Late Cambrian-Ordovician northeastern Gondwanan terranes in the basement of the Apuseni Mountains, Romania
Balintoni, I.1; Balica, C.1; Ducea, M. N.2; Zaharia, L.1; Chen, Fukun3; Cliveti, M.1; Hann, H. P.4; Li, Li-Qiu3; Ghergari, L.1
刊名JOURNAL OF THE GEOLOGICAL SOCIETY
2010-12-01
卷号167期号:6页码:1131-1145
ISSN号0016-7649
DOI10.1144/0016-76492009-156
文献子类Article
英文摘要The pre-Alpine basement of the Apuseni Mountains (Romanian Carpathians) comprises three terranes: Somes, Baia de Aries and Biharia. Metaigneous rocks within these terranes record Late Cambrian-Ordovician U-Pb zircon crystallization ages. Two samples from an orthogneiss layer in the Somes, terrane yielded an age of 459.8 +/- 2.7 Ma. In the Baia de Aries, terrane, an augen gneiss yielded an age of 470.8 +/- 3.8 Ma, a porphyroid yielded an age of 467.8 +/- 3.8 Ma and two metagranites yielded ages of 467.8 +/- 4.7 Ma and 467.1 +/- 3.9 Ma, respectively. Three samples from a metagranitoid outcrop located in the lower part of the Biharia terrane yielded an age of 495.0 +/- 2.1 Ma. Three other samples from a metabasite layer situated lithostratigraphically several hundred metres above the metagranitoid yielded an age of 477.8 +/- 3.2 Ma. Detrital U/Pb zircon ages from a paragneiss interlayered within the Baia de Aries, terrane scatter between 548 and 3518 Ma. Detrital zircon ages together with the inherited ages recorded by magmatic zircon populations suggest a northeastern Gondwanan provenance for the Somes,, Baia de Aries, and Biharia terranes, adjacent to the Arabian-Nubian Shield. Lead loss in some zircons is interpreted to have taken place during the Variscan orogeny.
WOS关键词U-PB AGES ; AVALONIAN-CADOMIAN BELT ; SAXO-THURINGIAN ZONE ; AUSTROALPINE BASEMENT ; BOHEMIAN MASSIF ; TAUERN WINDOW ; EASTERN ALPS ; EVOLUTION ; VARISCAN ; ZIRCON
WOS研究方向Geology
语种英语
出版者GEOLOGICAL SOC PUBL HOUSE
WOS记录号WOS:000283124300005
资助机构(ID-480 CNCSIS) ; (ID-480 CNCSIS) ; (1/226 2005 CNCSIS) ; (1/226 2005 CNCSIS) ; (37-01/2004-2006 MEC) ; (37-01/2004-2006 MEC) ; (ID-480 CNCSIS) ; (ID-480 CNCSIS) ; (1/226 2005 CNCSIS) ; (1/226 2005 CNCSIS) ; (37-01/2004-2006 MEC) ; (37-01/2004-2006 MEC) ; (ID-480 CNCSIS) ; (ID-480 CNCSIS) ; (1/226 2005 CNCSIS) ; (1/226 2005 CNCSIS) ; (37-01/2004-2006 MEC) ; (37-01/2004-2006 MEC) ; (ID-480 CNCSIS) ; (ID-480 CNCSIS) ; (1/226 2005 CNCSIS) ; (1/226 2005 CNCSIS) ; (37-01/2004-2006 MEC) ; (37-01/2004-2006 MEC)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/72244]  
专题中国科学院地质与地球物理研究所
通讯作者Balintoni, I.
作者单位1.Univ Babes Bolyai, Dept Geol, Fac Biol & Geol, RO-400084 Cluj Napoca, Romania
2.Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
4.Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany
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Balintoni, I.,Balica, C.,Ducea, M. N.,et al. Late Cambrian-Ordovician northeastern Gondwanan terranes in the basement of the Apuseni Mountains, Romania[J]. JOURNAL OF THE GEOLOGICAL SOCIETY,2010,167(6):1131-1145.
APA Balintoni, I..,Balica, C..,Ducea, M. N..,Zaharia, L..,Chen, Fukun.,...&Ghergari, L..(2010).Late Cambrian-Ordovician northeastern Gondwanan terranes in the basement of the Apuseni Mountains, Romania.JOURNAL OF THE GEOLOGICAL SOCIETY,167(6),1131-1145.
MLA Balintoni, I.,et al."Late Cambrian-Ordovician northeastern Gondwanan terranes in the basement of the Apuseni Mountains, Romania".JOURNAL OF THE GEOLOGICAL SOCIETY 167.6(2010):1131-1145.
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