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Article: Discovery of probable Tunguska cosmic body material: Anomalies of platinum group elements and rare-earth elements in peat near the Explosion Site (1908)
Title | Discovery of probable Tunguska cosmic body material: Anomalies of platinum group elements and rare-earth elements in peat near the Explosion Site (1908) |
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Authors | |
Keywords | Element anomalies ICP-MS PGE REE Tunguska explosion |
Issue Date | 2000 |
Publisher | Pergamon. The Journal's web site is located at http://www.elsevier.com/locate/pss |
Citation | Planetary And Space Science, 2000, v. 48 n. 15, p. 1447-1455 How to Cite? |
Abstract | Ten Sphagnum fuscum peat samples collected from different depths of a core including the layer affected by the 1908 Tunguska explosion in the Tunguska area of Central Siberia, Russia, were analyzed by ICP-MS to determine the concentrations of Pd, Rh, Ru, Co, REE, Y, Sr, and Sc. The analytical results indicate that the Pd and Rh concentrations in the event- and lower layers were 14.0-19.9, and 1.23-1.56 ppb, respectively, about 3-9 times and 3 times higher than the background values in the normal layers. In addition, the patterns of CI-chondrite-normalized REE in the event layers were much flatter than in the normal layers, and differed from those in the nearby traps. Hence, it can be inferred from the characteristics of the elemental geochemistry that the explosion was probably associated with extraterrestrial material, and which, most probably, was a small comet core the dust fraction of which was chemically similar to carbonaceous chondrites (CI). In terms of the Pd and REE excess fluxes in the explosion area, it can be estimated that the celestial body that exploded over Tunguska in 1908 weighed more than 106 t, corresponding to a radius of > 60 m. If the celestial body was a comet, then its total mass was more than 2 × 107 t, and it had > 160 m radius, and released an energy of > 107 t TNT. © 2000 Elsevier Science Ltd. All rights reserved. |
Persistent Identifier | http://hdl.handle.net/10722/73068 |
ISSN | 2023 Impact Factor: 1.8 2023 SCImago Journal Rankings: 0.611 |
ISI Accession Number ID | |
References |
DC Field | Value | Language |
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dc.contributor.author | Hou, QL | en_HK |
dc.contributor.author | Kolesnikov, EM | en_HK |
dc.contributor.author | Xie, LW | en_HK |
dc.contributor.author | Zhou, MF | en_HK |
dc.contributor.author | Sun, M | en_HK |
dc.contributor.author | Kolesnikova, NV | en_HK |
dc.date.accessioned | 2010-09-06T06:47:45Z | - |
dc.date.available | 2010-09-06T06:47:45Z | - |
dc.date.issued | 2000 | en_HK |
dc.identifier.citation | Planetary And Space Science, 2000, v. 48 n. 15, p. 1447-1455 | en_HK |
dc.identifier.issn | 0032-0633 | en_HK |
dc.identifier.uri | http://hdl.handle.net/10722/73068 | - |
dc.description.abstract | Ten Sphagnum fuscum peat samples collected from different depths of a core including the layer affected by the 1908 Tunguska explosion in the Tunguska area of Central Siberia, Russia, were analyzed by ICP-MS to determine the concentrations of Pd, Rh, Ru, Co, REE, Y, Sr, and Sc. The analytical results indicate that the Pd and Rh concentrations in the event- and lower layers were 14.0-19.9, and 1.23-1.56 ppb, respectively, about 3-9 times and 3 times higher than the background values in the normal layers. In addition, the patterns of CI-chondrite-normalized REE in the event layers were much flatter than in the normal layers, and differed from those in the nearby traps. Hence, it can be inferred from the characteristics of the elemental geochemistry that the explosion was probably associated with extraterrestrial material, and which, most probably, was a small comet core the dust fraction of which was chemically similar to carbonaceous chondrites (CI). In terms of the Pd and REE excess fluxes in the explosion area, it can be estimated that the celestial body that exploded over Tunguska in 1908 weighed more than 106 t, corresponding to a radius of > 60 m. If the celestial body was a comet, then its total mass was more than 2 × 107 t, and it had > 160 m radius, and released an energy of > 107 t TNT. © 2000 Elsevier Science Ltd. All rights reserved. | en_HK |
dc.language | eng | en_HK |
dc.publisher | Pergamon. The Journal's web site is located at http://www.elsevier.com/locate/pss | en_HK |
dc.relation.ispartof | Planetary and Space Science | en_HK |
dc.subject | Element anomalies | en_HK |
dc.subject | ICP-MS | en_HK |
dc.subject | PGE | en_HK |
dc.subject | REE | en_HK |
dc.subject | Tunguska explosion | en_HK |
dc.title | Discovery of probable Tunguska cosmic body material: Anomalies of platinum group elements and rare-earth elements in peat near the Explosion Site (1908) | en_HK |
dc.type | Article | en_HK |
dc.identifier.openurl | http://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0032-0633&volume=48&spage=1447&epage=1455&date=2000&atitle=Discovery+of+probable+Tunguska+cosmic+body+material:+anomalies+of+platinum+group+elements+and+rare-earth+elements+in+peat+near+the+Explosion+Site+(1908) | en_HK |
dc.identifier.email | Zhou, MF:mfzhou@hkucc.hku.hk | en_HK |
dc.identifier.email | Sun, M:minsun@hku.hk | en_HK |
dc.identifier.authority | Zhou, MF=rp00844 | en_HK |
dc.identifier.authority | Sun, M=rp00780 | en_HK |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.scopus | eid_2-s2.0-0000260785 | en_HK |
dc.identifier.hkuros | 57995 | en_HK |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-0000260785&selection=ref&src=s&origin=recordpage | en_HK |
dc.identifier.volume | 48 | en_HK |
dc.identifier.issue | 15 | en_HK |
dc.identifier.spage | 1447 | en_HK |
dc.identifier.epage | 1455 | en_HK |
dc.identifier.isi | WOS:000166163300004 | - |
dc.publisher.place | United Kingdom | en_HK |
dc.identifier.scopusauthorid | Hou, QL=7005883718 | en_HK |
dc.identifier.scopusauthorid | Kolesnikov, EM=7005694781 | en_HK |
dc.identifier.scopusauthorid | Xie, LW=8523115400 | en_HK |
dc.identifier.scopusauthorid | Zhou, MF=7403506005 | en_HK |
dc.identifier.scopusauthorid | Sun, M=25932315800 | en_HK |
dc.identifier.scopusauthorid | Kolesnikova, NV=7005912139 | en_HK |
dc.identifier.issnl | 0032-0633 | - |