Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin

LI Cheng-hai; WANG Jia-hao; LIU Bao-jun; SU Ao; XU Dong-hao; LUO Quan-yuan; LIU Shan; MU Chuan

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Article Navigation > Acta Sedimentologica Sinica > 2014 > 32(6): 1162-1170

LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.

Citation:

LI Cheng-hai, WANG Jia-hao, LIU Bao-jun, SU Ao, XU Dong-hao, LUO Quan-yuan, LIU Shan, MU Chuan. Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1162-1170.

Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin

1.
School of Earth Resources China University of Geosciences, Wuhan 430074;
2.
Geophysical Exploration Research Institute of PetroChina Huabei Oilfield Company, Renqiu, Hebei 062552;
3.
Shenzhen Branch of CNOOC, Guangzhou 510420;
4.
Geophysical Research Institute, BGP, CNPC, Zhuozhou, Hebei 072750

Received Date: 2013-10-08
Rev Recd Date: 2013-12-16
Publish Date: 2014-12-10

Abstract

Based on the drilling and seismic data in Baiyun Depression, development and evolution of sedimentary facies are comprehensively analyzed in the Wenchang and Enping Formation, Baiyun Depression of Pearl River Mouth Basin. Through the limited well data, three sedimentary facies, delta facies, fan-delta facies and lacustrine facies, are identified in Baiyun Depression; Logging curve of delta facies shows an inverse cycle, but subset normal cycle in some parts; Logging curve(gamma-ray) of fan-delta curve shows an inverse cycle and subset normal cycle overall; Lacustrine facies mainly are mudstone deposition, partly mingled with sand bar or carbonate beach bar. Nine types of seismic facies are identified in Baiyun Dpression. The research shows that the continuinous subsidence of the basin causes the long time of the deep lacustrine facies development and the formation of the thick-layer resource rock. Influenced by lower Panyu Uplift, a delta facies developed in the northern gentle slope in Baiyun Depression, fan-delta facies developed from southwestern to southern abrupt slope. And the development of partial delta facies has a succession.
- Pearl River Mouth Basin,
- Baiyun depression,
- Paleogene,
- seismic facies,
- sedimentary facies

