珠三坳陷珠江组一段沉积体系演化过程及其控制因素

吴太霏; 王华; 刘恩涛; 陈林; 张璐; 陈思; 谢卫东; 谷志宇; 张启扬

doi:10.19509/j.cnki.dzkq.tb20220484

珠三坳陷珠江组一段沉积体系演化过程及其控制因素

doi: 10.19509/j.cnki.dzkq.tb20220484

吴太霏^1a,,
王华^1a, ,,
刘恩涛^1b,
陈林²,
张璐²,
陈思^1a,
谢卫东^1a,
谷志宇^1b,
张启扬^1a

1a.
中国地质大学(武汉)资源学院, 武汉 430074
1b.
中国地质大学(武汉)海洋学院, 武汉 430074
2.
中海石油(中国)有限公司湛江分公司, 广东湛江 524057

基金项目:

国家自然科学基金项目"浅海外陆架海底扇-水道重力流发育机制与储层非均质性表征" 2017ZX05035004

"中国海油南海油气资源院士工作站"支持

详细信息

作者简介:
吴太霏, E-mail: 1202020073@cug.edu.cn

通讯作者:
王华, E-mail: Wanghua@cug.edu.cn

中图分类号: P618.130.2
计量
- 文章访问数: 30
- PDF下载量: 4
- 被引次数: 0
出版历程
- 收稿日期: 2022-09-01
- 录用日期: 2022-12-13
- 修回日期: 2022-12-10

Evolutionary and controlling factors of sedimentary system in the First Member of the Zhujiang Formation in the Zhu Ⅲ Depression

WU Taifei^{1a
,},
WANG Hua^{1a
, ,},
LIU Entao^1b,
CHEN Lin²,
ZHANG Lu²,
CHEN Si^1a,
XIE Weidong^1a,
GU Zhiyu^1b,
ZHANG Qiyang^1a

1a.
School of Earth Resources, China University of Geosciences(Wuhan), Wuhan 430074, China
1b.
College of Marine Science and Technology, China University of Geosciences(Wuhan), Wuhan 430074, China
2.
Zhanjiang Branch of CNOOC China Limited, Zhanjiang Guangdong 524057, China

More Information

Author Bio:
WU Taifei, E-mail: 1202020073@cug.edu.cn

Corresponding author: WANG Hua, E-mail: Wanghua@cug.edu.cn

摘要

摘要:
珠江组一段沉积时期是珠三坳陷沉积体系演变的重要时期, 由早期的大范围三角洲沉积体系演化为晚期的浅海陆架沉积体系, 对其演化过程及控制因素展开研究, 不仅有利于揭示海侵过程中沉积体系演化过程, 而且对浅海陆架有利沉积相带预测具有指导意义。综合利用岩心、测井以及高分辨率三维地震资料, 建立了珠三坳陷珠江组一段四级层序地层格架, 通过地质-地球物理结合方法查明了珠江组一段沉积体系的时空演化特征, 并讨论了沉积演化的主控因素。研究表明: 珠三坳陷珠江组一段可划分为PS1、PS2、PS3、PS4共4个四级层序。PS3和PS4时期主要发育三角洲前缘沉积, 具有水下分流河道、分流间湾、河口坝和远砂坝等沉积微相组合; PS1和PS2时期以浅海陆架沉积体系大规模发育为特征, 在研究区西部发育潮流砂脊, 东部发育滨外砂坝。珠三坳陷沉积体系的平面展布以及垂向演化受相对海平面变化、物源供给强度、构造沉降与古地貌等综合控制。水下分流河道、潮流砂脊与滨外砂坝等微相砂岩占比高且物性好, 为油气储集的有利沉积相带。
- 沉积体系 /
- 控制因素 /
- 珠江组一段 /
- 珠三坳陷 /
- 珠江口盆地 /
- 浅海陆架 /
- 层序地层
Abstract: Objective
The First Member of the Zhujiang Formation in the Zhu Ⅲ Depression underwent significant changes in its sedimentary system. It transitioned from a large-scale delta system to a shallow sea shelf system. Understanding the evolutionary process and controlling factors of this basin is important for studying the sedimentary system during transgression and predicting favorable sedimentary facies zones on shallow sea shelves.
Methods
In this study, we used core, well logging, and high-resolution 3D seismic data to establish a stratigraphic framework for the First Member of the Zhujiang Formation. By combining geology and geophysics, we determined the temporal and spatial evolution characteristics of the sedimentary system and discussed the main controlling factors.
Results
Our findings show that the First Member of the Zhujiang Formation can be divided into four sequences: PS1, PS2, PS3, and PS4. PS3 and PS4 were dominated by delta deposits, including underwater distributary channels, estuarine dams, and distal dams. PS1 and PS2 were characterized by the development of large-scale shallow-sea shelf systems, with tidal sand ridges in the west and offshore sand dams in the east. The evolution of the sedimentary system in the Zhu Ⅲ Depression is influenced by sea level changes, source supply intensity, structural subsidence, and paleogeomorphology.
Conclusion
Microfacies sandstones, such as underwater distributary channels, tidal sand ridges, and coastal sand dams, have high percentages and good physical properties, making them favorable sedimentary facies zones for oil and gas reservoirs.
- sedimentary system /
- controlling factor /
- First Member of the Zhujiang Formation /
- Zhu Ⅲ Depression /
- Pearl River Mouth Basin /
- shallow sea shelves /
- stratigraphic framework
注释:

