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Journal Article
Journal: AAPG Bulletin
Published: 01 February 2016
AAPG Bulletin (2016) 100 (2): 289–314.
...Changyu Teng; Fang Hao; Huayao Zou; Xinhuai Zhou; Changgui Xu ABSTRACT The Tan-Lu fault system in the central Liaodong Bay subbasin, Bohai Bay Basin, has complex structural characteristics, and its tectonism during the Cenozoic is an important factor in oil accumulation. Three-dimensional seismic...
FIGURES | View All (17)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2004
AAPG Bulletin (2004) 88 (1): 71–97.
...Li-Yuan Hsiao; Stephan A. Graham; Nat Tilander Abstract The Tan-Lu fault system in the Liaodong Bay, Bohai, offshore China, affords an exceptional opportunity to document the structural features of a major strike-slip fault using two- and three-dimensional seismic reflection data, as well...
FIGURES | View All (20)
Image
Seismic cross section of the Liaodong Bay subbasin of the Bohai Bay Basin. Note that the Liaozhong and Liaodong grabens are bounded by strike-slip faults in this section, and that the inversion structure occurs only within the synrift sequence, indicating that it belongs to the synrift basin inversion (see Fig. 1C for the location of this cross section; see Fig. DR1 [text footnote 1] for noninterpreted seismic section). TLFZ—Tan-Lu fault zone.
Published: 17 April 2020
Figure 3. Seismic cross section of the Liaodong Bay subbasin of the Bohai Bay Basin. Note that the Liaozhong and Liaodong grabens are bounded by strike-slip faults in this section, and that the inversion structure occurs only within the synrift sequence, indicating that it belongs to the synrift
Image
Interpreted seismic sections through the eastern part of the Liaodong Bay subbasin (northern segment) showing intrabasinal structural deformation (see Fig. 1C for the location of these cross sections; see Fig. DR2 [text footnote 1] for noninterpreted seismic sections). TLFZ—Tan-Lu fault zone.
Published: 17 April 2020
Figure 4. Interpreted seismic sections through the eastern part of the Liaodong Bay subbasin (northern segment) showing intrabasinal structural deformation (see Fig. 1C for the location of these cross sections; see Fig. DR2 [text footnote 1 ] for noninterpreted seismic sections). TLFZ—Tan-Lu
Image
Interpreted seismic sections through the eastern part of the Liaodong Bay subbasin (southern segment) showing intrabasinal structural deformation (see Fig. 1C for the location of these cross-sections; see Fig. DR3 [text footnote 1] for noninterpreted seismic sections). TLFZ—Tan-Lu fault zone.
Published: 17 April 2020
Figure 5. Interpreted seismic sections through the eastern part of the Liaodong Bay subbasin (southern segment) showing intrabasinal structural deformation (see Fig. 1C for the location of these cross-sections; see Fig. DR3 [text footnote 1 ] for noninterpreted seismic sections). TLFZ—Tan-Lu
Image
Geological section showing the structural framework of the Liaodong Bay subbasin. The LZ and LD2 faults are two branches of the Tan-Lu fault. The vertical exaggeration is 2. See Figure 1B, C for location.
Published: 01 February 2016
Figure 3. Geological section showing the structural framework of the Liaodong Bay subbasin. The LZ and LD2 faults are two branches of the Tan-Lu fault. The vertical exaggeration is 2. See Figure 1B, C for location.
Image
Interpreted seismic cross sections across the LZ fault in the Liaodong Bay subbasin. E2s3 (the third member of the Shahejie Formation), which occurs in individual cross sections, is treated as a marker bed to demonstrate the deformation of the strata. The section has no vertical exaggeration. See Figure 1C for location. RS = residual strata that were originally in the Liaodongnan depression and were formed by the strike-slip tectonism and the late Oligocene erosional truncation; TWT = two-way traveltime.
Published: 01 February 2016
Figure 7. Interpreted seismic cross sections across the LZ fault in the Liaodong Bay subbasin. E 2 s 3 (the third member of the Shahejie Formation), which occurs in individual cross sections, is treated as a marker bed to demonstrate the deformation of the strata. The section has no vertical
Image
Structural profiles with oil pool distribution across the Liaodong Bay subbasin. Note the variation in migration directions among the four profiles. See Figures 1C, 4B, 5B, 6B, and 14 for locations. E1-2k = Kongdian Formation; E2s = Shahejie Formation; E3d = Dongying Formation; N1g = Guantao Formation; N1-2m = Minghuazhen Formation; Qp = Pingyuan Formation.
