南黄海MIS 3时期古黄河三角洲沉积范围的研究
1. 中山大学, 海洋工程与技术学院, 广东珠海 519800
2. 江苏第二师范学院, 城市与资源环境学院, 江苏南京 211200
3. 南京大学, 地理与海洋科学学院, 江苏南京 210023
| 摘 要： | 在南黄海西部海区废黄河三角洲之下存在一个分布范围较大、形成时间更早的（MIS 3时期）古黄河三角洲。通过详细梳理近几十年来相关研究成果，对本区MIS 3时期古黄河三角洲沉积范围主要有三类观点：第一类认为其分布于35°45′N~34°30′N, 123°E~124°E之间，前缘位于深水区；第二类认为其分布于山东半岛南部（36°N附近）至34°45′N, 120°E~123°15′E之间，前缘位于浅水区；第三类认为其南北方向上由海州湾至33°15′N，东西方向上由近岸至123°E之间，前缘位于浅水区。综合分析浅地层地震剖面、钻孔沉积物年代及长江、黄河沉积物特征等资料表明，目前存在对三角洲的判识依据有待商榷、研究分析所采用的钻孔时间分辨率偏低、三角洲物质来源不确定性等问题。为明确MIS 3时期古黄河三角洲沉积范围，今后需在深入认识三角洲沉积反射层理与结构、提高钻孔时间分辨率、精细三角洲物质来源及加强陆域古三角洲分布情况的探索等方面进一步开展深入研究。 |
| 关 键 词： | 古三角洲; 古黄河; 沉积范围; MIS 3; 南黄海陆架 |
| DOI： | 10.57237/j.res.2024.01.001 |
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收稿日期: 2023-11-27
接受日期: 2023-12-28
在线出版日期: 2024-01-20
The Sedimentation Range of the MIS 3 Old Yellow River Delta, South Yellow Sea
1. School of Ocean Engineering and Technology, Sun Yat-Sen University, Zhuhai 519800, China
2. School of Urban, Resource and Environmental Sciences, Jiangsu Second Normal University, Nanjing 211200, China
3. School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
| Abstract: | An old Yellow River delta with a larger distribution and earlier formation (MIS 3) under the Abandoned Yellow River delta in the western part of the South Yellow Sea (SYS). Based on the published studies and relevant research in recent decades, there are three points of view on the sedimentation range of the MIS 3 old Yellow River Delta in SYS: (1) It is distributed from 35°45′N to 34°30′N, between 123°E and 124°E, with the front edge located in deep water; (2) It is distributed from the southern part of Shandong Peninsula (near 36°N) to 34°45′N, between 120°E and 123°15′E, with the front edge located in shallow water; (3) It is distributed from Haizhou Bay to 33°15′N in the north-south direction, and from near shore to 123°E in the east-west direction, with the front edge located in shallow water. The comprehensive analysis of the shallow stratigraphic seismic profiles, borehole sediment ages and sediment characteristics of the Yangtze rivers and Yellow rivers indicates that there is questionable basis for delta identification, such as low temporal resolution of the boreholes and uncertainty of the deltaic material sources. In order to clarify the depositional extent of the MIS 3 old Yellow River delta, we must conduct further in-depth research in understanding of the deltaic sedimentary reflection structure, improving the borehole time resolution, refining the source of deltaic material and strengthening the exploration of the distribution of the terrestrial old delta. |
| Keywords: | Paleodelta; Old Yellow River; Sedimentation Range; MIS 3; South Yellow Sea |
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