所有作者声明不存在利益冲突。

HTML全文

图 1 珠江口盆地珠三坳陷构造位置图(据文献[22]修改)

Figure 1. Structural location of the ZhuⅢ Depression in the Pearl River Mouth Basin

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图 2 珠江口盆地珠三坳陷地层柱状图(相对海平面变化曲线据文献[27]修改；化学蚀变指数(CIA)曲线据文献[28]修改)

Figure 2. Stratigraphic column of the ZhuⅢ Depression in the Pearl River Mouth Basin

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图 3 D4井层序界面识别示意图

Figure 3. Sequence boundary identification in Well D4

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图 4 地震层序界面特征

Figure 4. Seismic reflective characteristics of sequence boundaries

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图 5 珠三坳陷珠江组一段典型地震相特征(地震剖面位置见图 1)

Figure 5. Characteristics of typical seismic facies of the First Member of the Zhujiang Formation in the Zhu Ⅲ Depression

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图 6 珠三坳陷珠江组一段岩心特征

a.D1井，1 272.74 m，灰色粉砂岩夹泥岩，透镜状层理与波状层理，滨外砂坝；b.D10井，1 270.56 m，灰色粉砂岩，鱼骨状交错层理，潮流砂脊；c.D10井，1 280.94 m，灰色泥质粉砂岩，波状层理与低角度交错层理，潮流砂脊；d.D7井，1 214.25 m，下部灰黑色泥岩，上部灰白色粉砂岩，两期反韵律的叠加，平行层理，河口坝；e.D7井，1 211.3 m，灰白色细砂岩，块状层理，水下分流河道；f.D6井，1 211.5 m，灰白色细砂岩，块状层理，见垂直方解石脉，水下分流河道；g.D4井，1 409.8 m，灰黑色泥岩，含透镜状灰色粉砂岩，波状层理，远砂坝

Figure 6. Core characteristics of the First Member of the Zhujiang Formation in the Zhu Ⅲ Depression

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图 7 珠三坳陷珠江组一段典型测井相特征

a.D4井，PS4，水下分流河道与河口坝；b.D1井，PS3，远砂坝与水下分流河道；c.D4井，PS2，潮流砂脊；d.D1井，PS1，滨外砂坝

Figure 7. Characteristics of the typical logging facies of the First Member of the Zhujiang Formation in the Zhu Ⅲ Depression

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图 8 珠三坳陷珠江组一段NE向连井剖面

Figure 8. NE-directional well connecting section of the First Member of the Zhujiang Formation in the Zhu Ⅲ Depression

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图 9 珠三坳陷琼海凸起PS4~PS1层序砂体体积分数图(a)、地震平面属性图(b)及沉积相垂向演化图(c)

Figure 9. Sand body percentage content diagram (a), seismic attribute map (b) and sedimentary facies diagram (c) of PS4-PS1 in the Qionghai Uplift of the Zhu Ⅲ Depression

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图 10 珠三坳陷琼海凸起T50界面古地貌图

Figure 10. Paleogeomorphology of the T50 interface of the Qionghai Uplift in the Zhu Ⅲ Depression

下载: 全尺寸图片幻灯片

参考文献(43)

