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He, Chuansong, Santosh, M., Chen, Xuanhua, Li, Xiaoyan (2014) Continental dynamics in a multi-convergent regime: a receiver function study from the North–South-Trending Tectonic Zone of China. International Geology Review, 56 (5) 525-536 doi:10.1080/00206814.2013.876901

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Reference TypeJournal (article/letter/editorial)
TitleContinental dynamics in a multi-convergent regime: a receiver function study from the North–South-Trending Tectonic Zone of China
JournalInternational Geology Review
AuthorsHe, ChuansongAuthor
Santosh, M.Author
Chen, XuanhuaAuthor
Li, XiaoyanAuthor
Year2014 (April 4)Volume56
Issue5
PublisherInforma UK Limited
DOIdoi:10.1080/00206814.2013.876901Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID308236Long-form Identifiermindat:1:5:308236:6
GUID0
Full ReferenceHe, Chuansong, Santosh, M., Chen, Xuanhua, Li, Xiaoyan (2014) Continental dynamics in a multi-convergent regime: a receiver function study from the North–South-Trending Tectonic Zone of China. International Geology Review, 56 (5) 525-536 doi:10.1080/00206814.2013.876901
Plain TextHe, Chuansong, Santosh, M., Chen, Xuanhua, Li, Xiaoyan (2014) Continental dynamics in a multi-convergent regime: a receiver function study from the North–South-Trending Tectonic Zone of China. International Geology Review, 56 (5) 525-536 doi:10.1080/00206814.2013.876901
In(2014, April) International Geology Review Vol. 56 (5) Informa UK Limited

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He, Chuansong, Santosh, M., Chen, Xuanhua, Li, Xiaoyan (2014) Crustal growth and tectonic evolution of the Tianshan orogenic belt, NW China: A receiver function analysis. Journal of Geodynamics, 75. 41-52 doi:10.1016/j.jog.2014.02.004
He, Chuansong, Dong, Shuwen, Chen, Xuanhua, Santosh, M., Li, Qiusheng (2014) Crustal structure and continental dynamics of Central China: A receiver function study and implications for ultrahigh-pressure metamorphism. Tectonophysics, 610. 172-181 doi:10.1016/j.tecto.2013.11.012
He, Chuansong, Dong, Shuwen, Santosh, M., Li, Qiusheng, Chen, Xuanhua (2015) Destruction of the North China Craton: a perspective based on receiver function analysis. Geological Journal, 50 (1) 93-103 doi:10.1002/gj.2530
He, Chuansong, Santosh, M., Dong, Shuwen (2015) Continental dynamics of Eastern China: Insights from tectonic history and receiver function analysis. Earth-Science Reviews, 145. 9-24 doi:10.1016/j.earscirev.2015.02.006
He, Chuansong, Santosh, M., Wu, Jianping, Chen, Xuanhua (2014) Plume or no plume: Emeishan Large Igneous Province in Southwest China revisited from receiver function analysis. Physics of the Earth and Planetary Interiors, 232. 72-78 doi:10.1016/j.pepi.2014.04.004
He, Chuansong, Dong, Shuwen, Santosh, M., Chen, Xuanhua (2014) Seismic structure of the Longmenshan area in SW China inferred from receiver function analysis: Implications for future large earthquakes. Journal of Asian Earth Sciences, 96. 226-236 doi:10.1016/j.jseaes.2014.09.026
He, Chuansong, Santosh, M. (2017) Intraplate earthquakes and their link with mantle dynamics: Insights from P-wave teleseismic tomography along the northern part of the North–South Tectonic Zone in China. Comptes Rendus Geoscience, 349 (3). 96-105 doi:10.1016/j.crte.2017.04.002
He, Chuansong, Dong, Shuwen, Santosh, M., Chen, Xuanhua (2013) Seismic Evidence for a Geosuture between the Yangtze and Cathaysia Blocks, South China. Scientific Reports, 3. doi:10.1038/srep02200
He, Chuansong, Dong, Shuwen, Chen, Xuanhua, Santosh, M., Niu, Shuyin (2014) Seismic evidence for plume-induced rifting in the Songliao Basin of Northeast China. Tectonophysics, 627. 171-181 doi:10.1016/j.tecto.2013.07.015
He, Chuansong, Santosh, M. (2020) Formation of the North–South Seismic Zone and Emeishan Large Igneous Province in Central China: Insights from P-Wave Teleseismic Tomography. Bulletin of the Seismological Society of America, 110 (6) 3064-3076 doi:10.1785/0120200067
He, Chuansong, Santosh, M. (2016) Crustal evolution and metallogeny in relation to mantle dynamics: A perspective from P-wave tomography of the South China Block. Lithos, 263. 3-14 doi:10.1016/j.lithos.2016.06.021
 
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