New data on the trace element composition and Lu-Hf isotopic system of zircons from the Early Cambrian granites of the Ufaley block (Middle Urals): a step to the correction of geodynamic concepts

Research subject . Composition and isotopic parameters of zircons and their host granites of the Bitim complex, localised in the eastern part of the Ufaley block (Middle Urals). Materials and methods . The determination of trace element composition and Lu-Hf isotope system in zircons was carried out...

Full description

Saved in:
Bibliographic Details
Published inLitosfera (Ekaterinburg. Online) Vol. 22; no. 1; pp. 55 - 74
Main Author Shardakova, G. Yu
Format Journal Article
LanguageEnglish
Russian
Published 02.03.2022
Online AccessGet full text
ISSN1681-9004
2500-302X
DOI10.24930/1681-9004-2022-22-1-55-74

Cover

Abstract Research subject . Composition and isotopic parameters of zircons and their host granites of the Bitim complex, localised in the eastern part of the Ufaley block (Middle Urals). Materials and methods . The determination of trace element composition and Lu-Hf isotope system in zircons was carried out by LA-ICP-MS (the “Geoanalitik” shared research facilities of the IGG UB RAS, Ekaterinburg). Results and conclusions . The images and geochemical features of the main zircon population from granites confirm their magmatic genesis and minimal alteration, which proves previously defined Vendian- Cambrian (520 ± 9 Ma) age for the granites. Younger zircons (401–459 Ma) differing in composition from the older ones, were formed during subsequent tectonic-thermal activity, possibly under the fluid action. The mixed mantle-crustal nature of substrate for the granite melting is indicated by specific isotopic parameters (87Sr/86Sr = 0.703389, εHf(t)aver = +6.3) and a number of characteristic ratios for zircons and granites. The geodynamic concepts of the granite formation settings of the Bitim complex are corrected: in the Vendian–Early Cambrian, a transform-type margin has developed in this sector, the divergent movements on which have been accompanied by a break in the continuity of the crust and the intrusion of a deep mantle diapir; the participation of the slab substance in the magma generation might also be assumed. Conclusions . The results obtained can be used for the geological mapping and correction of a general geodynamic scheme for the junction zone between the Ural Mobile Belt and the East European platform.
AbstractList Research subject . Composition and isotopic parameters of zircons and their host granites of the Bitim complex, localised in the eastern part of the Ufaley block (Middle Urals). Materials and methods . The determination of trace element composition and Lu-Hf isotope system in zircons was carried out by LA-ICP-MS (the “Geoanalitik” shared research facilities of the IGG UB RAS, Ekaterinburg). Results and conclusions . The images and geochemical features of the main zircon population from granites confirm their magmatic genesis and minimal alteration, which proves previously defined Vendian- Cambrian (520 ± 9 Ma) age for the granites. Younger zircons (401–459 Ma) differing in composition from the older ones, were formed during subsequent tectonic-thermal activity, possibly under the fluid action. The mixed mantle-crustal nature of substrate for the granite melting is indicated by specific isotopic parameters (87Sr/86Sr = 0.703389, εHf(t)aver = +6.3) and a number of characteristic ratios for zircons and granites. The geodynamic concepts of the granite formation settings of the Bitim complex are corrected: in the Vendian–Early Cambrian, a transform-type margin has developed in this sector, the divergent movements on which have been accompanied by a break in the continuity of the crust and the intrusion of a deep mantle diapir; the participation of the slab substance in the magma generation might also be assumed. Conclusions . The results obtained can be used for the geological mapping and correction of a general geodynamic scheme for the junction zone between the Ural Mobile Belt and the East European platform.