[1]	WU X, PU R, ZHANG G, et al. Seismic interpretation of the diapiric structures and gas chimneys in the Liwan gas field, Pearl River Mouth Basin, northern South China Sea[J]. Interpretation, 2018, 6(3): T499-T519. doi: 10.1190/INT-2017-0129.1
[2]	LIU J, ZHANG Z, CHEN Z, et al. Comprehensive identification technology of atypical bright spot oil reservoirs in deep water area of eastern South China Sea[C]//Anon. International Petroleum Technology Conference. [S. l. ]: OnePetro, 2019.
[3]	STUDEMAN M. Calculating China's advances in the South China Sea: Identifying the triggers of "Expansionism"[J]. Naval War College Review, 1998, 51(2): 68-90.
[4]	ZHAO Q, ZHU H, ZHANG X, et al. Geomorphologic reconstruction of an uplift in a continental basin with a source-to-sink balance: An example from the Huizhou-Lufeng Uplift, Pearl River Mouth Basin, South China Sea[J]. Marine and Petroleum Geology, 2021, 128: 104984. doi: 10.1016/j.marpetgeo.2021.104984
[5]	GE J, ZHAO X, TAN M, et al. Sequence stratigraphy and depositional evolution of the northeastern shelf (33.9-10.5 Ma) of the Pearl River Mouth Basin, South China Sea[J]. Marine and Petroleum Geology, 2022, 141: 105697. doi: 10.1016/j.marpetgeo.2022.105697
[6]	张曼莉, 林畅松, 何敏, 等. 珠江口盆地晚渐新世陆架边缘三角洲沉积层序结构及演化[J]. 石油与天然气地质, 2019, 40(4): 875-885. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201904017.htm ZHANG M L, LIN C S, HE M, et al. Sequence architecture and evolution of shelf-margin deltaic systems of the Late Oligocene in Pearl River Mouth Basin[J]. Oil & Gas Geology, 2019, 40(4): 875-885. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201904017.htm
[7]	LI D S. Geologic evolution of petroliferous basins on continental shelf of China[J]. AAPG Bulletin, 1984, 68(8): 993-1003.
[8]	彭松, 李珊珊, 张道军, 等. 珠江口盆地西部早中新世大型浅水三角洲展布特征及有利油气勘探方向[J]. 海洋地质前沿, 2019, 35(6): 46-56. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201906006.htm PENG S, LI S S, ZHANG D J, et al. Distribution pattern of the Early Miocene large shallow water delta in the western Pearl River Mouth Basin and its significance to oil and gas exploration[J]. Marine Geology Frontiers, 2019, 35(6): 46-56. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201906006.htm
[9]	朱筱敏, 葛家旺, 赵宏超, 等. 陆架边缘三角洲研究进展及实例分析[J]. 沉积学报, 2017, 35(5): 945-957. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201705007.htm ZHU X M, GE J W, ZHAO H C, et al, Development of shelf-edge delta researches and typical case analyses[J]. Acta Sedimentologica Sinica, 2017, 35(5): 945-957. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201705007.htm
[10]	徐长贵, 范彩伟. 南海西部近海大中型油气田勘探新进展与思考[J]. 中国海上油气, 2021, 33(2): 13-25. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD202102002.htm XU C G, FAN C W. New exploration progress and thinking of offshore large-medium-sized oil and gas fields in the western South China Sea[J]. China Offshore Oil and Gas, 2021, 33(2): 13-25. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD202102002.htm
[11]	李智高, 丁琳, 李小平, 等. 珠江口盆地珠一坳陷西部中新世早-中期沉积特征及控制因素[J]. 古地理学报, 2022, 24(1): 99-111. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202201008.htm LI Z G, DING L, LI X P, et al, Sedimentary characteristics and controlling factors of the western ZhuⅠ Depression during the Early-Middle Miocene, Pearl River Mouth Basin[J]. Journal of Palaeogeography, 2022, 24(1): 99-111. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX202201008.htm
[12]	钟泽红, 徐万兴, 刘芳, 等. 珠江口盆地西部珠三坳陷珠江组沉积演化[J]. 世界地质, 2018, 37(4): 1122-1136. doi: 10.3969/j.issn.1004-5589.2018.04.013 ZHONG Z H, XU W X, LIU F, et al, Sedimentary evolution of Zhujiang Formation in Zhu Ⅲ Depression, west Pearl River Mouth Basin[J]. Global Geology, 2018, 37(4): 1122-1136. (in Chinese with English abstract) doi: 10.3969/j.issn.1004-5589.2018.04.013
