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Temporal and spatial evolution and genetic mechanism of shallow continental shelf sandbodies in the northwestern Zhusan Depression
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Guangzeng Song1, 2, Ming Li3, Shuai Zhang3, Detian Yan2, Entao Liu2, Si Chen2
Haiyang Xuebao | 2023, 45(2) : 62 - 73
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Haiyang Xuebao | 2023, 45(2): 62-73
Article
Temporal and spatial evolution and genetic mechanism of shallow continental shelf sandbodies in the northwestern Zhusan Depression
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Guangzeng Song1, 2, Ming Li3, Shuai Zhang3, Detian Yan2, Entao Liu2, Si Chen2
Affiliations
  • 1School of Water Conservancy and Environment, University of Jinan, Ji’nan 250022, China
  • 2Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
  • 3Hainan Branch of China National Offshore Oil Corporation Limited, Haikou 570300, China
Published: 2023-02-01 doi: 10.12284/hyxb2023017
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In order to clarify the genetic mechanism of shallow continental shelf sandbodies in the upper submember of the first member of Zhujiang Formation in the northwestern Zhusan Depression, with integrated use of geological and geophysical data, the five-order sequence framework was established firstly, inside of which, the shallow continental shelf sandbodies were identified and quantitatively described, and the temporal and spatial evolution of the shallow continental shelf sandbodies were analyzed, and the genetic mechanism was discussed. The results show that: (1) The upper submember of the first member of Zhujiang Formation in the study area can be divided into four five-order sequences, which were numbered as FS4, FS3, FS2 and FS1 from bottom to top. (2) There are two types of shelf sand bodies: tidal sand ridge and offshore sand bar, which are distributed in NW−SE direction. Tidal sand ridges are mainly distributed in the west of the study area, while offshore sand bars are concentrated in the east. (3) In the three five-order sequences FS4, FS3 and FS2, the scale and quantity of both tidal sand rdiges and offshore sand bars are relatively large, while in the upper five-order sequence FS1, the scale and quantity present poor. (4) Sedimentary base level (hydrodynamic condition), synsedimentary geomorphology and sediment debris supply jointly affected the development scale, distribution characteristics and temporal and spatial evolution of tidal sand ridges and offshore sand bars, which comprehensively constituted the genetic mechanism of shallow continental shelf sand bodies in the northwestern Zhusan Depression.

shallow continental shelf sandbody  /  subtle trap  /  high frequency sequence  /  base-level cycle  /  Zhusan Depression
Guangzeng Song, Ming Li, Shuai Zhang, Detian Yan, Entao Liu, Si Chen. Temporal and spatial evolution and genetic mechanism of shallow continental shelf sandbodies in the northwestern Zhusan Depression[J]. Haiyang Xuebao, 2023 , 45 (2) : 62 -73 . DOI: 10.12284/hyxb2023017
Year 2023 volume 45 Issue 2
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Article Info
doi: 10.12284/hyxb2023017
  • Receive Date:2022-05-29
  • Online Date:2025-12-26
  • Published:2023-02-01
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  • Received:2022-05-29
  • Revised:2022-08-14
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Affiliations
    1School of Water Conservancy and Environment, University of Jinan, Ji’nan 250022, China
    2Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
    3Hainan Branch of China National Offshore Oil Corporation Limited, Haikou 570300, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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