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长江流域岩体锆石U-Pb年龄与Hf同位素特征及沉积物源示踪意义

王扬扬 范代读

王扬扬, 范代读. 长江流域岩体锆石U-Pb年龄与Hf同位素特征及沉积物源示踪意义[J]. 海洋地质与第四纪地质, 2013, 33(5): 97-118. doi: 10.3724/SP.J.1140.2013.05097
引用本文: 王扬扬, 范代读. 长江流域岩体锆石U-Pb年龄与Hf同位素特征及沉积物源示踪意义[J]. 海洋地质与第四纪地质, 2013, 33(5): 97-118. doi: 10.3724/SP.J.1140.2013.05097
WANG Yangyang, FAN Daidu. U-Pb AGES AND Hf ISOTOPIC COMPOSITION OF CRYSTALLINE ZIRCONS FROM IGNEOUS ROCKS OF THE CHANGJIANG DRAINAGE BASIN AND THEIR IMPLICATIONS FOR PROVENANCE[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 97-118. doi: 10.3724/SP.J.1140.2013.05097
Citation: WANG Yangyang, FAN Daidu. U-Pb AGES AND Hf ISOTOPIC COMPOSITION OF CRYSTALLINE ZIRCONS FROM IGNEOUS ROCKS OF THE CHANGJIANG DRAINAGE BASIN AND THEIR IMPLICATIONS FOR PROVENANCE[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 97-118. doi: 10.3724/SP.J.1140.2013.05097

长江流域岩体锆石U-Pb年龄与Hf同位素特征及沉积物源示踪意义


doi: 10.3724/SP.J.1140.2013.05097
详细信息
    作者简介:

    王扬扬(1987-),女,博士生,主要研究方向为沉积地球化学.

  • 基金项目:

    国家自然科学基金项目(41076016,40830107);教育部高等学校博士学科点专项科研基金(20090072110004);中国地质调查局海保工程专项(GZH201100203);海洋地质国家重点实验室课题(MG200907);中央高校基本科研业务费专项资金

  • 中图分类号: P595

U-Pb AGES AND Hf ISOTOPIC COMPOSITION OF CRYSTALLINE ZIRCONS FROM IGNEOUS ROCKS OF THE CHANGJIANG DRAINAGE BASIN AND THEIR IMPLICATIONS FOR PROVENANCE

More Information
  • 摘要: 物源精细示踪是当前单矿物颗粒微区分析技术运用的重要领域。长江流域因面积巨大、源岩构成与分布非常复杂,充分掌握流域内岩体锆石U-Pb年龄等微区分析信息成为精细物源示踪的关键。在系统搜集与分析近十年来发表的长江流域内岩体锆石U-Pb年龄和Hf同位素组成的数据资料,结合区域地质各类岩体岩性、年龄和面积调查的新成果,认为只有少量锆石可直接根据特定年龄峰值进行物源判别,如<50、250~270和>3 000 Ma的3组锆石分别源自长江上游的昌都地块与金沙江缝合带、扬子地块北缘的峨眉山玄武岩省和三峡地区的崆岭群;联用锆石U-Pb年龄与εHf (t)值可进一步提高物源判别精度;但需注意再旋回的沉积锆石对沉积物源判别的影响。
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  • 收稿日期:  2012-05-15
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长江流域岩体锆石U-Pb年龄与Hf同位素特征及沉积物源示踪意义

doi: 10.3724/SP.J.1140.2013.05097
    作者简介:

    王扬扬(1987-),女,博士生,主要研究方向为沉积地球化学.

基金项目:

国家自然科学基金项目(41076016,40830107);教育部高等学校博士学科点专项科研基金(20090072110004);中国地质调查局海保工程专项(GZH201100203);海洋地质国家重点实验室课题(MG200907);中央高校基本科研业务费专项资金

  • 中图分类号: P595

摘要: 物源精细示踪是当前单矿物颗粒微区分析技术运用的重要领域。长江流域因面积巨大、源岩构成与分布非常复杂,充分掌握流域内岩体锆石U-Pb年龄等微区分析信息成为精细物源示踪的关键。在系统搜集与分析近十年来发表的长江流域内岩体锆石U-Pb年龄和Hf同位素组成的数据资料,结合区域地质各类岩体岩性、年龄和面积调查的新成果,认为只有少量锆石可直接根据特定年龄峰值进行物源判别,如<50、250~270和>3 000 Ma的3组锆石分别源自长江上游的昌都地块与金沙江缝合带、扬子地块北缘的峨眉山玄武岩省和三峡地区的崆岭群;联用锆石U-Pb年龄与εHf (t)值可进一步提高物源判别精度;但需注意再旋回的沉积锆石对沉积物源判别的影响。

English Abstract

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