[13]	HE M, ZHUO H, CHEN W, et al. Sequence stratigraphy and depositional architecture of the Pearl River Delta system, northern South China Sea: An interactive response to sea level, tectonics and paleoceanography[J]. Marine and Petroleum Geology, 2017, 84: 76-101. doi: 10.1016/j.marpetgeo.2017.03.022
[14]	YU Y, CAI L, ZHANG C, et al. Sedimentary sequence, evolution model and petroleum geological significance of forced regression: A case study of the Miocene Zhujiang Formation of the Pearl River Mouth Basin in the northern South China Sea[J]. Journal of Marine Science and Engineering, 2021, 9(11): 1298. doi: 10.3390/jmse9111298
[15]	李伟, 左倩媚, 刘平, 等. 珠江口盆地文昌凹陷浅海陆架砂体沉积特征及油气勘探意义[J]. 科学技术与工程, 2019, 19(33): 94-100. doi: 10.3969/j.issn.1671-1815.2019.33.013 LI W, ZUO W M, LIU P, et al. Sedimentary characteristics of continental shelf sand bodies and their significance for the oil-gas exploration in Wenchang Sag of Pearl River Mouth Basin[J]. Science Technology and Engineering, 2019, 19(33): 94-100. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-1815.2019.33.013
[16]	李俊良, 王海荣, 张建新, 等. 珠江口盆地西部珠江组潮流砂脊的分布、形态和水动力机制[J]. 石油与天然气地质, 2010, 31(5): 671-677. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201005020.htm LI J L, WANG H R, ZHANG J X, et al. Distribution, geometry and hydrodynamic mechanism of tidal sand ridges in the Zhujiang Formation, the western Pearl River Mouth Basin[J]. Oil & Gas Geology, 2010, 31(5): 671-677. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201005020.htm
[17]	聂逢君, 姜美珠, 李思田. 南海珠江口盆地珠三坳陷油气输导系统研究[J]. 石油实验地质, 2011, 33(4): 392-401. doi: 10.3969/j.issn.1001-6112.2011.04.013 NIE F J, JIANG M Z, LI S T. Petroleum migration system in Zhu Ⅲ Depression, Pearl River Mouth Basin, South China Sea[J]. Petroleum Geology and Experiment, 2011, 33(4): 392-401. (in Chinese with English abstract) doi: 10.3969/j.issn.1001-6112.2011.04.013
[18]	PINGLU L, CHUNTAO R. Tectonic characteristics and evolution history of the Pearl River Mouth Basin[J]. Tectonophysics, 1994, 235(1/2): 13-25.
[19]	姜华, 王华, 李俊良, 等. 珠江口盆地珠三坳陷层序地层样式分析[J]. 海洋地质与第四纪地质, 2009, 29(1): 87-93. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200901019.htm JIANG H, WANG H, LI J L, et al. Analysis on sequence formation styles of Zhu Ⅲ Depression in Pearl River Mouth Basin[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 87-93. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200901019.htm
[20]	朱伟林, 黎明碧, 吴培康. 珠江口盆地珠三坳陷石油体系[J]. 石油勘探与开发, 1997, 24(6): 21-23. doi: 10.3321/j.issn:1000-0747.1997.06.006 ZHU W L, LI M B, WU P K, et al. Petroleum system of Zhu Ⅲ Depression in Pearl River Mouth Basin[J]. Petroleum Exploration and Development, 1997, 24(6): 21-23. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-0747.1997.06.006
[21]	LI H, CHEN S, ZHANG Y, et al. Faults in the Zhu-3 Depression of Pearl River Mouth Basin and their control over hydrocarbon accumulation[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 115-124.
[22]	杨计海, 杨希冰, 游君君, 等. 珠江口盆地珠三坳陷油气成藏规律及勘探方向[J]. 石油学报, 2019, 40(增刊1): 11-25. doi: 10.7623/syxb2019S1002 YANG J H, YANG X B, YOU J J, et al. Hydrocarbon accumulation law and exploration direction in Zhu Ⅲ Depression, Pearl River Mouth Basin[J]. Acta Petrolei Sinica, 2019, 40(S1): 11-25. (in Chinese with English abstract) doi: 10.7623/syxb2019S1002
[23]	姜华, 王华, 李俊良, 等. 珠江口盆地珠三坳陷油气成藏模式与分布规律[J]. 石油与天然气地质, 2009, 30(3): 275-281. doi: 10.3321/j.issn:0253-9985.2009.03.004 JIANG H, WANG H, LI J L, et al. Research on hydrocarbon pooling and distribution patterns in the Zhu-3 Depression, the Pearl River Mouth Basin[J]. Oil & Gas Geology, 2009, 30(3): 275-281. (in Chinese with English abstract) doi: 10.3321/j.issn:0253-9985.2009.03.004
