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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第43卷

期数:

2021年第05期

页码:

868-886

栏目:

基础地质与矿产地质

出版日期:

2021-09-15

文章信息/Info

Title:

Detrital Zircon U-Pb Dating of Middle Devonian Yangmaba Formation in Beichuan Area of Sichuan, China and Its Tectonic Significance

文章编号:

1672-6561(2021)05-0868-19

作者:

郭 涛¹; 2; 胡作维¹; 2*; 李 云¹; 2; 史 格¹; 2; 詹旗胜¹; 2; 李韶昱¹; 2; 管晋红¹; 2

(1. 成都理工大学 沉积地质研究院,四川 成都 610059; 2. 成都理工大学 油气藏地质及开发工程国家重点实验室,四川 成都 610059)

Author(s):

GUO Tao¹; 2;  HU Zuo-wei¹; 2*;  LI Yun¹; 2;  SHI Ge¹; 2;  ZHAN Qi-sheng¹; 2;  LI Shao-yu¹; 2;  GUAN Jin-hong¹; 2

(1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China)

关键词:

物源;  碎屑锆石U-Pb年龄;  中泥盆统;  沉积再旋回;  古地理;  冈瓦纳大陆;  扬子板块;  四川

Keywords:

provenance;  detrital zircon U-Pb age;  Middle Devonian;  sedimentary recycle;  paleogeography;  Gondwana continent;  Yangtze block;  Sichuan

分类号:

P597

DOI:

10.19814/j.jese.2021.01013

文献标志码:

A

摘要:

扬子板块与冈瓦纳大陆在中泥盆世是否存在亲缘性一直有较大的分歧,两者的古地理位置关系对扬子板块的构造演化具有重要意义。扬子板块西北缘四川北川地区中泥盆统养马坝组的碎屑锆石U-Pb定年结果表明:碎屑锆石年龄谱主要集中在1 000～900、850～720、650～500 Ma等3个区间,与冈瓦纳大陆以及下伏地层志留系碎屑锆石年龄谱进行比较,发现它们具有相似的碎屑锆石特征,均显示出典型的冈瓦纳特征。结合古地磁数据、养马坝组沉积环境演化特征、岩相古地理特征、大地构造演化特征以及前人研究成果等信息,综合分析了研究区养马坝组陆源碎屑的可能来源,认为其碎屑物质可能来自于下伏地层志留系沉积岩的沉积再旋回,中泥盆世扬子板块与冈瓦纳大陆不具有亲缘性。

Abstract:

Whether Yangtze block and Gondwana continent are related to each other during Middle Devonian, the paleo-geographical relationship between the two is of great significance to the tectonic evolution of Yangtze block. Based on the detrital zircon U-Pb chronology of Middle Devonian Yangmaba Formation in Beichuan area of Sichuan on the northwestern margin of Yangtze block, the results show that the age spectrum of detrital zircon is mainly concentrated in three intervals of 1 000-900, 850-720 and 650-500 Ma. Compared with Gondwana continent and the underlying Silurian detrital zircon age spectrum, it is found that they have similar detrital zircon characteristics, all showing typical Gondwana characteristics. Combined with the paleomagnetic data, the evolution characteristics of sedimentary environment of Yangmaba Formation, the evolution characteristics of lithofacies and paleogeography, the characteristics of tectonic evolution, and the results of previous studies, the possible sources of terrigenous clastics in Yangmaba Formation are comprehensively analyzed. The detrital material in Yangmaba Formation may come from the sedimentary recycle of the underlying Silurian sedimentary rocks, and Yangtze block is not related to Gondwana continent during Middle Devonian.

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备注/Memo

备注/Memo:

收稿日期:2021-01-18; 修回日期:2021-04-20投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41772100); 国家科技重大专项项目(2016ZX05050)
作者简介:郭 涛(1995-),女,山西晋中人,理学硕士研究生,E-mail:526750403@qq.com。
*通讯作者:胡作维(1981-),男,广东佛山人,教授,理学博士,E-mail:huzuowei@foxmail.com。

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