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SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China Tectonic implications and the need to redefine lithostratigraphic units
Wan, YS (Wan, Yusheng); Liu, DY (Liu, Dunyi); Xu, MH (Xu, Meihui); Zhuang, JM (Zhuang, Jianmin); Song, B (Song, Biao); Shi, YR (Shi, Yuruo); Du, LL (Du, Lilin)
刊名GONDWANA RESEARCH
2007
卷号12期号:1-2页码:166-183
关键词Proterozoic early Palaeozoic Cathaysia Block SHRIMP Nd-isotopes Rodinia South China
ISSN号1342-937X
英文摘要Northwestern Fujian Province is one of the most important Pre-Palaeozoic areas in the Cathaysia Block of South China. Metavolcano-sedimentary and metasedimentary rocks of different types, ages and metamorphic grades (granulite to upper greenschist facies) are present, and previously were divided into several Formations and Groups. Tectonic contacts occur between some units, whereas (deformed) unconformities have been reported between others. New SHRIMP U-Pb zircon ages presented here indicate that the original lithostratigraphy and the old "Group" and "Formation" terminology should be abandoned. Thus the "Tianjingping Formation" was not formed in the Archaean or Palaeoproterozoic, as previously considered, but must be younger than its youngest detrital zircons (1790 Ma) but older than regional metamorphism (460 Ma). Besides magmatic zircon ages of 807 Ma obtained from metavolcano-sedimentary rocks of the "Nanshan Formation" and 751-728 Ma for the "Mamianshan Group", many inherited and detrital zircons with ages ranging from 1.0 to 0.8 Ga were also found in them. These ages indicate that the geological evolution of the study area may be related to the assembly and subsequent break-up of the Rodinia supercontinent. The new zircon results poorly constrain the age of the "Mayuan Group" as Neoproterozoic to early Palaeozoic (728-458 Ma), and not Palaeoproterozoic as previously thought. Many older inherited and detrital zircons with ages of 3.6, 2.8, 2.7, 2.6-2.5, 2.0-1.8 and 1.6 Ga were found in this study. A 3.6 Ga detrital grain is the oldest one so far identified in northwestern Fujian Province as well as throughout the Cathaysia Block. Nd isotope t(DM) values of eight volcano-sedimentary and clastic sedimentary rock samples centre on 2.73-1.68 Ga, being much older than the formation ages of their protoliths and thus showing that the recycling of older crust played an important role in their formation. These rocks underwent high grade metamorphism in the early Palaeozoic (458-425 Ma) during an important tectono-thermal event in the Cathaysia Block. (c) 2006 Published by Elsevier B.V. on behalf of International Association for Gondwana Research.
学科主题地质年代学
WOS关键词SOUTH CHINA ; SM-ND ; MESOPROTEROZOIC SUPERCONTINENT ; SOUTHEASTERN CHINA ; SINGLE ZIRCON ; EVOLUTION ; RODINIA ; MAGMATISM ; MANTLE ; CONFIGURATION
WOS研究方向Geology
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000248283100013
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/38484]  
专题中国地质调查局
作者单位Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China Chinese Acad Geol Sci, Beijing SHRIMP Ctr, Beijing 100037, Peoples R China Fujian Inst Geol Survey, Fujian 365001, Peoples R China
推荐引用方式
GB/T 7714
Wan, YS ,Liu, DY ,Xu, MH ,et al. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China Tectonic implications and the need to redefine lithostratigraphic units[J]. GONDWANA RESEARCH,2007,12(1-2):166-183.
APA Wan, YS .,Liu, DY .,Xu, MH .,Zhuang, JM .,Song, B .,...&Du, LL .(2007).SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China Tectonic implications and the need to redefine lithostratigraphic units.GONDWANA RESEARCH,12(1-2),166-183.
MLA Wan, YS ,et al."SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China Tectonic implications and the need to redefine lithostratigraphic units".GONDWANA RESEARCH 12.1-2(2007):166-183.
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