Growth of the South American convergent margin (lat. 31°-36°S) during Late Paleozoic times:: A U-Pb and Hf-isotope study of detrital zircons from a fossil accretionary system

被引：0

作者：

Willner, A. P.

Gerdes, A.

Massonne, H.-J.

机构：

[1] Univ Stuttgart, Inst Mineral & Kristallog, D-70174 Stuttgart, Germany

[2] Mineral JW Goethe Univ, Inst Geowissensch, D-60438 Frankfurt, Germany

[3] Ruhr Univ Bochum, Inst Geol Mineral & Geophys, D-44780 Bochum, Germany

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 2007年 / 71卷 / 15期

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D O I：

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中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

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页码：A1119 / A1119

页数：1

共 11 条

[1] Provenance of late Palaeozoic metasediments of the SW South American Gondwana margin:: a combined U-Pb and Hf-isotope study of single detrital zircons
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[2] History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29°-36° S revealed by a U-Pb and Lu-Hf isotope study of detrital zircon from late Paleozoic accretionary systems
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[3] U-Pb ages and Hf-isotope data of detrital zircons from the late Neoarchean-Paleoproterozoic Minas Basin, SE Brazil
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[8] Activation of northern margin of the North China Craton in Late Paleozoic:Evidence from U-Pb dating and Hf isotopes of detrital zircons from the Upper Carboniferous Taiyuan Formation in the Ningwu-Jingle basin
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[9] U-Pb dating and Hf isotope study of detrital zircons from the Zhifu Group, Jiaobei Terrane, North China Craton: Provenance and implications for Precambrian crustal growth and recycling
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[10] U-Pb and Hf isotope analysis of detrital zircons from Devonian-Permian strata of Kotel'ny Island (New Siberian Islands, Russian Eastern Arctic): Insights into the Middle-Late Paleozoic evolution of the Arctic
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