References

[1]	庞雄,陈长民,朱明,等. 南海北部陆坡白云深水区油气成藏条件探讨[J]. 中国海上油气,2006,18(3):145-149 [Pang Xiong, Chen Changmin, Zhu Ming, et al. A discussion about hydrocarbon accumulation conditions in Baiyun deep-water area, the northern continental slope, South China Sea [J]. China Offshore Oil and Gas, 2006, 18(3): 145-149]
[2]	柳保军,庞雄,颜承志,等. 珠江口盆地白云深水区沉积充填演化及控制因素分析[J]. 中国海上油气,2011,23(1):19-25 [Liu Baojun, Pang Xiong, Yan Chengzhi, et al. An analysis of deposition evolution and its controls in Baiyun deep-water area, Pearl River Mouth basin [J]. China Offshore Oil and Gas, 2011, 23(1): 19-25]
[3]	庞雄,陈长民,彭大钧,等. 南海珠江深水扇系统及油气[M]. 北京:科学出版社,2007:1-303 [Pang Xiong, Chen Changmin, Peng Dajun, et al. The Pearl River Deep-water Fan System or Petroleum in South China Sea [M]. Beijing: Science Press, 2007: 1-303]
[4]	彭大钧,陈长民,朱明,等. 南海珠江口盆地深水扇系统的发现[J]. 石油学报,2004,25(5):17-23 [Peng Dajun, Chen Changmin, Pang Xiong, et al. Discovery of deep-water fan system in the South China Sea [J]. Acta Petrolei Sinica, 2004, 25(5): 17-23]
[5]	彭大钧,庞雄,陈长民,等. 南海珠江深水扇系统的形成特征与控制因素[J]. 沉积学报,2006,24(1):10-17 [Peng Dajun, Pang Xiong, Chen Changmin, et al. The characteristics and controlling factors for the formation of deep-water fan system in South China Sea [J]. Acta Sedimentologica Sinica, 2006, 24(1): 10-17]
[6]	庞雄,陈长民,施和生,等. 相对海平面变化与南海珠江深水扇系统的响应[J]. 地学前缘,2005,12(3):167-177 [Pang Xiong, Chen Changmin, Shi Hesheng, et al. Response between relative sea-level change and the Pearl River deepwater fan system in the South China Sea [J]. Earth Science Frontiers, 2005, 12(3): 167-177]
[7]	庞雄,申俊,袁立忠,等. 南海珠江深水扇系统及其油气勘探前景[J]. 石油学报,2006,27(3):11-15 [Pang Xiong, Shen Jun, Yuan Lizhong, et al. Petroleum prospect in deep-water fan system of the Pearl River in the South China Sea [J]. Acta Petrolei Sinica, 2006, 27(3): 11-15]
[8]	庞雄,陈长民,彭大钧,等. 南海珠江深水扇系统的层序地层学研究[J]. 地学前缘,2007,14(1):220-229 [Pang Xiong, Chen Changmin, Peng Dajun, et al. Sequence stratigraphy of Pearl River deep-water fan systems of the South China Sea [J]. Earth Science Frontiers, 2007, 14(1): 220-229]
[9]	彭大钧,庞雄,陈长民,等. 从浅水陆架走向深水陆坡—南海深水扇的研究[J]. 沉积学报,2005,23(1):1-11 [Peng Dajun, Pang Xiong, Chen Changmin, et al. From shallow-water shelf to deep-water slope—The research of deep-water fan systems in South China sea [J]. Acta Sedimentologica Sinica, 2005, 23(1): 1-11]
[10]	柳保军,申俊,庞雄,等. 珠江口盆地白云凹陷珠海组浅海三角洲沉积特征[J]. 石油学报,2007,28(2):49-56 [Liu Baojun, Shen Jun, Pang Xiong, et al. Characteristics of continental delta in Zhuhai Formation of Baiyun depression in Pearl River Mouth Basin[J]. Acta Petrolei Sinica, 2007, 28(2): 49-56]
[11]	陈长民,施和生,许仕策,等. 珠江口盆地(东部)第三系油气藏形成条件[M]. 北京:科学出版社,2003:1-30 [Chen Changmin, Shi Hesheng, Xu Shice, et al. Original Condition of the Tertiary Oil and Gas Accumulation, Pearl River Mouth Basin [M]. Beijing: Science Press, 2003: 1-30]
[12]	代一丁,庞雄. 珠江口盆地珠二凹陷石油地质特征[J]. 中国海上油气:地质,1999,12(3):169-180 [Dai Yiding, Pang Xiong. Petroleum geological characteristic of Zhu Ⅱ depression, Pearl River Mouth Basin [J]. China offshore Oil and Gas: Geology, 1999, 12(3): 169-180]
[13]	米立军,张功成,沈怀磊,等. 珠江口盆地深水区白云凹陷始新统—下渐新统沉积特征[J]. 石油学报,2008,29(1):29-34[Mi Lijun, Zhang Gongcheng, Shen Huailei, et al. Eocene-Lower Oligocene sedimentation characteristics of Baiyun sag in the deep water area of Pearl River Mouth Basin [J]. Acta Petrolei Sinica, 2008, 29(1): 29-34]
[14]	连世勇,何敏,庞雄,等. 珠江口盆地深水区白云凹陷始新世洼陷结构研究[J]. 石油学报,2007,28(3):13-16[Lian Shiyong, He Min, Pang Xiong, et al. Research on Eocene structure of Baiyun sag in deep-water area of Pearl River Mouth Basin [J]. Acta Petrolei Sinica, 2007, 28(3): 13-16]
[15]	孙珍,庞雄,钟志洪,等. 珠江口盆地白云凹陷新生代构造演化动力学[J]. 地学前缘,2005,12 (4):489-498 [Sun Zhen, Pang Xiong, Zhong Zhihong, et al. Dynamics of Tertiary tectonic evolution of the Baiyun sag in the Pearl River Mouth Basin [J]. Earth Science Frontiers, 2005, 12(4): 489-498]
[16]	庞雄,陈长民,彭大钧,等. 南海北部白云深水区之基础地质[J]. 中国海上油气,2008,20(4):215-222 [Pang Xiong, Chen Changmin, Peng Dajun, et al. Basic geology of Baiyun deep-water area in the northern South China Sea [J]. China Offshore Oil and Gas, 2008, 20(4): 215-222]
[17]	张万选,张厚福,曾洪流. 陆相地震地层学[M]. 北京:石油大学出版社,1993:1-43 [Zhang Wanxuan, Zhang Houfu, Zeng Hongliu. Continental Seismic Stratigraphy[M]. Beijing: Petroleum University Press, 1993: 1-43]
[18]	鲜本忠,姜在兴. 断陷湖盆中下切谷的形成机理初探—以泌阳凹陷为例[C]//全国沉积学大会摘要论文集,2001:122-123 [Xian Benzhong, Jang Zaixing. The preliminary research of the development of the incised valley in lacustrine fault basins — takes Miyang depression as an Example[C]//Abstract of Sedimentological Congress in China, 2001: 122-123]

