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Enping Formation
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Journal Article
Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 July 2018
AAPG Bulletin (2018) 102 (7): 1323–1342.
...Junwen Peng; Xiongqi Pang; Hesheng Shi; Huijie Peng; Shuang Xiao ABSTRACT Upper Eocene Enping Formation mudstones in the Pearl River Mouth Basin, South China Sea, which formed during a lake-flooding event, are one of the most important sets of cap rocks in the basin. However, the generation...
Image
Schematic and conceptual formation model of Enping Formation source rocks i...
in Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 July 2018
Figure 16. Schematic and conceptual formation model of Enping Formation source rocks in the Huilu area, Pearl River Mouth Basin.
Image
Thickness distribution of Enping Formation source rocks in the Huilu area, ...
in Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 July 2018
Figure 15. Thickness distribution of Enping Formation source rocks in the Huilu area, Pearl River Mouth Basin (contour values in meters; modified from Peng et al., 2016 ). HZ = Huizhou; LF = Lufeng; XJ = Xijiang.
Image
Crossplot of T max versus hydrogen index of Enping Formation mudstone in...
in Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 July 2018
Figure 8. Crossplot of T max versus hydrogen index of Enping Formation mudstone in Huilu area, northern Pearl River Mouth Basin. Template modified from Espitalié (1985). HC = hydrocarbon; HZ = Huizhou; I = type I kerogen; II = type II kerogen; III = type III kerogen; LF = Lufeng; R o
Image
Organic maceral characteristics of Enping Formation mudstones in the northe...
in Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 July 2018
Figure 9. Organic maceral characteristics of Enping Formation mudstones in the northern Pearl River Mouth Basin (data from Zhu et al., 2007 ). Note that wells Huizhou (HZ) 8, HZ 23, and Xijiang (XJ) 24 are located in Huilu area ( Figure 1 ), whereas wells XJ 33 and Panyu (PY) 33 are located
Image
Gas and mass chromatograms of Enping Formation (E 2 e) mudstones from the H...
in Hydrocarbon-generation potential of upper Eocene Enping Formation mudstones in the Huilu area, northern Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 July 2018
Figure 11. Gas and mass chromatograms of Enping Formation (E 2 e) mudstones from the Huilu area: (A), (D), (G), and (J) show distribution characteristics of tricyclic terpanes (mass-to-charge ratio [ m/z ] 191); (B), (E), (H), and (K) show distribution characteristics of steranes ( m/z 217); (C
Image
—The dicardarane of oil and source rock of the Enping Formation in the Wenc...
in Petroleum Systems of the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 June 1999
Figure 15 —The dicardarane of oil and source rock of the Enping Formation in the Wenchang A sag (from Gong et al., 1997 ).
Image
—Isopach map of the Enping Formation in the Zhu III subbasin.
in Petroleum Systems of the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 June 1999
Figure 13 —Isopach map of the Enping Formation in the Zhu III subbasin.
Image
—Organic matter maturity of the Enping Formation in the Wenchang A sag, Zhu...
in Petroleum Systems of the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 June 1999
Figure 16 —Organic matter maturity of the Enping Formation in the Wenchang A sag, Zhu III subbasin.
Image
—Elemental composition of kerogens of the Enping Formation in the Wenchang ...
in Petroleum Systems of the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea
> AAPG Bulletin
Published: 01 June 1999
Figure 14 —Elemental composition of kerogens of the Enping Formation in the Wenchang A sag, Zhu III subbasin.
Journal Article
Geochemical characteristics, origins, and model of lacustrine source rocks in the Zhu 1 depression, eastern Pearl River Mouth Basin, South China Sea
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 September 2017
AAPG Bulletin (2017) 101 (9): 1543–1564.
..., is characterized by two thick, Paleogene, organic-rich synrift units, the Wenchang and Enping Formations. The integration of bulk geochemical and biomarker data with tectonic and sedimentary information provides the basis for a comprehensive assessment of the environmental and ecological changes through geologic...
Journal Article
Geochemical characteristics and analysis of crude-oil source in the deep-water area of the Baiyun Sag, South China Sea
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2018
Russ. Geol. Geophys. (2018) 59 (5): 499–511.
.... Crude oil in the northern area of the Baiyun Sag is more mature than samples in the eastern part of the sag. Despite limited source rock data, we were able to conclude that the crude oil samples were derived mainly from the Enping Formation; other potential source rocks of the Wenchang and Zhuhai...
