

4 Citations (Scopus)

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Earth and Planetary Sciences