The discovery of the oldest rocks in the Kuluketage area and its geological implications
文献类型:期刊论文
作者 | Long XiaoPing1; Yuan Chao1; Sun Min2; Xiao WenJiao3; Zhao GuoChun2; Zhou KeFa4; Wang YuJing1; Hu AiQin1 |
刊名 | SCIENCE CHINA-EARTH SCIENCES
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出版日期 | 2011-03-01 |
卷号 | 54期号:3页码:342-348 |
关键词 | Tarim Craton Archean crustal growth zircon dating Hf isotope |
ISSN号 | 1674-7313 |
DOI | 10.1007/s11430-010-4156-z |
文献子类 | Article |
英文摘要 | The basement rocks in the Kuluketage area are composed predominately of tonalite-trondhjemite-granodiorite rocks, and occured mainly in Xinger and Korla. U-Pb dating of TTG gneiss near Korla yielded a late Neoarchean weighted mean (207)Pb/(206)Pb age of 2.65 Ga, which is the oldest published age for the TTG rocks in the Kuluketage area and thus suggests that Archean terrane in the area was formed in the late Neoarchean. The Korla gneiss is much younger than the TTG rocks in the northern Altyn Tagh, eastern Tarim Craton, indicating that the oldest terrane of the Tarim Craton was exposed probably in the northern Altyn Tagh. Until late Neoarchean, the Tarim continent extends to the Kuluketage area and finally had generated a relatively large uniform Archean basement within the craton. Zircon Hf isotopic analyses of the TTG gneiss give low E >(Hf)(t) values (-5 to 1) with Paleoarchean to Mesoarchean two-stage model ages (T (DM) (2)) between 3.0 and 3.3 Ga, suggesting that the basement rocks in the northern Tarim Craton were derived dominately from partial melting of Paleoarchean to Mesoarchean juvenile crustal material. The Hf model ages, therefore, indicate that no continent crust older than 3.3 Ga existed in the Kuluketage area. |
WOS关键词 | HF ISOTOPE COMPOSITION ; U-PB AGE ; CRUSTAL EVOLUTION ; CONTINENTAL-CRUST ; TARIM BLOCK ; SOUTH CHINA ; LU-HF ; GEOCHRONOLOGICAL EVIDENCE ; LIAONING PROVINCE ; YANGTZE CRATON |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000288121700002 |
出版者 | SCIENCE CHINA PRESS |
资助机构 | National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; National Natural Science Foundation of China(40803009 ; National Natural Science Foundation of China(40803009 ; CAS/SAFEA ; CAS/SAFEA ; 40772130) ; 40772130) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; National Natural Science Foundation of China(40803009 ; National Natural Science Foundation of China(40803009 ; CAS/SAFEA ; CAS/SAFEA ; 40772130) ; 40772130) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; National Natural Science Foundation of China(40803009 ; National Natural Science Foundation of China(40803009 ; CAS/SAFEA ; CAS/SAFEA ; 40772130) ; 40772130) ; National Basic Research Program of China(2007CB411308) ; National Basic Research Program of China(2007CB411308) ; National Natural Science Foundation of China(40803009 ; National Natural Science Foundation of China(40803009 ; CAS/SAFEA ; CAS/SAFEA ; 40772130) ; 40772130) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/74652] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Long XiaoPing |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochem, Guangzhou 510640, Guangdong, Peoples R China 2.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Xinjiang Resources & Environm Ctr, Urumqi 830000, Peoples R China |
推荐引用方式 GB/T 7714 | Long XiaoPing,Yuan Chao,Sun Min,et al. The discovery of the oldest rocks in the Kuluketage area and its geological implications[J]. SCIENCE CHINA-EARTH SCIENCES,2011,54(3):342-348. |
APA | Long XiaoPing.,Yuan Chao.,Sun Min.,Xiao WenJiao.,Zhao GuoChun.,...&Hu AiQin.(2011).The discovery of the oldest rocks in the Kuluketage area and its geological implications.SCIENCE CHINA-EARTH SCIENCES,54(3),342-348. |
MLA | Long XiaoPing,et al."The discovery of the oldest rocks in the Kuluketage area and its geological implications".SCIENCE CHINA-EARTH SCIENCES 54.3(2011):342-348. |
入库方式: OAI收割
来源:地质与地球物理研究所
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