Published: 01 February 2016
Figure 15. Structural profiles with oil pool distribution across the Liaodong Bay subbasin. Note the variation in migration directions among the four profiles. See Figures 1C , 4B , 5B , 6B , and 14 for locations. E 1-2 k = Kongdian Formation; E 2 s = Shahejie Formation; E 3 d = Dongying
Image
Map of the tectonic framework of the Tan-Lu fault system and Liaodong Bay, Bohai, offshore China. Seismic profiles ST, ER, A, B, CS/CN, PU, PA, and D are shown in Figures 7, 6, 8, 9, 11, 14, 15, and 10, respectively. See Figure 1 for location.
Published: 01 January 2004
Figure 4 Map of the tectonic framework of the Tan-Lu fault system and Liaodong Bay, Bohai, offshore China. Seismic profiles ST, ER, A, B, CS/CN, PU, PA, and D are shown in Figures 7 , 6 , 8 , 9 , 11 , 14 , 15 , and 10 , respectively. See Figure 1 for location.
Image
Paleogene tectonic evolution of the Tan-Lu fault and enclosing Liaodong Bay rift basin.
Published: 01 January 2004
Figure 16 Paleogene tectonic evolution of the Tan-Lu fault and enclosing Liaodong Bay rift basin.
Journal Article
Journal: GSA Bulletin
Published: 17 April 2020
GSA Bulletin (2020) 132 (11-12): 2572–2586.
...Figure 3. Seismic cross section of the Liaodong Bay subbasin of the Bohai Bay Basin. Note that the Liaozhong and Liaodong grabens are bounded by strike-slip faults in this section, and that the inversion structure occurs only within the synrift sequence, indicating that it belongs to the synrift...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2014
AAPG Bulletin (2014) 98 (10): 2109–2129.
... in lacustrine basins. An integration of geological, geophysical, and geochemical analysis is employed to investigate the origin of crude oil, the carrier-bed architecture, and migration pathways from source to trap in the JX1-1 oil field, Liaodong Bay subbasin, Bohai Bay Basin. Detailed geochemical studies...
FIGURES | View All (14)
Image
(A) Regional location of the Tan-Lu fault zone and the Bohai Bay Basin in eastern China (modified from Huang et al., 2016). (B) Simplified structure of the Cenozoic Bohai Bay Basin. (C) Simplified structure of the Liaodong Bay subbasin. Note that the Liaodong Bay subbasin is the offshore portion of the Liaohe subbasin within the Bohai Bay Basin. TLFZ—Tan-Lu fault zone.
Published: 17 April 2020
Figure 1. (A) Regional location of the Tan-Lu fault zone and the Bohai Bay Basin in eastern China (modified from Huang et al., 2016 ). (B) Simplified structure of the Cenozoic Bohai Bay Basin. (C) Simplified structure of the Liaodong Bay subbasin. Note that the Liaodong Bay subbasin
Image
Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence of the Liaodong Bay Subbasin. (B) aa′ profile across the JZ27-6-1 and JZ21-1-1 wells in the northern Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of this cross section. (C) bb′ profile across the JX1-1-1–JZ31-1-1–JZ31-2-1 wells in the central Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of the cross section. (D) Distribution of predicted and drilled turbidite traps and traps associated with truncation in the SEd3 sequence of the Liaozhong depression, Liaodong Bay Subbasin, which shows that the distribution of the stratigraphic traps is related to the strike-slip fault. See the dashed rectangle in panel A of this figure for the location of this area. The sequence interpretation, depositional system mapping, and turbidite prediction were based on the core- and well-log data of 116 wells, two-dimensional seismic data covering the whole Liaodong Bay Subbasin, and three-dimensional seismic data in the northern, central, and southern areas of the Liaozhong depression. The several wells labeled on the maps are part of key exploration wells shown for location reference.
Published: 01 September 2013
Figure 11 Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence
Image
Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence of the Liaodong Bay Subbasin. (B) aa′ profile across the JZ27-6-1 and JZ21-1-1 wells in the northern Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of this cross section. (C) bb′ profile across the JX1-1-1–JZ31-1-1–JZ31-2-1 wells in the central Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of the cross section. (D) Distribution of predicted and drilled turbidite traps and traps associated with truncation in the SEd3 sequence of the Liaozhong depression, Liaodong Bay Subbasin, which shows that the distribution of the stratigraphic traps is related to the strike-slip fault. See the dashed rectangle in panel A of this figure for the location of this area. The sequence interpretation, depositional system mapping, and turbidite prediction were based on the core- and well-log data of 116 wells, two-dimensional seismic data covering the whole Liaodong Bay Subbasin, and three-dimensional seismic data in the northern, central, and southern areas of the Liaozhong depression. The several wells labeled on the maps are part of key exploration wells shown for location reference.
