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Tabei Uplift

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Journal Article
Journal: GSA Bulletin
Published: 15 May 2024
GSA Bulletin (2024) 136 (11-12): 4985–5008.
... and dissolution processes related to the proximity to regional paleoerosion surfaces (e.g., unconformities) in the northern part of the Tarim Basin. Figure 1. (A) Simplified tectonic map showing major strike-slip fault distributions in the Tabei Uplift and Shuntuo Low Uplift in the Tarim Basin, China...
FIGURES | View All (16)
Journal Article
Journal: GSA Bulletin
Published: 27 February 2024
GSA Bulletin (2024) 136 (9-10): 3810–3824.
... of hydrocarbon generation and expulsion in source rock via the integration of the fluorescence of oil inclusions, inclusion homogenization temperatures, and in situ U-Pb dating of calcite veins containing hydrocarbon inclusions. In the QT1 well area of the Tabei uplift belt, our reconstructed hydrocarbon...
FIGURES | View All (13)
Journal Article
Published: 01 July 2021
Russ. Geol. Geophys. (2021) 62 (07): 808–827.
...Q. Liu; H. Xu; Z. Lei; Z. Li; Y. Xiong; S. Li; B. Luo; D. Chen Abstract —The hydrocarbon formation mechanism and potential targets in clastic strata from the Tabei Uplift, Tarim Basin, are documented using the fault mesh petroleum plays theory, based on integrating seismic, well log, well core...
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Journal Article
Published: 01 February 2019
Russ. Geol. Geophys. (2019) 60 (2): 215–230.
...Zhicheng Lei; Huaimin Xu; Tongwen Jiang; Zhongchao Li; Jingwen Li; Weilu Li; Yunbin Xiong; Songze Li; Junwei Zhao Abstract —The Carboniferous Donghe sandstone reservoir is the most important target in the Tabei Uplift of the Tarim Basin, which contains a range of hydrocarbon types, including...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 December 2011
AAPG Bulletin (2011) 95 (12): 2061–2083.
...Hongliu Zeng; Robert Loucks; Xavier Janson; Guizhong Wang; Yiping Xia; Bingheng Yuan; Ligui Xu Abstract High-quality three-dimensional seismic data acquired in the central Tabei Uplift, Tarim Basin, western China, provide a rare opportunity to characterize in exceptional detail the three...
FIGURES | View All (18)
Journal Article
Journal: Geophysics
Published: 03 June 2011
Geophysics (2011) 76 (4): B127–B137.
...Hongliu Zeng; Guizhong Wang; Xavier Janson; Robert Loucks; Yiping Xia; Ligui Xu; Bingheng Yuan Abstract Anomalous seismic-amplitude bright spots are a common feature in deeply buried (5500 to 6500 m) Ordovician limestone strata in the Central Tabei Uplift area of the Tarim Basin in northwest China...
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Image
Stratigraphic column for the Tabei uplift, Tarim Basin, spanning from the Sinian (Precambrian) to the Triassic. Figure is modified after Lin et al. (2015), Hu et al. (2016), and Ge et al. (2020).
Published: 01 January 2025
Figure 2. Stratigraphic column for the Tabei uplift, Tarim Basin, spanning from the Sinian (Precambrian) to the Triassic. Figure is modified after Lin et al. (2015) , Hu et al. (2016) , and Ge et al. (2020) .
Image
Petroleum system event chart of the Tabei uplift (modified from Q. Li et al., 2010 and Yang et al., 2020b). Є = Cambrian; C = Carboniferous; D = Devonian; E-Q = Paleogene–Quaternary; J = Jurassic; K = Cretaceous; O = Ordovician; P = Permian; S = Silurian; T = Triassic.
Published: 01 July 2024
Figure 17. Petroleum system event chart of the Tabei uplift (modified from Q. Li et al., 2010 and Yang et al., 2020b ). Є = Cambrian; C = Carboniferous; D = Devonian; E-Q = Paleogene–Quaternary; J = Jurassic; K = Cretaceous; O = Ordovician; P = Permian; S = Silurian; T = Triassic.
