The break-up of East Gondwana along the northeast coast of Oman: Evidence from the Batain basin
- Author(s)
- Marc Hauser, Rossana Martini, Albert Matter, Leopold Krystyn, Tjerk Peters, Gerard Stampfli, Louisette Zaninetti
- Abstract
Recent detailed studies on the Batain nappes (northeast coast of Oman), which represent a special part of the so-called 'Oman Exotics', have led to a better understanding of the Neotethyan geodynamic evolution. The Batain Exotics bear witness to volcanic activity, sea-level changes, tectonic instability, rifting and oceanization along the Eastern Oman margin during Late Palaeozoic and Mesozoic times. They allow definition of the Batain basin as an aborted Permian branch of Neotethys. This marine basin was created in Early Permian times extending southward to the East African/Madagascar region and was linked to the Karoo rift system. The presented revised classification of the Batain nappes considers the Batain basin to be no longer a part of the Hawasina basin and the Neotethyan margin proper. We attribute the Batain basin to a Mozambique Somali-Masirah rift system (Somoma). This system started in Early Permian, times, creating a marine basin between Arabia and India/Madagascar; rifting in the Late Triassic and oceanization during Late Jurassic times led to the separation of East Gondwana.
- Organisation(s)
- Department of Palaeontology
- External organisation(s)
- Université Lille I - Sciences et Technologies, Université de Genève, Universität Bern, Université de Lausanne
- Journal
- Geological Magazine
- Volume
- 139
- Pages
- 145-157
- No. of pages
- 13
- ISSN
- 0016-7568
- Publication date
- 2002
- Peer reviewed
- Yes
- Austrian Fields of Science 2012
- 105118 Palaeontology
- Sustainable Development Goals
- SDG 14 - Life Below Water
- Portal url
- https://ucrisportal.univie.ac.at/en/publications/cf535db7-dbcc-4f01-9eda-9d788682379b