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华夏地块龙泉地区发现亚洲最古老的锆石

邢光福 杨祝良 陈志洪 姜杨 洪文涛 靳国栋 余明刚 赵希林 段政

地球学报Issue(4):395-402,8.
地球学报Issue(4):395-402,8.DOI:10.3975/cagsb.2015.04.02

华夏地块龙泉地区发现亚洲最古老的锆石

The Discovery of the Asian Oldest Zircons in Longquan, Cathaysia Block

邢光福 1杨祝良 1陈志洪 1姜杨 1洪文涛 1靳国栋 1余明刚 1赵希林 1段政1

作者信息

  • 1. 中国地质调查局南京地质调查中心,江苏南京 210016
  • 折叠

摘要

Abstract

At present, zircons are the only residual material of the Hadean crust, and constitute a crucial clue to understanding the early crustal evolution. Rencently, we found the two ~4100 Ma detrital zircons from a Paleozoic quartzite in the Longquan area of the Cathaysia Block, through SHRIMP zircon data. One zircon (207Pb/206Pb age of 4127±4 Ma) shows normal oscillatory zonation and constant mantle-like oxygen isotope ratios (δ18O = 5.8‰ to 6.0‰), and might have crystallized in ancient mantle-derived magmas or partial melts of primitive crust. Obviously, this is the oldest age in the reported zircon ages of Asia. The other zircon grain has a ~4100 Ma magmatic core surrounded by a ~4070 Ma metamorphic mantle. The 4070 Ma indicates the most reliable metamorphic age of the earth. Outside the mantle, two overgrowth bands are 3800~3600 Ma, implying that the magmatic core (crust) underwent complex evolutions after ~4100Ma. These data demonstate the diversity of the Earth’s earliest crustal nature and tectonic setting, and provide crucial evidence for us to understand the earliest crustal evolution.

关键词

锆石/冥古宙/龙泉/华夏陆块

Key words

zircon/Hadean/Longquan/Cathaysia Block

分类

天文与地球科学

引用本文复制引用

邢光福,杨祝良,陈志洪,姜杨,洪文涛,靳国栋,余明刚,赵希林,段政..华夏地块龙泉地区发现亚洲最古老的锆石[J].地球学报,2015,(4):395-402,8.

基金项目

本文由中国地质调查局工作项目“华东基础地质综合调查与片区总结”(编号:1212011220542)和国家自然科学基金项目(编号:41002024 (编号:1212011220542)

41202141)联合资助。获中国地质调查局、中国地质科学院2014年度地质科技十大进展第七名。 ()

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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