Author Shardakova, G. Yu
Author_xml – sequence: 1
  givenname: G. Yu
  surname: Shardakova
  fullname: Shardakova, G. Yu
  organization: A.N. Zavaritsky Institute of Geology and Geochemistry, Urals Branch of RAS
BookMark eNqNUctu1TAQtVCRuJT-w4gVLEwnzsNJV6CrQpEusKESu2iuH8WQ2JHtqgq_x4_hXBALVkgj2Zo558zMmafszAdvGHte4SvRDDVeVl1f8QGx4QKF4CUq3rZcNo_YTrSIvEbx5Yzt_uKesIuUviGi6GWHKHfs50fzAJoyQfCQvxrIkZQBM5nZ-AwqzEtILrtSJa_hcM9vLLgUclicgrSmbGYIFn64qIJPYGOYTzrXFKcV9jQfoyMPd5G8yyZt2K18a2kyKxynoL7Diw9O66kkI03p5RUQFNkFcjhBVYjRqNMIhXxngl49zaV7aajMktMz9rioJXPx5z1nt2-vP-9v-OHTu_f7NweuRF08arS1Vd-TPlLTdt1R9TVqgWTKv5HWSlPVzYCKamplbTrRDQpl1-qWUA5S1-fs6reuiiGlaOy4RDdTXMcKx9NFxs3pcXN63C4ylqjGth1lU8iv_yErl2nbqjjupv-R-AU_-Jfj
CitedBy_id crossref_primary_10_24930_2500_302X_2024_24_5_767_784
Cites_doi 10.1016/j.lithos.2007.06.016
10.2138/am.2010.3521
10.2113/0530027
10.1016/S0024-4937(99)00052-3
10.24930/1681-9004-2018-18-5-692-705
10.1134/S1819714013030044
10.1016/j.gca.2012.08.032
10.1134/S0016852110010024
10.1016/j.chemgeo.2007.07.026
10.5800/GT-2021-12-2-0525
10.1016/S0009-2541(01)00355-2
10.1038/207343a0
10.1016/S0012-821X(01)00379-X
10.1130/0091-7613(2000)028<0627:REECOZ>2.3.CO;2
10.1134/S1028334X09090074
10.2138/am-2003-1013
10.1016/S0098-3004(98)00143-5
10.1134/S1028334X06020309
10.1007/s00410-018-1529-3
10.1130/G23603A.1
10.30911/0207-4028-2021-40-1-3-24
10.1016/j.gca.2004.07.006
10.1093/petrology/egq070
10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2
10.1007/s00410-007-0201-0
10.1016/j.lithos.2006.12.007
10.1130/0091-7613(2002)030<0039:ROTCMI>2.0.CO;2
10.1130/0091-7613(2001)029<0127:RCSWFA>2.0.CO;2
10.1016/j.chemgeo.2008.10.035
10.1134/S1028334X10060036
10.21440/2307-2091-2020-2-48-63
10.1016/S0024-4937(98)00024-3
10.1134/S1028334X08090122
10.1016/S0301-9268(01)00191-7
10.1134/S1028334X19080026
10.1130/B26166.1
10.1016/j.lithos.2018.06.029
10.1093/petrology/42.11.2033
10.1007/s00024-010-0204-z
10.2113/0530089
10.1093/petrology/42.6.1067
10.5800/GT-2021-12-2-0522
10.1007/BF00371047
10.1016/j.lithos.2012.10.017
10.1016/S0024-4937(02)00082-8
10.1134/S0016702911040033
10.1144/GSL.SP.1989.042.01.19
10.1134/S0016702915090025
10.1007/s00410-006-0068-5
ContentType Journal Article
DBID AAYXX
CITATION
DOI 10.24930/1681-9004-2022-22-1-55-74
DatabaseName CrossRef
DatabaseTitle CrossRef
DatabaseTitleList CrossRef
DeliveryMethod fulltext_linktorsrc
Discipline Geology
EISSN 2500-302X
EndPage 74
ExternalDocumentID 10_24930_1681_9004_2022_22_1_55_74
GroupedDBID 642
AAYXX
ADBBV
ALMA_UNASSIGNED_HOLDINGS
BCNDV
CITATION
GROUPED_DOAJ
ID FETCH-LOGICAL-c2304-4dff188adba4566bc830d20ae66b47ff7e13490ca3a573e6269c0765d5a0797d3
ISSN 1681-9004
IngestDate Tue Jul 01 01:12:05 EDT 2025
Thu Apr 24 23:08:52 EDT 2025
IsDoiOpenAccess false
IsOpenAccess true
IsPeerReviewed true
IsScholarly true
Issue 1
Language English
Russian
License https://www.lithosphere.ru/jour/about/editorialPolicies#openAccessPolicy
LinkModel OpenURL
MergedId FETCHMERGED-LOGICAL-c2304-4dff188adba4566bc830d20ae66b47ff7e13490ca3a573e6269c0765d5a0797d3
OpenAccessLink https://www.lithosphere.ru/jour/article/download/1538/1326
PageCount 20
ParticipantIDs crossref_primary_10_24930_1681_9004_2022_22_1_55_74
crossref_citationtrail_10_24930_1681_9004_2022_22_1_55_74
ProviderPackageCode CITATION
AAYXX
PublicationCentury 2000
PublicationDate 2022-03-02
PublicationDateYYYYMMDD 2022-03-02
PublicationDate_xml – month: 03
  year: 2022
  text: 2022-03-02
  day: 02
PublicationDecade 2020
PublicationTitle Litosfera (Ekaterinburg. Online)
PublicationYear 2022