Published: 01 September 2013
Figure 11 Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence
Image
Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence of the Liaodong Bay Subbasin. (B) aa′ profile across the JZ27-6-1 and JZ21-1-1 wells in the northern Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of this cross section. (C) bb′ profile across the JX1-1-1–JZ31-1-1–JZ31-2-1 wells in the central Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of the cross section. (D) Distribution of predicted and drilled turbidite traps and traps associated with truncation in the SEd3 sequence of the Liaozhong depression, Liaodong Bay Subbasin, which shows that the distribution of the stratigraphic traps is related to the strike-slip fault. See the dashed rectangle in panel A of this figure for the location of this area. The sequence interpretation, depositional system mapping, and turbidite prediction were based on the core- and well-log data of 116 wells, two-dimensional seismic data covering the whole Liaodong Bay Subbasin, and three-dimensional seismic data in the northern, central, and southern areas of the Liaozhong depression. The several wells labeled on the maps are part of key exploration wells shown for location reference.
Published: 01 September 2013
Figure 11 Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence
Image
Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence of the Liaodong Bay Subbasin. (B) aa′ profile across the JZ27-6-1 and JZ21-1-1 wells in the northern Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of this cross section. (C) bb′ profile across the JX1-1-1–JZ31-1-1–JZ31-2-1 wells in the central Liaozhong depression, showing the sand-body distribution within the sequence-stratigraphic framework. See panel A in this figure for the location of the cross section. (D) Distribution of predicted and drilled turbidite traps and traps associated with truncation in the SEd3 sequence of the Liaozhong depression, Liaodong Bay Subbasin, which shows that the distribution of the stratigraphic traps is related to the strike-slip fault. See the dashed rectangle in panel A of this figure for the location of this area. The sequence interpretation, depositional system mapping, and turbidite prediction were based on the core- and well-log data of 116 wells, two-dimensional seismic data covering the whole Liaodong Bay Subbasin, and three-dimensional seismic data in the northern, central, and southern areas of the Liaozhong depression. The several wells labeled on the maps are part of key exploration wells shown for location reference.
Published: 01 September 2013
Figure 11 Distribution of sand bodies within the sequence-stratigraphic framework of the Oligocene Dongying Formation in the Liaozhong depression of the Liaodong Bay Subbasin. (A) Sedimentary systems distribution in the SEd3 (third member of the Dongying Formation, or Dongying 3) sequence
Image
Map view of the Cenozoic tectonic evolution of the Tan-Lu fault system in the central Liaodong Bay subbasin. (A) From the Paleocene to the late Eocene, the Tan-Lu fault system underwent northwest–southeast extension. (B) From the Oligocene to the present, the regional extension continued, with right-lateral strike-slip tectonism dominant. Note the tectonic maximum stress direction through time in the Liaodong Bay subbasin. The contraction component produced by strike-slip was manifested as an anticline extending along the LZ fault, and it also induced extensional faulting in the shallow strata. See text for further discussion.
Published: 01 February 2016
Figure 12. Map view of the Cenozoic tectonic evolution of the Tan-Lu fault system in the central Liaodong Bay subbasin. (A) From the Paleocene to the late Eocene, the Tan-Lu fault system underwent northwest–southeast extension. (B) From the Oligocene to the present, the regional extension
Series: AAPG Memoir
Published: 01 January 1992
DOI: 10.1306/M54555C28
EISBN: 9781629811086
... Abstract The Suizhong 36-1 oil field was discovered by Bohai Oil Corporation, a subsidiary of CNOOC, in 1987 in the Bohai Gulf, Liaodong Bay. The structure consists of Oligocene fluviodeltaic and lacustrine sandstones that contain heavy oil in a combination structural-stratigraphic trap...
Image
(A) Sub-basins of the Bohai Bay Basin (modified from Hao et al. 2009a). (B) Distribution of sags and uplifts and main oil fields in the Liaodong Bay sub-basin. Maps created with GeoEast. [Colour online.]
Published: 31 March 2020
Fig. 1. (A) Sub-basins of the Bohai Bay Basin (modified from Hao et al. 2009 a ). (B) Distribution of sags and uplifts and main oil fields in the Liaodong Bay sub-basin. Maps created with GeoEast. [Colour online.]