globalchange  > 气候变化与战略
DOI: 10.1016/j.earscirev.2019.102899
论文题名:
Sources of bias in detrital zircon geochronology: Discordance, concealed lead loss and common lead correction
作者: Andersen T.; Elburg M.A.; Magwaza B.N.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2019
卷: 197
语种: 英语
中文关键词: Common lead ; Detrital zircon ; Lead loss ; Lu-Hf ; Provenance ; U-Pb
英文关键词: detrital deposit ; geochronology ; hafnium ; isotopic composition ; lead ; lutetium ; provenance ; uranium-lead dating ; zircon
英文摘要: The distribution pattern of U-Pb ages of detrital zircon in a sedimentary rock is commonly assumed to reflect the ages of igneous or metamorphic processes in rocks that have contributed material to the sedimentary basin (i.e. the protosources), directly or through recycling of older sedimentary rocks. If the Pb isotopic composition of detrital zircon is modified by processes after crystallization, or influenced by unintended effects of data treatment such as discordance filters and common lead correction, the value of detrital zircon as geological indicator is compromised. Discordance filters will identify zircons having suffered recent lead loss, but significant amounts of ancient lead loss may pass undetected. Lead loss events after the zircon's primary crystallization can be induced by regional or contact metamorphism, but also by low temperature processes during diagenesis and weathering, and can be coupled to uptake of a mixture of common lead and unsupported radiogenic lead, which cannot be properly corrected by common‑lead correction routines. Concealed ancient lead loss and overcorrection for common 207Pb may cause bias towards lower ages, while remaining within acceptable discordance limits. This creates spurious age fractions that may give false indications of sedimentary provenance, invalidate estimates of maximum limits for the age of deposition, and cause problems for comparison and correlation studies based on detrital zircon age data. Careful scrutiny of all U-Pb analyses in combination with Hf isotope analysis may help identifying these effects in detrital zircon data, but will not provide a universal guarantee against biased age spectra. © 2019 The Authors
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165760
Appears in Collections:气候变化与战略

Files in This Item:

There are no files associated with this item.


作者单位: Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern, Oslo, N-0316, Norway; Department of Geology, University of Johannesburg, PO Box 524, Auckland Park, Johannesburg, 2006, South Africa

Recommended Citation:
Andersen T.,Elburg M.A.,Magwaza B.N.. Sources of bias in detrital zircon geochronology: Discordance, concealed lead loss and common lead correction[J]. Earth Science Reviews,2019-01-01,197
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Andersen T.]'s Articles
[Elburg M.A.]'s Articles
[Magwaza B.N.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Andersen T.]'s Articles
[Elburg M.A.]'s Articles
[Magwaza B.N.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Andersen T.]‘s Articles
[Elburg M.A.]‘s Articles
[Magwaza B.N.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

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