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Lingshui Formation

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Journal Article
Journal: Interpretation
Published: 14 May 2020
Interpretation (2020) 8 (3): SM53–SM64.
... have studied the main factors for the development of abnormally high porosity in the Lingshui Formation reservoir of the Yacheng area. We found the sandstones were mainly subarkose, arkose, and lithic arkose and were texturally and compositionally immature. The research suggested that the sandstones...
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Summary of sandstone lithofacies and pores in the <span class="search-highlight">Lingshui</span> <span class="search-highlight">Formation</span>.
Published: 14 May 2020
Table 1. Summary of sandstone lithofacies and pores in the Lingshui Formation.
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Rock composition data of the <span class="search-highlight">Lingshui</span> <span class="search-highlight">Formation</span> sandstones plotted in the t...
Published: 14 May 2020
Figure 2. Rock composition data of the Lingshui Formation sandstones plotted in the triangular chart (after Folk, 1974 ): 1, quartz arenite; 2, subarkose; 3, sublitharenite; 4, arkose; 5, lithic arkose; 6, feldspathic litharenite; 7, litharenite.
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(a) Percentage of pore types in the <span class="search-highlight">Lingshui</span> <span class="search-highlight">Formation</span> sandstones, (b) rela...
Published: 14 May 2020
Figure 6. (a) Percentage of pore types in the Lingshui Formation sandstones, (b) relationship between the different lithofacies and reservoir physical characteristics (porosity, abundance of feldspar, and secondary pores formed by FD) in the Lingshui Formation of the Ya’nan Sag.
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1998
AAPG Bulletin (1998) 82 (7): 1372–1384.
...Fang Hao; Sitian Li; Yongchuan Sun; Qiming Zhang ABSTRACT The Yacheng gas field is located in the footwall of the No. 1 fault, the boundary fault between the Yinggehai and Qiongdongnan basins. The main reservoir is the fan-delta sandstones in the Lingshui Formation. The seals are Meishan Formation...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1998
AAPG Bulletin (1998) 82 (5): 757–772.
... formed at 10.5 Ma, which was earlier than gas migration and accumulation. The Meishan Formation, with 7–10 MPa (1015–1450 psi) expelling pressure and 49–66 MPa (7105–9570 psi) overpressure combined, effectively seals YA13-1 gases. The reservoir of Lingshui Formation sands has average values of 14.9...
FIGURES | View All (15)
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Subsidence curve of sections ( a ) A–A′ and ( b ) B–B′ traversing the Lings...
Published: 25 March 2024
Fig. 8. Subsidence curve of sections ( a ) A–A′ and ( b ) B–B′ traversing the Lingshui and Baodao sub-basins, respectively (for location, see Fig. 1 ). E 2 , Eocene; E 3 y, Yacheng Formation; E 3 l, Lingshui Formation; N 1 s, Sanya Formation; N 1 m, Meishan Formation; N 1 h, Huangliu Formation
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Two-dimensional gas migration modeling results at present day along a trans...
Published: 01 June 2009
Figure 13 Two-dimensional gas migration modeling results at present day along a transect across the Lingshui Sag, showing possible sources and migration directions of petroleum. The location of the section is shown in Figure 1 . Q = Quaternary; YG = Yinggehai Formation; HL = Huangliu Formation
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Burial history curves at the depocenters of (a) the Baiyun Sag in the Pearl...
Published: 01 June 2009
Figure 10 Burial history curves at the depocenters of (a) the Baiyun Sag in the Pearl River Mouth (PRM) Basin and (b) the Lingshui Sag in the Qiongdongnan (QDN) Basin. R o = vitrinite reflectance; WC = Wenchang Formation; EP = Enping Formation; ZH = Zhuhai Formation; ZJ = Zhujiang Formation; HJ
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1998
AAPG Bulletin (1998) 82 (5A): 757–772.
... formed at 10.5 Ma, which was earlier than gas migration and accumulation. The Meishan Formation, with 7-10 MPa (1015-1450 psi) expelling pressure and 49-66 MPa (7105-9570 psi) overpressure combined, effectively seals YA13-1 gases. The reservoir of Lingshui Formation sands has average values of 14.9...
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Distribution of carbon and oxygen isotopic compositions of the carbonate ce...
Published: 14 May 2020
Figure 9. Distribution of carbon and oxygen isotopic compositions of the carbonate cements in the Lingshui Formation sandstones ( Yang et al., 2010 ).
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(a) Vertical distribution of core porosity, (b) vitrinite reflectance (    ...
Published: 14 May 2020
Figure 5. (a) Vertical distribution of core porosity, (b) vitrinite reflectance ( R o ), and (c) smectite content in the I/S of different sandstones in the Lingshui Formation of the Ya’nan Sag.
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(a) Bathymetric map showing the distribution of the sags in the Qiongdongna...
Published: 14 May 2020
Figure 1. (a) Bathymetric map showing the distribution of the sags in the Qiongdongnan basin and the locations of the utilized boreholes as well as the profile in (b) and (b) cross section of the Lingshui Formation in the Ya’nan Sag.
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—Cross sections showing the structural differences between (A) the Qiongdon...
Published: 01 July 1998
Figure 2 —Cross sections showing the structural differences between (A) the Qiongdongnan Basin and (B) the Yinggehai Basin. Y-L = Yacheng and Lingshui formations; M-S = Meishan and Sanya formations (after Hao et al., 1995).
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—(A) Cross section showing the rift structure of the Qiongdongnan Basin, an...
Published: 01 April 1995
Figure 3 —(A) Cross section showing the rift structure of the Qiongdongnan Basin, and (B) the shale diapir of the Yinggehai Basin (see Figure 2 for location). Y-L = Yacheng and Lingshui formations; M-S = Meishan and Sanya formations.
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A geological cross section of the BD19-2      CO  2      gas pool in the Qi...
Published: 01 July 2015
Figure 8 A geological cross section of the BD19-2 CO 2 gas pool in the Qiongdongnan basin illustrating the migration and accumulation of mantle-derived CO 2 gas. LS1, LS2, and LS3 = the upper, middle, and lower part of Lingshui Formation; YC = Yacheng Formation
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–Scatter plots of the (A) porosity of potassium feldspar and quartz overgro...
Published: 01 May 1998
Figure 9 –Scatter plots of the (A) porosity of potassium feldspar and quartz overgrowths and (B) permeability of potassium feldspar and quartz overgrowths for Lingshui Formation sandstones, YA13-1 area. Note that between 1 and 6% overgrowths improves reservoir quality because they occur
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—Simplified section across the No. 1 fault and the Yacheng gas field (see  ...
Published: 01 July 1998
Figure 4 —Simplified section across the No. 1 fault and the Yacheng gas field (see Figure 1 for location). E 3 L 2 , E 3 L 3 = the second and third members of the Lingshui Formation, respectively; N 1 S = Sanya formation; Ben = benzene; nC 6 , iC 6 , and cC 6 represent normal, branched
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—Structural hydrodynamic potential maps in E L3 . The gas migration trend i...
Published: 01 May 1993
is a structure map of the Oligocene Lingshui Formation lower member (E L3 ). (b) The V map is the water equipotential-surface map in E L3 . (c) The U map is the gas equipotential-surface map in E L3 . The maps were drawn by data derived from seismic logs.
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1993
AAPG Bulletin (1993) 77 (5): 888–895.
... is a structure map of the Oligocene Lingshui Formation lower member (E L3 ). (b) The V map is the water equipotential-surface map in E L3 . (c) The U map is the gas equipotential-surface map in E L3 . The maps were drawn by data derived from seismic logs. ...
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