鄂尔多斯盆地东南部韩城地区延长组碎屑锆石U-Pb年代学特征及物源指示意义

刘旭东; 张忠义; 彭恒; 刘江燕; 丰孝林; 张晓磊; 王建强

doi:10.16152/j.cnki.xdxbzr.2024-04-015

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鄂尔多斯盆地东南部韩城地区延长组碎屑锆石U-Pb年代学特征及物源指示意义

地球科学 | 更新时间：2024-08-01

- 鄂尔多斯盆地东南部韩城地区延长组碎屑锆石U-Pb年代学特征及物源指示意义
- Detrital zircons from the Yanchang Formation in Hancheng area, southeastern Ordos Basin U-Pb chronological characteristics and provenance indication significance
- 西北大学学报（自然科学版） 2024年54卷第4期页码：741-754
- 作者机构：
  
  1.西北大学　大陆动力学国家重点实验室/地质学系/赵文智院士工作室，陕西　西安　710069
  2.低渗透油气田勘探开发　国家工程实验室，陕西　西安　710018
  3.中国石油长庆油田分公司勘探开发研究院，陕西　西安　710018
- 作者简介：
  
  刘旭东，男，从事盆地构造相关研究，202021441@stumail.nwu.edu.cn。
  王建强，男，副教授，博士生导师，从事盆地地质与热年代学研究，wjq@nwu.edu.cn。
- 基金信息：
  
  国家自然科学基金(42230815;41972153);陕西省高校青年创新团队科研项目(22JP086);陕西省高校青年创新团队(2019-45)
- DOI：10.16152/j.cnki.xdxbzr.2024-04-015
  中图分类号： P62
- 纸质出版日期：2024-08-25，
  
  收稿日期：2024-01-09，
- 稿件说明：
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刘旭东, 张忠义, 彭恒, 等. 鄂尔多斯盆地东南部韩城地区延长组碎屑锆石U-Pb年代学特征及物源指示意义[J]. 西北大学学报（自然科学版）, 2024,54(4):741-754.

LIU Xudong, ZHANG Zhongyi, PENG Heng, et al. Detrital zircons from the Yanchang Formation in Hancheng area, southeastern Ordos Basin U-Pb chronological characteristics and provenance indication significance[J]. Journal of Northwest University (Natural Science Edition), 2024,54(4):741-754.
刘旭东, 张忠义, 彭恒, 等. 鄂尔多斯盆地东南部韩城地区延长组碎屑锆石U-Pb年代学特征及物源指示意义[J]. 西北大学学报（自然科学版）, 2024,54(4):741-754. DOI： 10.16152/j.cnki.xdxbzr.2024-04-015.

LIU Xudong, ZHANG Zhongyi, PENG Heng, et al. Detrital zircons from the Yanchang Formation in Hancheng area, southeastern Ordos Basin U-Pb chronological characteristics and provenance indication significance[J]. Journal of Northwest University (Natural Science Edition), 2024,54(4):741-754. DOI： 10.16152/j.cnki.xdxbzr.2024-04-015.

摘要

围绕鄂尔多斯盆地东南部中晚三叠世延长组物源演化，以盆地东南部韩城薛峰川地区延长组剖面为研究对象，运用碎屑锆石U-Pb年代学探讨了韩城地区延长期的物源特征。结果表明，韩城薛峰川地区延长组自下而上不同层段碎屑锆石U-Pb年龄谱峰特征基本一致，峰值段主要集中在晚古生代晚期（250~263 Ma）、古元古宙晚期（1 689~1 774 Ma，1 867~1 885 Ma）和古元古宙早期（2 490~2 560 Ma），太古宙年龄仅零星分布，而中新元古宙和早古生代年龄均缺失。综合物源对比认为，韩城地区延长期盆地物源主要来自于其东北部的华北克拉通内部及阴山造山带地区，而华北板块南缘及秦岭地区的南部物源特征不明显。这种物源特征与盆地西南部延长期物源复杂多变的特点形成了鲜明对比，表明鄂尔多斯盆地东南部延长期具有稳定的东北物源特征，推测其南地区在延长期仍存在分隔南部物源的深湖相沉积，该认识对探讨延长期湖盆演化具有重要意义。

Abstract

Focusing on the provenance evolution of the Yanchang Formation in the Middle and Late Triassic in the southeastern part of Ordos Basin

this paper investigates the provenance characteristics of the Yanchang Formation in the southeastern part of the basin by using detrital zircon U-Pb chronology. The results show that the U-Pb age spectra of detrital zircons from different strata of Yanchang Formation in Xufengchuan area

Hancheng are consistent

and the peak segments are mainly concentrated in the late Late Paleozoic (250~263 Ma) and late Paleoproterozoic (1 689~1 774 Ma

1 867~1 885 Ma) and early Paleoproterozoic (2 490~2 560 Ma)

the Archean ages are only scattered

while the Middle Proterozoic and Early Paleozoic ages are missing. The comprehensive provenance comparison shows that the provenance of Yanchang basin in Hancheng area mainly comes from the North China Craton and Yinshan Orogenic belt in the northeast of the basin

while the provenance characteristics of the south margin of North China Plate and the south Qinling area are not obvious. These provenance characteristics are in sharp contrast to the complex and variable provenance characteristics of the extended period in the southwest of the Ordos Basin

suggesting that the southeast of the Ordos Basin has stable northeast provenance characteristics. It is speculated that there are still deep lacustrine sediments separating the southern provenance during the extended period in the southern part of the Ordos Basin

which is of great significance for the study of the evolution of the lake basin during the extended period.

关键词

鄂尔多斯盆地延长组碎屑锆石U-Pb年代学物源特征

Keywords

Ordos BasinYanchang Formationdetrital zircon U-Pb geochronologyprovenance characteristics

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