IGGCAS OpenIR
Provenance of the Paleoproterozoic Hutuo Group basal conglomerates and Neoarchean crustal growth in the Wutai Mountains, North China Craton: Evidence from granite and quartzite pebble zircon U-Pb ages and Hf isotopes
Du LiLin1; Yang ChongHui1; Wang Wei2; Ren LiuDong1; Wan YuSheng1,3; Song HuiXia1; Gao LinZhi1; Geng YuanSheng1; Hou KeJun4
2012-11-01
Source PublicationSCIENCE CHINA-EARTH SCIENCES
ISSN1674-7313
Volume55Issue:11Pages:1796-1814
SubtypeArticle
AbstractZircon U-Pb ages (SHRIMP and LA-ICPMS) and Lu-Hf isotope data (LA-ICPMS) are presented for two granite and two quartzite pebbles from the basal conglomerates of the Sijizhuang Formation in the Hutuo Group from the Wutai Mountains area in the North China Craton. These two granite pebbles give zircon Pb-207/Pb-206 ages of 2513 +/- 8 Ma and 2527 +/- 8 Ma respectively, which are consistent with the emplacement ages of the Wangjiahui grey granite and Guangmingsi or Shifo granite in the Wutai Mountains. Detrital zircons from those two quartzite pebbles are mostly 2550-2490 Ma old with lesser number of 2800-2550 Ma grains, which is similar to the ages of detrital zircons from quartzites in the Gaofan Subgroup of the Neoarchean Wutai Group. Thus, the pebbles in the Hutuo Group basal conglomerates were derived locally from Wutai Mountains Neoarchean sources. Zircons from the Sijizhuang Formation conglomerate granite and quartzite pebbles mostly have positive E > (Hf)(t) values, a minority with E > (Hf)(t) values like model depleted mantle (DM) of the same age, but with most showing DM model ages 200-100 Ma. This indicates that most of the source materials were derived from the mantle within the previous 200 million years, whereas some are derived from 2550-2510 Ma juvenile crustal additions. This additional evidence suggests that in the North China Craton there was important initial polycyclic crustal formation and cratonization in the late Neoarchaean, prior to superimposed Palaeoproterozoic orogenic cycles.
KeywordHutuo Group Sijizhuang Formation conglomerate zircon U-Pb age Hf isotope sedimentary provenance crustal growth
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1007/s11430-012-4407-2
Funding OrganizationChina Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152)
WOS KeywordPLASMA-MASS SPECTROMETRY ; HIGH-PRESSURE GRANULITES ; TECTONIC EVOLUTION ; CENTRAL ZONE ; METAMORPHIC EVOLUTION ; DETRITAL ZIRCONS ; GREENSTONE-BELT ; BASEMENT ROCKS ; FUPING COMPLEX ; SANGGAN AREA
Indexed BySCI
Language英语
Funding OrganizationChina Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152) ; China Geological Survey(1212010611802 ; China Geological Survey(1212010611802 ; National Natural Science Foundation of China(41172171) ; National Natural Science Foundation of China(41172171) ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China(J0721 ; National Commission on Stratigraphy of China(1212010511702-01 ; National Commission on Stratigraphy of China(1212010511702-01 ; 1212010711815 ; 1212010711815 ; J0907) ; J0907) ; 1212011120142) ; 1212011120142) ; 1212011120152) ; 1212011120152)
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000310326600004
PublisherSCIENCE PRESS
Citation statistics
Cited Times:8[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/84693
Collection中国科学院地质与地球物理研究所
Corresponding AuthorDu LiLin
Affiliation1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Beijing SHRIMP Ctr, Beijing 100037, Peoples R China
4.Chinese Acad Geol Sci, Inst Mineral Resources, Beijing 100037, Peoples R China
Recommended Citation
GB/T 7714
Du LiLin,Yang ChongHui,Wang Wei,et al. Provenance of the Paleoproterozoic Hutuo Group basal conglomerates and Neoarchean crustal growth in the Wutai Mountains, North China Craton: Evidence from granite and quartzite pebble zircon U-Pb ages and Hf isotopes[J]. SCIENCE CHINA-EARTH SCIENCES,2012,55(11):1796-1814.
APA Du LiLin.,Yang ChongHui.,Wang Wei.,Ren LiuDong.,Wan YuSheng.,...&Hou KeJun.(2012).Provenance of the Paleoproterozoic Hutuo Group basal conglomerates and Neoarchean crustal growth in the Wutai Mountains, North China Craton: Evidence from granite and quartzite pebble zircon U-Pb ages and Hf isotopes.SCIENCE CHINA-EARTH SCIENCES,55(11),1796-1814.
MLA Du LiLin,et al."Provenance of the Paleoproterozoic Hutuo Group basal conglomerates and Neoarchean crustal growth in the Wutai Mountains, North China Craton: Evidence from granite and quartzite pebble zircon U-Pb ages and Hf isotopes".SCIENCE CHINA-EARTH SCIENCES 55.11(2012):1796-1814.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Du LiLin]'s Articles
[Yang ChongHui]'s Articles
[Wang Wei]'s Articles
Baidu academic
Similar articles in Baidu academic
[Du LiLin]'s Articles
[Yang ChongHui]'s Articles
[Wang Wei]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Du LiLin]'s Articles
[Yang ChongHui]'s Articles
[Wang Wei]'s Articles
Terms of Use
No data!
Social Bookmark/Share
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit Add to Technorati
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.