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- Publisher Website: 10.1007/s11434-006-2152-7
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Article: Electron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism?
Title | Electron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism? |
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Authors | |
Keywords | Electron Microprobe Dating Late Pan-African Thermal Event Monazite Qinling Orogen |
Issue Date | 2006 |
Publisher | Science China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/ |
Citation | Chinese Science Bulletin, 2006, v. 51 n. 21, p. 2645-2650 How to Cite? |
Abstract | Electron microprobe chemical dating was carried out on monazites enclosed in two generations of mineral paragenesis of St + Ky + Grt and Sil + And + Grt + St, respectively, from the Qinling Group. Two different ages, 520±23 Ma and 435±9 Ma, were obtained from these monazites. This indicates that the Qinling Group experienced a metamorphism during the Early Cambrian, which is probably in response to the Late Pan-African subduction-accretion tectonothermal event. © 2006 Science in China Press. |
Persistent Identifier | http://hdl.handle.net/10722/151200 |
ISSN | 2016 Impact Factor: 1.649 |
ISI Accession Number ID | |
References |
DC Field | Value | Language |
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dc.contributor.author | Chen, Q | en_US |
dc.contributor.author | Chen, N | en_US |
dc.contributor.author | Wang, Q | en_US |
dc.contributor.author | Sun, M | en_US |
dc.contributor.author | Wang, X | en_US |
dc.contributor.author | Li, X | en_US |
dc.contributor.author | Shu, G | en_US |
dc.date.accessioned | 2012-06-26T06:18:35Z | - |
dc.date.available | 2012-06-26T06:18:35Z | - |
dc.date.issued | 2006 | en_US |
dc.identifier.citation | Chinese Science Bulletin, 2006, v. 51 n. 21, p. 2645-2650 | en_US |
dc.identifier.issn | 1001-6538 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/151200 | - |
dc.description.abstract | Electron microprobe chemical dating was carried out on monazites enclosed in two generations of mineral paragenesis of St + Ky + Grt and Sil + And + Grt + St, respectively, from the Qinling Group. Two different ages, 520±23 Ma and 435±9 Ma, were obtained from these monazites. This indicates that the Qinling Group experienced a metamorphism during the Early Cambrian, which is probably in response to the Late Pan-African subduction-accretion tectonothermal event. © 2006 Science in China Press. | en_US |
dc.language | eng | en_US |
dc.publisher | Science China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/ | en_US |
dc.relation.ispartof | Chinese Science Bulletin | en_US |
dc.subject | Electron Microprobe Dating | en_US |
dc.subject | Late Pan-African Thermal Event | en_US |
dc.subject | Monazite | en_US |
dc.subject | Qinling Orogen | en_US |
dc.title | Electron microprobe chemical ages of monazite from Qinling Group in the Qinling Orogen: Evidence for Late Pan-African metamorphism? | en_US |
dc.type | Article | en_US |
dc.identifier.email | Sun, M:minsun@hku.hk | en_US |
dc.identifier.authority | Sun, M=rp00780 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.doi | 10.1007/s11434-006-2152-7 | en_US |
dc.identifier.scopus | eid_2-s2.0-33751006627 | en_US |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-33751006627&selection=ref&src=s&origin=recordpage | en_US |
dc.identifier.volume | 51 | en_US |
dc.identifier.issue | 21 | en_US |
dc.identifier.spage | 2645 | en_US |
dc.identifier.epage | 2650 | en_US |
dc.identifier.isi | WOS:000242914600014 | - |
dc.publisher.place | China | en_US |
dc.identifier.scopusauthorid | Chen, Q=35478183900 | en_US |
dc.identifier.scopusauthorid | Chen, N=12796732200 | en_US |
dc.identifier.scopusauthorid | Wang, Q=14046248000 | en_US |
dc.identifier.scopusauthorid | Sun, M=25932315800 | en_US |
dc.identifier.scopusauthorid | Wang, X=7501858663 | en_US |
dc.identifier.scopusauthorid | Li, X=23469678400 | en_US |
dc.identifier.scopusauthorid | Shu, G=14046160500 | en_US |
dc.identifier.issnl | 1001-6538 | - |