莺歌海盆地东方区晚中新世粗粒与细粒沉积物源汇系统特征及成因分析

doi:10.3799/dqkx.2025.251

莺歌海盆地东方区晚中新世粗粒与细粒沉积物源汇系统特征及成因分析

doi: 10.3799/dqkx.2025.251

何小胡^1,2,3,
姜涛^1, ,,
冯婧姿¹,
张亚震^2,3,
袁丙龙^2,3,
刘国昌⁴,
何杰¹

1. 中国石油大学(北京)油气资源与工程全国重点实验室, 北京, 102249;
2. 中国地质大学海洋地质资源湖北省重点实验室, 湖北武汉, 430074;
3. 中海石油(中国)有限公司海南分公司, 海南海口, 570312;
4. 中国海油南海油气能源院士工作站, 海口, 570312

基金项目:

海南省院士创新平台科研项目(编号YSPTZX202302)

海南省重点研发项目专项研究基金(编号ZDYF2024GXJS293)

国家自然科学基金项目(编号42276073,42202119)联合资助的成果

详细信息

作者简介:
何小胡(1982-),男,高级工程师,研究方向:南海西部石油天然气勘探综合研究与管理.E-mail:hexh@cnooc.com

通讯作者:
姜涛(1979-),男,教授,研究方向:海洋地质与资源.ORCID:0000-0001-8845-8582.E-mail:taojiang@cug.edu.cn

中图分类号: P618
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出版历程
- 收稿日期: 2025-09-18
- 网络出版日期: 2025-12-03

摘要

摘要: 为了解莺歌海盆地东方区黄流组一段粗粒与细粒沉积物源汇系统的差异特征，综合运用矿物学、锆石U-Pb年代学和Sr-Nd同位素分析方法，分别对莺歌海盆地东方区黄流组一段粗粒与细粒沉积物的物源特征进行定量分析。结果表明：莺歌海盆地东方区晚中新世粗粒沉积物的红河物源平均供源占比可达约65%，越南中部物源平均供源占比约为16%，海南岛物源平均供源占比约为19%；细粒沉积物的红河物源平均供源占比约为44%，越南中部物源平均供源占比约为37%，海南岛物源平均供源占比约为19%。粗粒沉积物比细粒沉积物具有更高的红河物源和更少的越南中部物源，推测是受晚中新世青藏高原快速隆升，红河断裂反转的影响。此外，粗粒与细粒沉积物源汇系统特征的差异还受到沉积物中较低的重矿物和较高的泥质含量的影响。
- 莺歌海盆地 /
- 源汇系统 /
- 重矿物 /
- 锆石U-Pb年代学 /
- Sr-Nd同位素
Abstract: In order to understand the different characteristics of the source-sink system of the first member of the Huangliu Formation in the eastern part of the Yinggehai Basin, the provenance characteristics of coarse-grained and fine-grained sediments in the first member of Huangliu Formation in the eastern part of Yinggehai Basin were quantitatively analyzed by means of mineralogy, zircon U-Pb chronology and Sr-Nd isotope analysis. The results show that the average source proportion of the late Miocene coarse-grained sediments in the eastern part of Yinggehai Basin can reach ~65%, that in central Vietnam is ~16%, and that in Hainan Island is ~19%. The average source of fine sediment is ~44% in Red River, ~37% in central Vietnam and ~19% in Hainan Island. Coarse-grained sediments have higher Red River provenance and less central Vietnam provenance than fine-grained sediments, presumably due to the rapid uplift of the Qinghai-Tibet Plateau and the reversal of the Red River Fault Zone in the Late Miocene. Furthermore, the differences in the characteristics of the source-sink systems of coarse-grained and fine-grained sediment are also influenced by the lower content of heavy minerals and the higher content of mud in the sediments.
- Yinggehai Basin /
- Source-sink system /
- Heavy minerals /
- Zircon U-Pb chronology /
- Sr-Nd isotope

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