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin

1. School of Earth Resources China University of Geosciences, Wuhan 430074;

2. Geophysical Exploration Research Institute of PetroChina Huabei Oilfield Company, Renqiu, Hebei 062552;

3. Shenzhen Branch of CNOOC, Guangzhou 510420;

4. Geophysical Research Institute, BGP, CNPC, Zhuozhou, Hebei 072750

Received Date: 2013-10-08

Rev Recd Date: 2013-12-16

Publish Date: 2014-12-10

Key words:

Abstract: Based on the drilling and seismic data in Baiyun Depression, development and evolution of sedimentary facies are comprehensively analyzed in the Wenchang and Enping Formation, Baiyun Depression of Pearl River Mouth Basin. Through the limited well data, three sedimentary facies, delta facies, fan-delta facies and lacustrine facies, are identified in Baiyun Depression; Logging curve of delta facies shows an inverse cycle, but subset normal cycle in some parts; Logging curve(gamma-ray) of fan-delta curve shows an inverse cycle and subset normal cycle overall; Lacustrine facies mainly are mudstone deposition, partly mingled with sand bar or carbonate beach bar. Nine types of seismic facies are identified in Baiyun Dpression. The research shows that the continuinous subsidence of the basin causes the long time of the deep lacustrine facies development and the formation of the thick-layer resource rock. Influenced by lower Panyu Uplift, a delta facies developed in the northern gentle slope in Baiyun Depression, fan-delta facies developed from southwestern to southern abrupt slope. And the development of partial delta facies has a succession.

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Reference (18)