[24]	陈少平, 王华, 刘丽芳, 等. 断裂时空差异性演化及其对生烃凹陷形成的控制: 以珠江口盆地珠三坳陷为例[J]. 断块油气田, 2015, 22(1): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201501001.htm CHEN S P, WANG H, LIU L F, et al. Space-time diversity evolution of faults and its control on formation of hydrocarbon generation sag: Taking ZhuⅢ Depression in Pearl River Mouth Basin as an example[J]. Fault-Block Oil and Gas Field, 2015, 22(1): 1-6. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201501001.htm
[25]	姜华, 王华, 肖军, 等. 古地貌对边缘海盆地沉积充填特征的控制: 以南海珠江口盆地珠三坳陷为例[J]. 石油天然气学报, 2008, 30(1): 10-15, 387. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200801004.htm JIANG H, WANG H, XIAO J, et al. Control of paleomorphology to sedimentary filling in marginal sea basin: By taking Zhu Ⅲ Depression for Example[J]. Journal of Oil and Gas Technology, 2008, 30(1): 10-15, 387. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200801004.htm
[26]	吴静. 珠江口盆地恩平凹陷北部隆起区油气远源富集与主控因素[J]. 地质科技通报, 2022, 41(4): 117-124. doi: 10.19509/j.cnki.dzkq.2022.0020 WU J. Key factors of far-source hydrocarbon enrichment in the northern uplift area of Enping Sag in Pearl Mouth Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 117-124. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0020
[27]	LIU E T, SI C, YAN D T, et al. Detrital zircon geochronology and heavy mineral composition constraints on provenance evolution in the western Pearl River Mouth Basin, northern South China Sea: A source to sink approach[J]. Marine and Petorleum Geology, 2022, 145: 105884 doi: 10.1016/j.marpetgeo.2022.105884
[28]	林畅松, 施和生, 李浩, 等. 南海北部珠江口盆地陆架边缘斜坡带层序结构和沉积演化及控制作用[J]. 地球科学, 2018, 43(10): 3407-3422. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201810007.htm LIN C S, SHI H S, LI H, et al. Sequence architecture, depositional evolution and controlling processes of continental slope in Pearl River Mouth Basin, northern South China Sea[J]. Earth Science, 2018, 43(10): 3407-3422. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201810007.htm
[29]	王华. 层序地层学基本原理[M]. 武汉: 中国地质大学出版社, 2008. WANG H. The basic theory, method and application of sequence stratigraphy[M]. Wuhan: China University of Geosciences Press, 2008. (in Chinese)
[30]	秦国权. 珠江口盆地新生代晚期层序地层划分和海平面变化[J]. 中国海上油气(地质), 2002, 16(1): 2-11. https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200201000.htm QIN G Q. Late Cenozoic sequence stratigraphy and sea level change in the Pearl River Estuary Basin[J] China Offshore Oil and Gas(Geology), 2002, 16(1): 2-11. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200201000.htm
[31]	黄彦庆, 肖开华, 金武军, 等. 川东北元坝西部须家河组致密砂岩裂缝发育特征及控制因素[J]. 地质科技通报, 2023, 42(2): 105-114. doi: 10.19509/j.cnki.dzkq.2022.0099 HUANG Y Q, XIAO K H, JIN W J, et al. Characteristics and controlling factors of tight sandstone reservoir fractures in the Xujiahe Formation of the western Yuanba area, northeastern Sichuan Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(2): 105-114. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0099
[32]	陈淑鹏, 蔡苏阳, 梁云, 等. 吐哈盆地胜北洼陷中侏罗统致密砂岩储层孔隙发育特征及控制因素[J]. 地质科技通报, 2023, 42(3): 189-200. doi: 10.19509/j.cnki.dzkq.2022.0129 CHEN S P, CAI S Y, LIANG Y, et al. Pore characteristics and its controlling factors in the Middle Jurassic tight sandstone reservoirs of the Shengbei Sag, Turpan-Hami Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 189-200. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.2022.0129
[33]	陈维涛, 杜家元, 龙更生, 等. 珠江口盆地海相层序地层发育的控制因素分析[J]. 沉积学报, 2012, 30(1): 73-83. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201201008.htm CHEN W T, DU J Y, LONG G S, et al. Analysis on controlling factors of marine sequence stratigraphy evolution in Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2012, 30(1): 73-83. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201201008.htm