References ref13
ref57
ref12
ref56
ref15
ref59
ref14
ref58
ref53
ref52
ref11
ref55
ref10
ref54
ref17
ref16
ref19
ref18
ref51
ref50
ref46
ref45
ref48
ref47
ref42
ref41
ref44
ref43
ref49
ref8
ref7
ref9
ref4
ref3
ref6
ref5
ref40
ref35
ref34
ref37
ref36
ref31
ref30
ref74
ref33
ref32
ref2
ref1
ref39
ref38
ref71
ref70
ref73
ref72
ref24
ref68
ref23
ref67
ref26
ref25
ref69
ref20
ref64
ref63
ref22
ref66
ref21
ref65
ref28
ref27
ref29
ref60
ref62
ref61
References_xml – ident: ref44
  doi: 10.1016/j.lithos.2007.06.016
– ident: ref37
  doi: 10.2138/am.2010.3521
– ident: ref26
  doi: 10.2113/0530027
– ident: ref2
  doi: 10.1016/S0024-4937(99)00052-3
– ident: ref47
  doi: 10.24930/1681-9004-2018-18-5-692-705
– ident: ref8
  doi: 10.1134/S1819714013030044
– ident: ref27
– ident: ref65
  doi: 10.1016/j.gca.2012.08.032
– ident: ref29
  doi: 10.1134/S0016852110010024
– ident: ref45
  doi: 10.1016/j.chemgeo.2007.07.026
– ident: ref67
  doi: 10.5800/GT-2021-12-2-0525
– ident: ref34
– ident: ref50
  doi: 10.1016/S0009-2541(01)00355-2
– ident: ref72
  doi: 10.1038/207343a0
– ident: ref30
– ident: ref36
– ident: ref12
  doi: 10.1016/S0012-821X(01)00379-X
– ident: ref25
  doi: 10.1130/0091-7613(2000)028<0627:REECOZ>2.3.CO;2
– ident: ref32
  doi: 10.1134/S1028334X09090074
– ident: ref18
  doi: 10.2138/am-2003-1013
– ident: ref40
– ident: ref23
– ident: ref64
  doi: 10.1016/S0098-3004(98)00143-5
– ident: ref66
  doi: 10.1134/S1028334X06020309
– ident: ref39
  doi: 10.1007/s00410-018-1529-3
– ident: ref21
  doi: 10.1130/G23603A.1
– ident: ref54
– ident: ref71
– ident: ref9
  doi: 10.30911/0207-4028-2021-40-1-3-24
– ident: ref3
– ident: ref58
– ident: ref7
– ident: ref24
  doi: 10.1016/j.gca.2004.07.006
– ident: ref16
  doi: 10.1093/petrology/egq070
– ident: ref41
– ident: ref60
– ident: ref74
– ident: ref51
– ident: ref48
– ident: ref13
  doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2
– ident: ref14
  doi: 10.1007/s00410-007-0201-0
– ident: ref5
  doi: 10.1016/j.lithos.2006.12.007
– ident: ref43
  doi: 10.1130/0091-7613(2002)030<0039:ROTCMI>2.0.CO;2
– ident: ref1
  doi: 10.1130/0091-7613(2001)029<0127:RCSWFA>2.0.CO;2
– ident: ref17
  doi: 10.1016/j.chemgeo.2008.10.035
– ident: ref55
– ident: ref52
  doi: 10.1134/S1028334X10060036
– ident: ref57
  doi: 10.21440/2307-2091-2020-2-48-63
– ident: ref61
  doi: 10.1016/S0024-4937(98)00024-3
– ident: ref35
  doi: 10.1134/S1028334X08090122
– ident: ref53
  doi: 10.1016/S0301-9268(01)00191-7
– ident: ref38
– ident: ref63
– ident: ref6
  doi: 10.1134/S1028334X19080026
– ident: ref11
  doi: 10.1130/B26166.1
– ident: ref59
– ident: ref73
  doi: 10.1016/j.lithos.2018.06.029
– ident: ref15
  doi: 10.1093/petrology/42.11.2033
– ident: ref46
– ident: ref28
– ident: ref42
– ident: ref10
  doi: 10.1007/s00024-010-0204-z
– ident: ref22
  doi: 10.2113/0530089
– ident: ref49
– ident: ref19
  doi: 10.1093/petrology/42.6.1067
– ident: ref31
  doi: 10.5800/GT-2021-12-2-0522
– ident: ref69
  doi: 10.1007/BF00371047
– ident: ref68
  doi: 10.1016/j.lithos.2012.10.017
– ident: ref20
  doi: 10.1016/S0024-4937(02)00082-8
– ident: ref56
– ident: ref4
  doi: 10.1134/S0016702911040033
– ident: ref62
  doi: 10.1144/GSL.SP.1989.042.01.19
– ident: ref33
  doi: 10.1134/S0016702915090025
– ident: ref70
  doi: 10.1007/s00410-006-0068-5
SSID ssj0002876007
ssib046627809
ssib044751621
Score 2.1754992
Snippet Research subject . Composition and isotopic parameters of zircons and their host granites of the Bitim complex, localised in the eastern part of the Ufaley...