Image
(A) Variation of methane δ 13 C versus ethane δ 13 C for fluid inclusion ga...
in Evidence for deeply buried, oil-prone source rocks in the Baiyun depression, Pearl River Mouth Basin, northern South China Sea
> AAPG Bulletin
Published: 15 April 2021
, Qiongdongnan Basin (QDN), are from Hao et al. (1998 , 2000) . Coal-type gases from the Middle–Lower Jurassic coal measures in the Tarim, Junggar, and Turpan–Hami Basins and from the Upper Triassic Xujiahe Formation coal measure in the Sichuan Basin are from Dai et al. (2014) . (B) The mixing of the Enping
Journal Article
Evidence for deeply buried, oil-prone source rocks in the Baiyun depression, Pearl River Mouth Basin, northern South China Sea
Hongwei Ping, Honghan Chen, Puqiang Zhai, Junzhang Zhu, Wanlin Xiong, Lingtao Kong, Se Gong, Tania J. Vergara, Simon C. George
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 15 April 2021
AAPG Bulletin (2021) 105 (4): 749–783.
..., Qiongdongnan Basin (QDN), are from Hao et al. (1998 , 2000) . Coal-type gases from the Middle–Lower Jurassic coal measures in the Tarim, Junggar, and Turpan–Hami Basins and from the Upper Triassic Xujiahe Formation coal measure in the Sichuan Basin are from Dai et al. (2014) . (B) The mixing of the Enping...
Journal Article
Geochemistry, origin, and deep-water exploration potential of natural gases in the Pearl River Mouth and Qiongdongnan basins, South China Sea
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 June 2009
AAPG Bulletin (2009) 93 (6): 741–761.
.... In contrast, the gases from the PRM basin contain lower amounts of benzene and toluene and lighter δ 13 C 2 values (−24 to −34‰). Widely variable concentrations of bicadinane and oleanane were identified from the associated condensates, which can be mostly correlated with the lower Oligocene Enping Formation...
Image
Activation energy distributions for four source rock types determined by an...
in Evidence for deeply buried, oil-prone source rocks in the Baiyun depression, Pearl River Mouth Basin, northern South China Sea
> AAPG Bulletin
Published: 15 April 2021
source rock from well PY5-8-1 (oil-prone type II kerogen), which was used to model the hydrocarbon generation history of the semideep-water and deep-water lacustrine facies source rocks in the Wenchang Formation in the Baiyun depression. (B) Enping Formation source rock from well HZ8-1-1 (gas-prone type
Journal Article
Origin, source, mixing, and thermal maturity of natural gases in the Panyu lower uplift and the Baiyun depression, Pearl River Mouth Basin, northern South China Sea
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 November 2018
AAPG Bulletin (2018) 102 (11): 2171–2200.
... the heavy hydrocarbon gases (propane, butanes, and pentanes) are derived from both the Wenchang and Enping (type III kerogen) Formations, based on an integrated comparison of carbon isotopic compositions of the natural gases, typical type I/II and type III kerogen-derived gases, and the Enping and Wenchang...
Image
Surface distribution of oil sources in the Baiyun Sag. I, organic matter (O...
in Geochemical characteristics and analysis of crude-oil source in the deep-water area of the Baiyun Sag, South China Sea
> Russian Geology and Geophysics
Published: 01 May 2018
Fig. 13. Surface distribution of oil sources in the Baiyun Sag. I, organic matter (OM) derived from the Enping Formation, primarily; II, OM derived from the Enping and Wenchang Formations; III, OM derived from the Wenchang Formation, primarily; IV, OM derived from the Enping and Zhuhai Formations
Image
GC-MS TIC, m / z 191 and m / z 217 traces of five oil samples represent...
in Geochemical characteristics and analysis of crude-oil source in the deep-water area of the Baiyun Sag, South China Sea
> Russian Geology and Geophysics
Published: 01 May 2018
Fig. 12. GC-MS TIC, m / z 191 and m / z 217 traces of five oil samples representing different sources. S1-EP, single source from the Enping Formation; S1-WC, single source from the Wenchang Formation; M1, mixed sources from the Enping and Wenchang Formation; M2, mixed sources from the Enping
Journal Article
Petroleum Systems of the Zhu III Subbasin, Pearl River Mouth Basin, South China Sea
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 June 1999
AAPG Bulletin (1999) 83 (6): 990–1003.
...Figure 15 —The dicardarane of oil and source rock of the Enping Formation in the Wenchang A sag (from Gong et al., 1997 ). ...
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