[34]	JIN S D, WANG H, CAO H Y, et al. Sedimentation of the Paleogene Liushagang Formation and the response to regional tectonics in the regional tectonics in the Fushan Sag, Beibuwan Basin, South China Sea[J]. Austrian Journal of Earth Sciences, 2014, 107(2): 112-130.
[35]	朱锐, 张昌民, 杜家元, 等. 珠江口盆地新近纪海平面升降过程及其对砂体的控制[J]. 高校地质学报, 2015, 21(4): 685-693. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201504013.htm ZHU R, ZHANG C M, DU J Y, et al. Controls of Neogene sea level change on sand bodies in the Pearl River Mouth Basin[J]. Geological Journal of China Universities, 2015, 21(4): 685-693. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201504013.htm
[36]	高志前, 樊太亮, 李岩, 等. 塔里木盆地寒武-奥陶纪海平面升降变化规律研究[J]. 吉林大学学报: 地球科学版, 2006, 36(4): 549-556. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200604008.htm GAO Z Q, FAN T L, LI Y, et al. Study on eustatic sea-level change rule in Cambrian-Ordovician in Tarim Basin[J]. Journal of Jilin University: Earth Science Edition, 2006, 36(4): 549-556. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200604008.htm
[37]	CHEN S, STEEL R, WANG H, et al. Clinoform growth and sediment flux into Late Cenozoic Qiongdongnan shelf margin, South China Sea[J]. Basin Research, 2020, 32: 302-319.
[38]	ZHAO R, CHEN S, OLARIU C, et al. A model for oblique accretion on the South China Sea margin: Red River(Song Hong) sediment transport into Qiongdongnan Basin since Upper Miocene[J]. Marine Geology, 2019, 416: 106001.
[39]	陈梅, 施小斌, 刘凯, 等. 南海北缘珠三坳陷新生代构造沉降特征[J]. 海洋地质与第四纪地质, 2017, 37(6): 47-56. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201706006.htm CHEN M, SHI X B, LIU K, et al. Cenozoic tectonic subsidence of the ZhuⅢ Depression in the Pearl River Mouth Basin, northern South China Sea[J]. Marine Geology & Quaternary Geology, 2017, 37(6): 47-56. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201706006.htm
[40]	ZHAO Y, WANG H, YAN D, et al. Sedimentary characteristics and model of gravity flows in the Eocene Liushagang Formation in Weixi'nan Depression, South China Sea[J]. Journal of Petroleum Science and Engineering, 2020, 190: 107082.
[41]	于海洋, 索艳慧, 杜晓东, 等. 珠江口盆地渐-中新世古气候及物源特征: 以阳江东凹为例[J]. 大地构造与成矿学, 2021, 45(1): 53-63. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202101005.htm YU H Y, SUO Y H, DU X D, et al. Oligocene-Miocene provenance and paleoclimate of the Pearl River Mouth Basin: A case study of the eastern Yangjiang Sag[J]. Geotectonica et Metallogenia, 2021, 45(1): 53-63. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202101005.htm
[42]	刘可行, 甘华军, 陈思, 等. 高精度层序格架下的陆相断陷湖盆沉积体系演化: 以南堡凹陷老爷庙地区东营组三段为例[J]. 地质科技情报, 2019, 38(3): 88-102. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903009.htm LIU K X, GAN H J, CHEN S, et al. Evolution of sedimentary of continental faulted lacustrine basin under high-precision sequence framework: A case from the Third Member of Dongying Formation in Laoyemiao area, Nanpu Sag[J]. Geology and Science Technology Information, 2019, 38(3): 88-102. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903009.htm
[43]	王华, 陈思, 甘华军, 等. 浅海背景下大型浊积扇研究进展及堆积机制探讨: 以莺歌海盆地黄流组重力流为例[J]. 地学前缘, 2015, 22(1): 21-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501004.htm WANG H, CHEN S, GAN H J, et al. Accumulation mechanism of large shallow marine turbidite deposits: A case study of gravity flow deposits of the Huangliu Formation in Yinggehai Basin[J]. Earth Science Frontiers, 2015, 22(1): 21-34. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501004.htm