江汉盆地新生代早期河流演化研究：来自地表河流和盆地钻孔碎屑锆石U-Pb年龄的约束

张洋; 陈孝康; 林旭; 李长安; 刘海金; 刘杰

doi:10.19509/j.cnki.dzkq.tb20220154

江汉盆地新生代早期河流演化研究：来自地表河流和盆地钻孔碎屑锆石U-Pb年龄的约束

doi: 10.19509/j.cnki.dzkq.tb20220154

张洋^1a,,
陈孝康^1a,
林旭^{1a, 1b, ,},
李长安²,
刘海金³,
刘杰^1a

1a.
三峡大学土木与建筑学院, 湖北宜昌 443002
1b.
三峡大学三峡地区地质灾害与生态环境湖北省协同创新中心, 湖北宜昌 443002
2.
中国地质大学(武汉)地理与信息工程学院, 武汉 430078
3.
东华理工大学地球科学学院, 南昌 330013

基金项目:

国家自然科学基金项目 41972212

湖北省楚天学者人才计划 8210403

详细信息

作者简介:
张洋(1987—), 男, 讲师, 主要从事建筑与土木工程相关研究工作。E-mail: 33702577@cug.edu.cn

通讯作者:
林旭(1984—), 男, 副教授, 主要从事青藏高原隆升和中国大河起源的教学和科研工作。E-mail: hanwuji-life@163.com

中图分类号: P534.6;P343.1
计量
- 文章访问数: 724
- PDF下载量: 81
- 被引次数: 0
出版历程
- 收稿日期: 2022-04-08
- 录用日期: 2022-05-09
- 修回日期: 2022-04-20

Early Cenozoic drainage evolution in the Jianghan Basin: Constraints from detrital zircon U-Pb ages of surface rivers and cores in the basin

Zhang Yang^{1a
,},
Chen Xiaokang^1a,
Lin Xu^{1a, 1b
, ,},
Li Chang'an²,
Liu Haijin³,
Liu Jie^1a

1a.
School of Civil Engineering and Architecture, China Three Gorges University, Yichang Hubei 443002, China
1b.
Collaborative Innovation Center for Geo-Hazards and Eco-Environment in Three Gorges Area, China Three Gorges University, Yichang Hubei 443002, China
2.
School of Geography and Information Engineering, China University of Geosciences(Wuhan), Wuhan 430078, China
3.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China

摘要

摘要:
大型河流的演化是构造-气候相互作用的结果, 对其开展演化历史研究是揭示地球深部动力过程对地表过程影响的关键切入点。保存于江汉盆地的新生代地层详细记录了汉江、长江等大型河流的演化信息。通过对汉江流域进行系统的碎屑锆石U-Pb年龄分析(n = 690), 结合前人在江汉盆地主要汇入河流发表的锆石U-Pb年龄数据, 将其与江汉盆地内早始新世沉积钻孔的锆石U-Pb年龄数据进行了对比。结果表明, 汉江下游的碎屑锆石U-Pb年龄物质组成混合了秦岭西部、大巴山和秦岭东部的河流碎屑物质信号, 采用其下游干流样品的锆石U-Pb年龄组成进行物源对比更具有代表性; 江汉盆地早始新世的碎屑物质主要来自秦岭和大别山, 这主要归结为江汉盆地内部断陷与这些造山带的隆升形成显著的地势差异, 为大型河流发育奠定基础; 发源于武陵山和黄陵背斜的河流此时并不是江汉盆地中部、东部和南部凹陷的物质供给河流; 黄陵背斜以西的长江在早始新世未进入江汉盆地。总体而言, 江汉盆地在新生代早期的沉积物源以近源造山带为主, 是对盆地周缘造山带隆升和类季风气候的沉积响应。
- 江汉盆地 /
- 锆石 /
- U-Pb年龄 /
- 河流演化
Abstract: Objective
The evolution of large rivers is closely linked to the interactions between tectonic and climatic processes. Understanding the evolutionary history of these rivers is crucial for uncovering the influence of deep dynamic processes on the Earth's surface. In the Jianghan Basin, the preserved Cenozoic strata provide valuable insights into the evolutionary history of the Han and Yangtze Rivers.
Methods
By conducting a systematic analysis of detrital zircon U-Pb ages (n=690) in the Hanjiang River Basin, the sediments in the lower reaches of the Hanjiang River contain a mixture of fluvial detrital signals from the Qinling and Dabie mountains. The detrital zircon U-Pb ages of these samples from the lower reaches of the Hanjiang River are more representative for determining their provenance. We have compared these new data with previously published fluvial sedimentary zircon U-Pb ages from the Jianghan Basin, as well as detrital zircon U-Pb ages from drilling cores obtained from Early Eocene strata in the basin.
Results
Provenance analysis reveals that the detrital material in the Jianghan Basin during the Early Eocene was primarily derived from the Qinling-Dabie Mountains. This can be attributed to the significant difference in elevation between the depression within the Jianghan Basin and the surrounding uplifted orogenic belts, which provided the necessary conditions for the development of large rivers. It is important to note that the Wuling Mountain and Huangling Anticline rivers did not serve as the main sources of sediment supply for the central, eastern, and southern depressions of the Jianghan Basin during this time period. Additionally, the Yangtze River, located west of the Huangling Anticline, did not flow into the Jianghan Basin in the Early Eocene.
Conclusion
Overall, the sediments in the Jianghan Basin were predominantly proximal deposits sourced from the adjacent orogenic belt, which can be attributed to the exhumation of the orogenic belt and a monsoon-like climate in the early Cenozoic era.
- Jianghan Basin /
- zircon /
- U-Pb ages /
- river evolution
注释:

(所有作者声明不存在利益冲突)

HTML全文

图 1 江汉盆地位置图

图中数字分别代表前人采样点(1^[5]，2^[6]，3^[7])。1为长江、汉江和湘江的采样点，分别位于宜昌、钟祥和长沙；2为汉江的采样点，靠近武汉；3的采样点主要位于长江各主要支流汇入其干流前几千米处

Figure 1. Location of the Jianghan Basin

下载: 全尺寸图片幻灯片

图 2 江汉盆地地层构造划分和地层柱状图

a. 江汉盆地构造单元划分(据文献[31]修改)，c-c^′代表图 2-c中的剖面位置; b. 江汉盆地沉积地层柱状图(据文献[31]修改); c. 江汉盆地剖面c-c^′古近纪时沉积相复原图(据文献[32]修改)

Figure 2. Stratigraphic structure division and column chart of the Jianghan Basin

下载: 全尺寸图片幻灯片

图 3 江汉盆地钻孔位置图

a. 江汉盆地地质图(据文献[36]修改); b. 钻孔采样图(据文献[36])

Figure 3. Borehole locations in the Jianghan Basin

下载: 全尺寸图片幻灯片

图 4 野外样品采集点分布图

图中数字代表前人采样点(1^[5]、2^[29]、3^[6])，1和2采样点靠近襄阳，3采样点靠近武汉

Figure 4. Distribution of sampling locations with the number for previous sampling points

下载: 全尺寸图片幻灯片

图 5 锆石Th/U结果散点图

Figure 5. Scatter plot of the ratio of Th/U for detrital zircon grains

下载: 全尺寸图片幻灯片

图 6 江汉及唐白河锆石U-Pb年龄频率分布图

a~g. 汉江上游和中游(本次研究); h. 唐白河(据文献[26]); i. 汉江下游(据文献[40])

Figure 6. Frequency distribution of detrital zircon U-Pb ages in the Hanjiag river and Tangbai river

下载: 全尺寸图片幻灯片

图 7 汉江盆地锆石U-Pb年龄频率分布图

a~e. 钻孔数据(据文献[36]); f. 长江(据文献[29]); g. 汉江(据文献[6]); h~l. 沮漳河、湘江、清江+澧水+沅江、汨罗江+陆水、澴水+举水+巴水(据文献[5])

Figure 7. U-Pb age frequency distribution of zircons in the Jianghan Basin

下载: 全尺寸图片幻灯片

图 8 江汉盆地锆石U-Pb年龄三维MDS图

Figure 8. Three dimensional scaling map of the detrital zircon U-Pb ages in the Jianghan Basin

下载: 全尺寸图片幻灯片

图 9 古地理重建图

a. 早始新世华南板块河流分布图；b. 早古近纪华南板块构造与气候特征图(据文献[52, 62]修改)

Figure 9. Paleogeographic reconstruction

下载: 全尺寸图片幻灯片

表 1 样品采集信息

Table 1. Collected sampling information

河流/钻孔(样品)	采样点	经度(E)	纬度(N)	数据来源
堰河(MX-1)	勉县	106°43′1″	33°08′51″	本研究
漾家河(MX-3)	勉县	106°44′15″	33°07′38″	本研究
汉江(ML-1)	勉县	106°44′43″	33°08′34″	本研究
旬河(XYH-1)	旬阳	109°20′07″	32°49′18″	本研究
汉江(XY-1)	旬阳	109°21′29″	32°46′08″	本研究
堵河(DY-1)	黄龙	110°33′43″	32°41′10″	本研究
汉江(XF-1)	襄阳	111°58′18″	32°05′43″	本研究
汉江	武汉	114°12′02″	30°35′12″	文献[6]
唐白河	襄阳	112°18′36″	32°07′45″	文献[5]
长江	宜昌	111°18′43″	30°39′49″	文献[29]
沮漳河	当阳	111°44′56″	30°53′59″	文献[5]
澴河	孝昌	113°57′47″	31°14′58″	文献[5]
倒水	李集	114°40′08″	30°52′59″	文献[5]
举水	新洲	114°45′42″	30°55′47″	文献[5]
巴河	竹瓦	115°06′11″	30°38′33″	文献[5]
陆水	赤壁	113°51′34″	29°44′56″	文献[5]
汨罗江	汨罗	113°08′54″	28°47′30″	文献[5]
湘江	衡阳	112°56′55″	28°08′21″	文献[29]
资江	桃江	112°11′49″	28°36′09″	文献[5]
沅江	武陵	111°38′27″	28°59′38″	文献[5]
澧水	澧县	111°49′55″	29°37′23″	文献[5]
清江	宜都	107°29′06″	29°32′55″	文献[5]
钻孔(M96)				文献[36]
钻孔(Yx2)				文献[36]
钻孔(Yx1)				文献[36]
钻孔(Y1-1)				文献[36]
钻孔(Jx9)				文献[36]
钻孔(Cc1)				文献[36]
钻孔(H12)				文献[36]

下载: 导出CSV

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