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Tectono-metamorphic history of Neoproterozoic rocks in eastern Eritrea
Uppsala University.
1999 (English)In: PRECAMBRIAN RESEARCH, ISSN 0301-9268, Vol. 98, no 1-2, 83-105 p.Article in journal (Other scientific) Published
Abstract [en]

The Neoproterozoic juvenile crust of Eritrea lies within the East African Orogen that marks a megasuture along which the East and West Gondwana converged. In eastern Eritrea, repeatedly deformed Neoproterozoic rocks of this orogen consist of two lithotect

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1999. Vol. 98, no 1-2, 83-105 p.
Keyword [en]
East African Orogen; geothermobarometry; Gondwana; isostatic root recovery; Neoproterozoic; ARABIAN-NUBIAN SHIELD; LOW-P; GARNET; OPHIOLITES; EVOLUTION; ACCRETION; BASEMENT; CALIBRATION; CONSTRAINTS; NORTHEAST
URN: urn:nbn:se:uu:diva-27704OAI: oai:DiVA.org:uu-27704DiVA: diva2:55600
Addresses: Ghebreab W, Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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