Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1306/11211817270 |
Detrital zircon ages: A key to unraveling provenance variations in the eastern Yinggehai-Song Hong Basin, South China Sea | |
Wang, Ce1; Liang, Xinquan1; Foster, David A.2; Liang, Xirong1; Tong, Chuanxin3; Liu, Ping3 | |
2019-07-15 | |
发表期刊 | AAPG BULLETIN
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ISSN | 0149-1423 |
EISSN | 1558-9153 |
出版年 | 2019 |
卷号 | 103期号:7页码:1525-1552 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China; USA |
英文摘要 | The Yinggehai-Song Hong Basin has received a large amount of terrigenous sediment from different continental blocks since the Paleogene. The Yingdong slope, which is located on the eastern side of this basin, is an important potential gas province, but the provenance of the marine sediments in this area are poorly understood. The detrital zircon U-Pb geochronology of sedimentary rocks from the lower Miocene to Quaternary is examined in this study to investigate the temporal and spatial variations in provenance since the early Miocene. The U-Pb ages of detrital zircon range from 3078 to 30 Ma, suggesting that sediment input is derived from multiple sources. Detailed analyses of these components indicate that both the Red River and Hainan are likely the major sources of the sediments on the Yingdong slope, with additional minor contributions from central Vietnam (eastern Indochina block) and possibly the Songpan-Garze block. Variations in the dominant detrital zircon populations within strati-graphic successions display an increasing contribution from the Red River since the middle Miocene. This resulted from the progradation of the Red River Delta in the northern basin and may have also been influenced by regional surface uplift and associated climate changes in East Asia. This study shows that the Red River has had a relatively stable provenance since at least the early Miocene, indicating that any large-scale drainage capture of the Red River should have occurred before circa 23 Ma. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000475472700001 |
WOS关键词 | U-PB GEOCHRONOLOGY ; RIVER SHEAR ZONE ; TIBETAN PLATEAU ; HAINAN ISLAND ; UPPER MIOCENE ; HF ISOTOPES ; QIONGDONGNAN BASINS ; CENOZOIC TECTONICS ; CRUSTAL EVOLUTION ; HEAVY MINERALS |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/184957 |
专题 | 地球科学 |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Guangdong, Peoples R China; 2.Univ Florida, Dept Geol Sci, Gainesville, FL USA; 3.China Natl Offshore Oil Corp Ltd, Zhanjiang Branch, Zhanjiang, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Ce,Liang, Xinquan,Foster, David A.,et al. Detrital zircon ages: A key to unraveling provenance variations in the eastern Yinggehai-Song Hong Basin, South China Sea[J]. AAPG BULLETIN,2019,103(7):1525-1552. |
APA | Wang, Ce,Liang, Xinquan,Foster, David A.,Liang, Xirong,Tong, Chuanxin,&Liu, Ping.(2019).Detrital zircon ages: A key to unraveling provenance variations in the eastern Yinggehai-Song Hong Basin, South China Sea.AAPG BULLETIN,103(7),1525-1552. |
MLA | Wang, Ce,et al."Detrital zircon ages: A key to unraveling provenance variations in the eastern Yinggehai-Song Hong Basin, South China Sea".AAPG BULLETIN 103.7(2019):1525-1552. |
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