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(2008) Early Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orogen?. Special Publication, 308. Geological Society of London. 69-90 doi:10.1144/sp308.3

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TitleEarly Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orogen?
ReportSpecial Publication
Year2008Volume308
PublisherGeological Society of London
DOIdoi:10.1144/sp308.3Search in ResearchGate
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Mindat Ref. ID435770Long-form Identifiermindat:1:5:435770:8
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Full Reference(2008) Early Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orogen?. Special Publication, 308. Geological Society of London. 69-90 doi:10.1144/sp308.3
Plain Text(2008) Early Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orogen?. Special Publication, 308. Geological Society of London. 69-90 doi:10.1144/sp308.3
In(2008) Special Publication Vol. 308. Geological Society of London

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(2003) Extensional collapse of the late Neoproterozoic-early Palaeozoic East African-Antarctic Orogen in central Dronning Maud Land, East Antarctica, in Proterozoic East Gondwana: Supercontinent Assembly and Breakup. Special Publication, 206. Geological Society of London. 271-287 doi:10.1144/gsl.sp.2003.206.01.14
(2008) Geochemistry of post‐kinematic mafic dykes from central to eastern Dronning Maud Land, East Antarctica: evidence for a Pan-African suture in Dronning Maud Land. Special Publication, 308. Geological Society of London. 235-252 doi:10.1144/sp308.12
(2017) Geological studies in the Baalsrudfjellet nunatak between the Schirmacher Oasis and the Wohlthat Mountains to establish the continuation of the East African Orogen (EAO) in central Dronning Maud Land, East Antarctica. Special Publication, 457. Geological Society of London. 37-59 doi:10.1144/sp457.3
(2008) Contrasting metamorphic P–T path between Schirmacher Hills and Mühlig-Hofmannfjella, central Dronning Maud Land, East Antarctica. Special Publication, 308. Geological Society of London. 401-417 doi:10.1144/sp308.20
(2003) Implications of late Pan-African shearing in western Dronning Maud Land, Antarctica. Special Publication, 210. Geological Society of London. 135-143 doi:10.1144/gsl.sp.2003.210.01.08
(2008) Geochronological constraints on the Late Proterozoic to Cambrian crustal evolution of eastern Dronning Maud Land, East Antarctica: a synthesis of SHRIMP U-Pb age and Nd model age data. Special Publication, 308. Geological Society of London. 21-67 doi:10.1144/sp308.2
(2008) Early Palaeozoic metasomatism of the Archaean Napier Complex, East Antarctica. Special Publication, 308. Geological Society of London. 283-316 doi:10.1144/sp308.14
(2013) Contrasting metamorphic records and their implications for tectonic process in the central Sør Rondane Mountains, eastern Dronning Maud Land, East Antarctica. Special Publication, 383. Geological Society of London. 113-133 doi:10.1144/sp383.4
(1996) The development of the crust off Dronning Maud Land, East Antarctica. Special Publication, 108. Geological Society of London. 243-264 doi:10.1144/gsl.sp.1996.108.01.18
(2001) Pervasive Pan-African reactivation of the Grenvillian crust and large igneous intrusions in central Dronning Maud Land, East Antarctica, in Continental reactivation and reworking. Special Publication, 184. Geological Society of London. 343-355 doi:10.1144/gsl.sp.2001.184.01.17
Jacobs, J, Bauer, W, Fanning, C.M (2003) Late Neoproterozoic/Early Palaeozoic events in central Dronning Maud Land and significance for the southern extension of the East African Orogen into East Antarctica. Precambrian Research, 126 (1) 27-53 doi:10.1016/s0301-9268(03)00125-6
 
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