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珠江三角洲西北部晚第四纪沉积演化研究

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通过对珠江三角洲西北部的地层、沉积演化过程开展深入研究,结果显示研究区发育有河流相、滨海相、浅海相和河海混杂相等沉积相;晚更新世时期沉积厚度变化较大,地层垂向相变相似;全新世时期,整体沉积厚度相差不大,受沉积环境和地形地貌影响,地层垂向沉积表现出同期异相性分布.晚第四纪以来,研究区沉积历史海陆交互相相变频繁,形成了复杂多样的三角洲沉积物.
Study on Late Quaternary Sedimentary Evolution in Northwest the Pearl River Delta
Through the in-depth study of the strata and sedimentary evolution process in the northwest of the Pearl River Delta,the results show that the study area has developed sedimentary facies such as fluvial facies,coastal facies,shallow marine facies,and river sea mixed facies;the sedimentary thickness changed greatly during the late Pleistocene,and the vertical facies changes of the strata were similar;during the Holocene period,the overall sedimentary thickness did not differ significantly,and due to the influence of sedimentary environment and topography,the vertical sedimentation of the strata showed a synchronous and heterogeneous distribution.Since the late Quaternary period,the sedimentary history of the study area has undergone frequent phase transitions between land and sea,forming complex and diverse delta sediments.

the Pearl River Deltalate Quaternarydevelopmental characteristicssedimentary evolution

史秋艾

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广东煤炭地质局,广东广州 510000

珠江三角洲 晚第四纪 发育特征 沉积演化

中国煤炭地质总局科技项目

ZMKJ-2020-J10-1

2024

中国煤炭地质
中国煤炭地质总局

中国煤炭地质

CSTPCD
影响因子:0.652
ISSN:1674-1803
年,卷(期):2024.36(7)
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