1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar.
Our recent geological survey of the basement of central and northern Madagascar allowed us to re-evaluate the evolution of this part of the East Africa-Antarctica Orogen (EAAO). Five crustal domains are recognised, characterised by distinctive lithologies and histories of sedimentation, magmatism, d...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.452.5540 2023-05-15T14:02:25+02:00 1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. R. M. Key C. Potter R. A. Smith The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.5540 http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.5540 http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf text ftciteseerx 2016-01-08T05:58:22Z Our recent geological survey of the basement of central and northern Madagascar allowed us to re-evaluate the evolution of this part of the East Africa-Antarctica Orogen (EAAO). Five crustal domains are recognised, characterised by distinctive lithologies and histories of sedimentation, magmatism, deformation and metamorphism, and separated by tectonic and/or unconformable contacts. Four consist largely of Archaean metamorphic rocks (Antongil, Masora and Antananarivo Cratons, Tsaratanana Complex). The fifth (Bemarivo Belt) comprises Proterozoic meta-igneous rocks. The Text Antarc* Antarctica Unknown |
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English |
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Our recent geological survey of the basement of central and northern Madagascar allowed us to re-evaluate the evolution of this part of the East Africa-Antarctica Orogen (EAAO). Five crustal domains are recognised, characterised by distinctive lithologies and histories of sedimentation, magmatism, deformation and metamorphism, and separated by tectonic and/or unconformable contacts. Four consist largely of Archaean metamorphic rocks (Antongil, Masora and Antananarivo Cratons, Tsaratanana Complex). The fifth (Bemarivo Belt) comprises Proterozoic meta-igneous rocks. The |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R. M. Key C. Potter R. A. Smith |
spellingShingle |
R. M. Key C. Potter R. A. Smith 1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
author_facet |
R. M. Key C. Potter R. A. Smith |
author_sort |
R. M. Key |
title |
1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
title_short |
1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
title_full |
1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
title_fullStr |
1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
title_full_unstemmed |
1 Polyphase Neoproterozoic orogenesis within the East Africa-Antarctica Orogenic Belt in central and northern Madagascar. |
title_sort |
1 polyphase neoproterozoic orogenesis within the east africa-antarctica orogenic belt in central and northern madagascar. |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.5540 http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.5540 http://nora.nerc.ac.uk/15741/1/Final_Revised_after_review.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766272690958630912 |