[1]	庞雄,陈长民,朱明,等. 南海北部陆坡白云深水区油气成藏条件探讨[J]. 中国海上油气,2006,18(3):145-149 [Pang Xiong, Chen Changmin, Zhu Ming, et al. A discussion about hydrocarbon accumulation conditions in Baiyun deep-water area, the northern continental slope, South China Sea [J]. China Offshore Oil and Gas, 2006, 18(3): 145-149]
[2]	柳保军,庞雄,颜承志,等. 珠江口盆地白云深水区沉积充填演化及控制因素分析[J]. 中国海上油气,2011,23(1):19-25 [Liu Baojun, Pang Xiong, Yan Chengzhi, et al. An analysis of deposition evolution and its controls in Baiyun deep-water area, Pearl River Mouth basin [J]. China Offshore Oil and Gas, 2011, 23(1): 19-25]
[3]	庞雄,陈长民,彭大钧,等. 南海珠江深水扇系统及油气[M]. 北京:科学出版社,2007:1-303 [Pang Xiong, Chen Changmin, Peng Dajun, et al. The Pearl River Deep-water Fan System or Petroleum in South China Sea [M]. Beijing: Science Press, 2007: 1-303]
[4]	彭大钧,陈长民,朱明,等. 南海珠江口盆地深水扇系统的发现[J]. 石油学报,2004,25(5):17-23 [Peng Dajun, Chen Changmin, Pang Xiong, et al. Discovery of deep-water fan system in the South China Sea [J]. Acta Petrolei Sinica, 2004, 25(5): 17-23]
[5]	彭大钧,庞雄,陈长民,等. 南海珠江深水扇系统的形成特征与控制因素[J]. 沉积学报,2006,24(1):10-17 [Peng Dajun, Pang Xiong, Chen Changmin, et al. The characteristics and controlling factors for the formation of deep-water fan system in South China Sea [J]. Acta Sedimentologica Sinica, 2006, 24(1): 10-17]
[6]	庞雄,陈长民,施和生,等. 相对海平面变化与南海珠江深水扇系统的响应[J]. 地学前缘,2005,12(3):167-177 [Pang Xiong, Chen Changmin, Shi Hesheng, et al. Response between relative sea-level change and the Pearl River deepwater fan system in the South China Sea [J]. Earth Science Frontiers, 2005, 12(3): 167-177]
[7]	庞雄,申俊,袁立忠,等. 南海珠江深水扇系统及其油气勘探前景[J]. 石油学报,2006,27(3):11-15 [Pang Xiong, Shen Jun, Yuan Lizhong, et al. Petroleum prospect in deep-water fan system of the Pearl River in the South China Sea [J]. Acta Petrolei Sinica, 2006, 27(3): 11-15]
[8]	庞雄,陈长民,彭大钧,等. 南海珠江深水扇系统的层序地层学研究[J]. 地学前缘,2007,14(1):220-229 [Pang Xiong, Chen Changmin, Peng Dajun, et al. Sequence stratigraphy of Pearl River deep-water fan systems of the South China Sea [J]. Earth Science Frontiers, 2007, 14(1): 220-229]
[9]	彭大钧,庞雄,陈长民,等. 从浅水陆架走向深水陆坡—南海深水扇的研究[J]. 沉积学报,2005,23(1):1-11 [Peng Dajun, Pang Xiong, Chen Changmin, et al. From shallow-water shelf to deep-water slope—The research of deep-water fan systems in South China sea [J]. Acta Sedimentologica Sinica, 2005, 23(1): 1-11]
[10]	柳保军,申俊,庞雄,等. 珠江口盆地白云凹陷珠海组浅海三角洲沉积特征[J]. 石油学报,2007,28(2):49-56 [Liu Baojun, Shen Jun, Pang Xiong, et al. Characteristics of continental delta in Zhuhai Formation of Baiyun depression in Pearl River Mouth Basin[J]. Acta Petrolei Sinica, 2007, 28(2): 49-56]
[11]	陈长民,施和生,许仕策,等. 珠江口盆地(东部)第三系油气藏形成条件[M]. 北京:科学出版社,2003:1-30 [Chen Changmin, Shi Hesheng, Xu Shice, et al. Original Condition of the Tertiary Oil and Gas Accumulation, Pearl River Mouth Basin [M]. Beijing: Science Press, 2003: 1-30]
[12]	代一丁,庞雄. 珠江口盆地珠二凹陷石油地质特征[J]. 中国海上油气:地质,1999,12(3):169-180 [Dai Yiding, Pang Xiong. Petroleum geological characteristic of Zhu Ⅱ depression, Pearl River Mouth Basin [J]. China offshore Oil and Gas: Geology, 1999, 12(3): 169-180]
[13]	米立军,张功成,沈怀磊,等. 珠江口盆地深水区白云凹陷始新统—下渐新统沉积特征[J]. 石油学报,2008,29(1):29-34[Mi Lijun, Zhang Gongcheng, Shen Huailei, et al. Eocene-Lower Oligocene sedimentation characteristics of Baiyun sag in the deep water area of Pearl River Mouth Basin [J]. Acta Petrolei Sinica, 2008, 29(1): 29-34]
[14]	连世勇,何敏,庞雄,等. 珠江口盆地深水区白云凹陷始新世洼陷结构研究[J]. 石油学报,2007,28(3):13-16[Lian Shiyong, He Min, Pang Xiong, et al. Research on Eocene structure of Baiyun sag in deep-water area of Pearl River Mouth Basin [J]. Acta Petrolei Sinica, 2007, 28(3): 13-16]
[15]	孙珍,庞雄,钟志洪,等. 珠江口盆地白云凹陷新生代构造演化动力学[J]. 地学前缘,2005,12 (4):489-498 [Sun Zhen, Pang Xiong, Zhong Zhihong, et al. Dynamics of Tertiary tectonic evolution of the Baiyun sag in the Pearl River Mouth Basin [J]. Earth Science Frontiers, 2005, 12(4): 489-498]
[16]	庞雄,陈长民,彭大钧,等. 南海北部白云深水区之基础地质[J]. 中国海上油气,2008,20(4):215-222 [Pang Xiong, Chen Changmin, Peng Dajun, et al. Basic geology of Baiyun deep-water area in the northern South China Sea [J]. China Offshore Oil and Gas, 2008, 20(4): 215-222]
[17]	张万选,张厚福,曾洪流. 陆相地震地层学[M]. 北京:石油大学出版社,1993:1-43 [Zhang Wanxuan, Zhang Houfu, Zeng Hongliu. Continental Seismic Stratigraphy[M]. Beijing: Petroleum University Press, 1993: 1-43]
[18]	鲜本忠,姜在兴. 断陷湖盆中下切谷的形成机理初探—以泌阳凹陷为例[C]//全国沉积学大会摘要论文集,2001:122-123 [Xian Benzhong, Jang Zaixing. The preliminary research of the development of the incised valley in lacustrine fault basins — takes Miyang depression as an Example[C]//Abstract of Sedimentological Congress in China, 2001: 122-123]

Types and Distribution of the Paleogene Sedimentary Facies in Baiyun Depression of Pearl River Mouth Basin

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通讯作者: 陈斌, bchen63@163.com

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