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Conference Paper: An introduction to the major NSFC Program 'Reconstruction of East Asian Blocks in Pangea'

TitleAn introduction to the major NSFC Program 'Reconstruction of East Asian Blocks in Pangea'
Authors
Keywords8103 TECTONOPHYSICS Continental cratons
8102 TECTONOPHYSICS Continental contractional orogenic belts and inversion tectonics
8125 TECTONOPHYSICS Evolution of the Earth
8157 TECTONOPHYSICS Plate motions: past
Issue Date2013
PublisherThe Smithsonian/NASA Astrophysics Data System.
Citation
The 2013 Fall Meeting of the American Geophysical Union (AGU), San Francisco, CA., 9-13 December 2013. How to Cite?
AbstractPangea is the youngest supercontinent in Earth's history and its main body formed about 250 million years ago. As supported by voluminous evidence from reliable geological, paleomagnetic and paleontological data, configurations of major continental blocks in Pangea have been widely accepted. However, controversy has long surrounded the reconstructions of East Asian blocks in Pangea. So far, most Pangea reconstructions assume that continental blocks in East Asia had never become parts of Pangea before its breakup. In these reconstruction models, configurations of East Asian blocks in Pangea were mainly based on geological and paleomagnetic data before the 1990's but did not fully consider recent data produced by Chinese researchers about collisional mountain belts between continental blocks in East Asia. To precisely reconstruct the East Asian blocks in Pangea, the Natural Science Foundation of China (NSFC) recently set up a Major NSFC Program entitled 'Reconstruction of East Asian Blocks in Pangea'. On the basis of summarizing and integrating previous data, this major program will carry out detailed field-based structural, metamorphic, geochemical, geochronological, paleomagnetic and paleontonological investigations on key segments of the Central Asian Orogenic Belt, Central China Orogenic Belt and Paleo-Tethys Belt, which assembled major continental blocks in East Asia, in order to determine the timing and processes of opening and closuring of the Paleo-Asian Ocean, Proto-Tethyan Ocean (Qin-Qi-Kun Ocean) and Paleo-Tethyan Ocean. The program will not only answer where, when and how continental blocks in East Asia were assembled and whether or not they had become parts of Pangea before the breakup of the supercontinent, but will also improve and develop the theory of plate tectonics.
Descriptionabstract no. T41C-2595
Persistent Identifierhttp://hdl.handle.net/10722/201840

 

DC FieldValueLanguage
dc.contributor.authorZhao, Gen_US
dc.contributor.authorZhang, Gen_US
dc.contributor.authorWang, Yen_US
dc.contributor.authorHuang, Ben_US
dc.contributor.authorDong, Yen_US
dc.contributor.authorLi, Sen_US
dc.contributor.authorXiao, W-
dc.date.accessioned2014-08-21T07:44:27Z-
dc.date.available2014-08-21T07:44:27Z-
dc.date.issued2013en_US
dc.identifier.citationThe 2013 Fall Meeting of the American Geophysical Union (AGU), San Francisco, CA., 9-13 December 2013.en_US
dc.identifier.urihttp://hdl.handle.net/10722/201840-
dc.descriptionabstract no. T41C-2595-
dc.description.abstractPangea is the youngest supercontinent in Earth's history and its main body formed about 250 million years ago. As supported by voluminous evidence from reliable geological, paleomagnetic and paleontological data, configurations of major continental blocks in Pangea have been widely accepted. However, controversy has long surrounded the reconstructions of East Asian blocks in Pangea. So far, most Pangea reconstructions assume that continental blocks in East Asia had never become parts of Pangea before its breakup. In these reconstruction models, configurations of East Asian blocks in Pangea were mainly based on geological and paleomagnetic data before the 1990's but did not fully consider recent data produced by Chinese researchers about collisional mountain belts between continental blocks in East Asia. To precisely reconstruct the East Asian blocks in Pangea, the Natural Science Foundation of China (NSFC) recently set up a Major NSFC Program entitled 'Reconstruction of East Asian Blocks in Pangea'. On the basis of summarizing and integrating previous data, this major program will carry out detailed field-based structural, metamorphic, geochemical, geochronological, paleomagnetic and paleontonological investigations on key segments of the Central Asian Orogenic Belt, Central China Orogenic Belt and Paleo-Tethys Belt, which assembled major continental blocks in East Asia, in order to determine the timing and processes of opening and closuring of the Paleo-Asian Ocean, Proto-Tethyan Ocean (Qin-Qi-Kun Ocean) and Paleo-Tethyan Ocean. The program will not only answer where, when and how continental blocks in East Asia were assembled and whether or not they had become parts of Pangea before the breakup of the supercontinent, but will also improve and develop the theory of plate tectonics.-
dc.languageengen_US
dc.publisherThe Smithsonian/NASA Astrophysics Data System.-
dc.relation.ispartofAGU Fall Meeting 2013en_US
dc.subject8103 TECTONOPHYSICS Continental cratons-
dc.subject8102 TECTONOPHYSICS Continental contractional orogenic belts and inversion tectonics-
dc.subject8125 TECTONOPHYSICS Evolution of the Earth-
dc.subject8157 TECTONOPHYSICS Plate motions: past-
dc.titleAn introduction to the major NSFC Program 'Reconstruction of East Asian Blocks in Pangea'en_US
dc.typeConference_Paperen_US
dc.identifier.emailZhao, G: gzhao@hkucc.hku.hken_US
dc.identifier.authorityZhao, G=rp00842en_US
dc.description.naturelink_to_OA_fulltext-
dc.identifier.hkuros234182en_US
dc.publisher.placeUnited States-

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