【摘要】 根据珠江三角洲 16 6个第四纪古三角洲沉积物的测年数据 ,在扣除了古海平面变化、沉积层的压实效应和地壳静力均衡沉降等非构造因素的影响后 ,估算出晚第四纪以来三角洲地区的垂直构造运动速率。估算按北东、近东西和北西向 3组断裂所切截的 11个断块构造区分别进行。结果表明 ,位于三角洲南部的斗门断块和中部的广州 -番禺断块的活动速率相对较高 ,这个特征得到了三角洲晚第四纪古地理演变、断层活动年代学和地震活动研究的初步验证更多还原

【Abstract】 Based on 166 age data of Quaternary deposits in fossil delta, the rate of the vertical motion of the Zhujiang Delta since late Quaternary has been estimated by eliminating the non-tectonic effects, such as the change of ancient sea level, the compaction of sedimentary layer, and the isostatic crustal subsidence. The estimations have been conducted separately for 11 fault block tectonic regions, which are bounded by NE-trending, E-W-trending and NW-trending faults. The results have indicated that the rate of vertical motion of the Doumen fault block in the south and the Guangzhou-Panyu fault block in the middle parts of the Zhujiang Delta is relatively high. This conclusion has been supported by the results of the studies on the changes of ancient geographic environment, the timing of faulting, and the late Quaternary paleo-seismicity in the Zhujiang Delta area. In contrast to the previous studies, the present study emphasizes the changes of vertical motion rate in different fault blocks and in different time. The result of this study indicates that the secondary fault blocks of the Zhujiang Delta were dominated by elevation motion at a rate of 1～2mm/a during the early Holocene (10～4ka), and were dominated by subsidence at a rate of -3～-4mm/a during the late Holocene (～4ka). The elevation rates of Guangzhou-Panyu, Guanghua Plain, Shunde and Doumen fault blocks were greater than 1mm/a, while the subsidence rates in Guangzhou-Panyu, Shenzhen-Hong Kong, Zhongshan and Doumen fault blocks exceeded -2mm/a.更多还原