Geochemistry and Detrial Zircon Geochronology of Carboniferous Detrital Rocks in the Northern Margin of Dabie Mountains, Central China and Constraints to Distinguishing the Provenance Tectonic Attribute

详细信息   

• 责任者：Yang DongDong(College of Resources and Environment ; Hefei University of Technology ; Hefei 230009 ; China) ; Li ShuangYing
• 刊名：Acta Petrologica Sinica
• 出版年：2012
• 卷期：28(8)
• 关键词：碎屑岩 ; clastic rocks ; 大别山 ; Dabie Mountains
• 页码：p.2619-2628
• 图表：illus.,5 tables,33 refs.
• 分类号：0803
• issnNo：ISSN1000-0569
• isbnNo：CN11-1922/P

摘要

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line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">25.33×10^-6line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">, respectively; and the ratios of Rb/Sr, Th/U, La/Y, La/Sc and Th/Sc are respectively 1.49, 4.10,

    

line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">14.75, 31.92 and 0.89; the average of ΣREE is 146.2×10^-6line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px"> (54.11×10^-6line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">～256.0×10^-6line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">), δline !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">Eu is 0.64, light REE

    

line !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">enrichment. La/Yb is 12.58(3.94～15.42), and (La/Yb)_Nline !important; FONT: 12px/15px ����,verdana; WHITE-SPACE: normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(0,0,0); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px"> is 9.02. The dating of detrital zircons shows that the

    

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