Geochronology and geochemistry of the fossil-flora-bearing Wuda Tuff in North China Craton and its tectonic implications | |
Wang, Man1,4; Zhong, Yu-ting1; He, Bin1; Denyszyn, Steven W.2; Wang, Jun (王军)3,4; Xu, Yi-gang1,4,5 | |
刊名 | LITHOS |
2020-07-01 | |
卷号 | 364页码:10 |
关键词 | Wuda vegetational Pompeii Altered tuff North China Craton Zircon U-Pb geochronology Geochemistry Alxa Terrane |
ISSN号 | 0024-4937 |
DOI | 10.1016/j.lithos.2020.105485 |
英文摘要 | The Wuda Tuff Flora in the North China Craton (NCC) is a "vegetational Pompeii" and one of the most completely preserved marsh ecosystems of the late Paleozoic Northern Hemisphere. However, the precise age, geochemistry, and petrogenesis of the thick tuff containing this peat-forming flora have not been established. We conducted a comprehensive petrographic, mineralogical, whole-rock geochemical, and zircon U-Pb and Hf-O isotopic investigation of five samples from a vertical section through the tuff bed. Our results confirm that the material that buried the flora is a volcanic tuff bed that has undergone intensive post-deposition alteration. Whole-rock Al2O3/TiO2 ratios (65.8-103.5) and negative Eu/Eu* values (0.27-038) further suggest a felsic volcanic origin. Secondary ion mass spectrometry zircon U-Pb dating of the altered tuff bed yielded a weighted mean Pb-206/U-238 age of 295.9 +/- 1.4 Ma (1 sigma MSWD = 0.94, n = 39), constraining the age of the Wuda Tuff Flora to the earliest Permian. Depletions of Nb and Ta in both the whole-rock and zircon compositions indicate an arc-related setting for the volcanism.The positive epsilon Hf(t) values (0.0 to +5.0) and delta O-18 values (5.05 parts per thousand-6.17 parts per thousand) of zircon grains from the Wuda Tuff suggest a juvenile crust origin of the volcanic magma. Geochemical comparisons with contemporaneous igneous rocks suggest that the volcanic eruption that led to the formation of the Wuda Tuff and associated vegetational Pompeii was most probably caused by arc volcanism along the western margin of the NCC related to subduction of Paleo-Asian Ocean oceanic crust, implying that the Alm Terrane had not yet amalgamated with the NCC during the early Permian. (C) 2020 Published by Elsevier B.V. |
资助项目 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18000000] ; National Natural Science Foundation of China[41573028] |
WOS关键词 | PERMIAN VEGETATIONAL POMPEII ; HF ISOTOPE ANALYSES ; U-PB GEOCHRONOLOGY ; INNER-MONGOLIA ; ZIRCON MEGACRYSTS ; WORKING REFERENCE ; THRUST BELT ; ALXA BLOCK ; O ISOTOPES ; COAL |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
出版者 | ELSEVIER |
WOS记录号 | WOS:000536183500002 |
资助机构 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China |
内容类型 | 期刊论文 |
源URL | [http://ir.nigpas.ac.cn/handle/332004/31921] |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | He, Bin |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 2.Univ Western Australia, Sch Earth Sci, Perth, WA 6009, Australia 3.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 5.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Man,Zhong, Yu-ting,He, Bin,et al. Geochronology and geochemistry of the fossil-flora-bearing Wuda Tuff in North China Craton and its tectonic implications[J]. LITHOS,2020,364:10. |
APA | Wang, Man,Zhong, Yu-ting,He, Bin,Denyszyn, Steven W.,Wang, Jun ,&Xu, Yi-gang.(2020).Geochronology and geochemistry of the fossil-flora-bearing Wuda Tuff in North China Craton and its tectonic implications.LITHOS,364,10. |
MLA | Wang, Man,et al."Geochronology and geochemistry of the fossil-flora-bearing Wuda Tuff in North China Craton and its tectonic implications".LITHOS 364(2020):10. |
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