Dear All
Apologize for cross-posting.
I would like to invite you to submit your contribution (abstract) to "The Gondwana" session
(EGU2013 - Vienna 7-12 April, 2013).
http://meetingorganizer.copernicus.org/EGU2013/session/12077
Important Deadlines
- Support application (30 November 2012)
- Abstract submission (09 January 2013)
The Gondwana
This session aims to draw the tectonic evolution of the orogenies
that were formed due to the collision between East- and West-Gondwana
(Pan-African, Brasiliano, Adelaidean and Beardmore orogenies). The
collision between East- and West-Gondwana was associated by closure of
several major Neoproterozoic oceans (Kröner & Stern, 2004). These
are the Mozambique Ocean between East Gondwana (Australia, Antarctica,
southern India) and West Gondwana (Africa, South America), the Adamastor
Ocean between Africa and South America, the Damara Ocean between the
Kalahari and Congo cratons, and the Trans-Sahara Ocean between the West
African Craton and a poorly known pre-Pan-African terrane in
north-central Africa (Klerkx & Deutsch, 1977; Toteu et al., 1990;
Black & Liegeois, 1993) variously known as the Nile or Sahara
Craton.
This session will discuss any rock type which was formed or deformed
during the collision. As well as it will discuss the structural elements
those were formed during the collision.
Have a good day
Tamer
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Mag.Dr.rer.nat. Tamer Abu-Alam
Researcher , Graz Univ., Austria
Assistance prof. of Geology, Tanta Univ.,
Egypt
[log in to unmask][log in to unmask]Phone: 0043-316-380-5680
http://wegener.kfunigraz.ac.at/group/tabualam/tamerindex.html
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