SourceID crossref
SourceType Enrichment Source
Index Database
StartPage 55
Title New data on the trace element composition and Lu-Hf isotopic system of zircons from the Early Cambrian granites of the Ufaley block (Middle Urals): a step to the correction of geodynamic concepts
Volume 22
hasFullText 1
inHoldings 1
isFullTextHit
isPrint
link http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV1bi9NAFB7qiuCLeMX1xnlQUMrU3C--idRdZOvTFtanMJlMlm6lKb0Iuw_-OX-Cf8hzzmTSsCquCyWENHOSdr7MfDP55jtCvMxCzyC117JKqlhGxiSy1HUm6zILdJSXcc6Z5yafk8Np9OkkPhkMfvZUS9tNOdIXf1xXcp1axWNYr7RK9j9qtguKB3Af6xe3WMO4vVIdkziRJJ7tjD_le8DH1FhFOKvFW0kWvyI42srDejhbN5tmOdOthzORxYvZSpNipltq0roe83IufP5PV-SRYd1pmafWRC5J867nxFAnPMkxnK7wB78Kcrt-GoMvHbHVlAJEO256aprqfKFIlK_tosl1nyIfYRuzrs1KUejxXJGZNPszjIZ9X9TWWBIBrubNN6bAB6Phl21_GgNHwKTj6s1s-klGWhGbi3hk-BjSM-wkPM633jXXQfAbLG3ba-1-217cpv653D_gWDMkRWV3Mcm3gh9fxrFMo12v6JQAlzrLTsKIgyeOVlCsgmIVFKvAj1_EcZFGN8TNAMcu1FtMvo9dI0cGi36y40wROfA7D7Uznu2kd6WcFMjdpTXL5cu9_eut94hVjyEd3xV32qENvLc4vScGZnFf3Drg1NHnD8QPRCsQWqFZAKICGK3QohV6aAVEKzBawaEVLFqhqaFFKxBaOQ6jFRxawaGVzqWvLVqB0QqvLVaBsfrmHSggnMKm4VN3OKXCO5yCw-lDMf04Pv5wKNsUIlLT2w4ZVXXtZ5mqSoUjhaTU2DZVgacM7kdpXaeG7Dk9rUIVp6HB0X2uvTSJq1h5aZ5W4SOxt2gW5rGAUGtk6ynlc0ujDAPmYV4rPzJlpXyVRfsid_9_oVt_fUrz8rX4N1T2RdiVXVqXmSuUenKtUk_F7d3z90zsbVZb8xyJ9aZ8wUD9BY2IxIg
linkProvider ISSN International Centre
openUrl ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=New+data+on+the+trace+element+composition+and+Lu-Hf+isotopic+system+of+zircons+from+the+Early+Cambrian+granites+of+the+Ufaley+block+%28Middle+Urals%29%3A+a+step+to+the+correction+of+geodynamic+concepts&rft.jtitle=Litosfera+%28Ekaterinburg.+Online%29&rft.au=Shardakova%2C+G.+Yu&rft.date=2022-03-02&rft.issn=1681-9004&rft.eissn=2500-302X&rft.volume=22&rft.issue=1&rft.spage=55&rft.epage=74&rft_id=info:doi/10.24930%2F1681-9004-2022-22-1-55-74&rft.externalDBID=n%2Fa&rft.externalDocID=10_24930_1681_9004_2022_22_1_55_74
thumbnail_l http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=1681-9004&client=summon
thumbnail_m http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=1681-9004&client=summon
thumbnail_s http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=1681-9004&client=summon