Image
Cross section showing the structural framework of the Tabei uplift belt in the Tarim Basin, China. Section location in Figure 1B. (modified from Li et al., 2021b).
Published: 27 February 2024
Figure 2. Cross section showing the structural framework of the Tabei uplift belt in the Tarim Basin, China. Section location in Figure 1B . (modified from Li et al., 2021b ).
Image
Hand specimens from the Yuertusi Formation of the Tabei uplift belt, China (A1, B1, C1, D1), and photomicrographs under transmitted light (TL) (A2, B2, C2, D2) and cathodoluminescence (CL) microscopy (A3, B3, C3, D3) of parts of the samples used for measurements. (A1, A2, A3) Two fracture-filling calcite veins (QT1-stage I and QT1-stage II) from well QT1 at 5966.79 m. (B1, B2, B3) At a depth of 8644.25 m, two fracture-filling calcite veins (LT1-stage I and LT1-stage II) were observed in well LT1. (C1, C2, C3) At a depth of 8522.56 m in well LT3, there is a fracture-filling calcite vein referred to as LT3-stage I. (D1, D2, D3) In well LT3, fracture-filling calcite veins (referred to as LT3-stage II) were observed at a depth of 8523.22 m.
Published: 27 February 2024
Figure 4. Hand specimens from the Yuertusi Formation of the Tabei uplift belt, China (A1, B1, C1, D1), and photomicrographs under transmitted light (TL) (A2, B2, C2, D2) and cathodoluminescence (CL) microscopy (A3, B3, C3, D3) of parts of the samples used for measurements. (A1, A2, A3) Two
Image
Hydrocarbon generation history of the Tabei uplift (wells XH1, YQ6, TS2, QT1, and LT3). According to the findings of Zheng et al. (2022) and Li et al. (2022), the maturities of the wells at ca. 288–270 Ma are as follows: well YQ6 is 2.5 and 1.8, well TS2 is 2.1 and 0.9, and well XH1 is 1.3 and 0.4. At ca. 270–260 Ma, the maturities of the wells are 2.5 and 1.8 for well YQ6, 2.2 and 1.1 for well TS2, and 1.3 and 0.4 for well XH1. N-Q—Neogene–Quaternary; E—Paleogene; K—Cretaceous; J—Jurassic; T—Triassic; P—Permian; C—Carboniferous; D—Devonian; S—Silurian; O—Ordovician; Є—Cambrian; Z—Sinian.
Published: 27 February 2024
Figure 13. Hydrocarbon generation history of the Tabei uplift (wells XH1, YQ6, TS2, QT1, and LT3). According to the findings of Zheng et al. (2022) and Li et al. (2022) , the maturities of the wells at ca. 288–270 Ma are as follows: well YQ6 is 2.5 and 1.8, well TS2 is 2.1 and 0.9, and well
Image
(A) Map showing the location of the Tahe oil field in the Tabei uplift and outcrops in the Keping uplift, northern Tarim Basin. (B) Map of four outcrops in the Keping uplift, including the Penglaiba (PLB), Kepingshuinichang (KPSNC), Yangjikan (YJK) and Dabantage (DBTG) outcrops. (C) Map of the Tahe oil field in which the studied wells are marked with orange dots (modified from Wu et al., 2018a).
Published: 01 December 2022
Figure 1. (A) Map showing the location of the Tahe oil field in the Tabei uplift and outcrops in the Keping uplift, northern Tarim Basin. (B) Map of four outcrops in the Keping uplift, including the Penglaiba (PLB), Kepingshuinichang (KPSNC), Yangjikan (YJK) and Dabantage (DBTG) outcrops. (C) Map
Image
Tectonic locations of the Tarim Basin (a), Tabei Uplift (b) and Donghetang area (c), respectively; d, fault system and reservoir distribution of the Carboniferous Donghe sandstone in the Donghetang area; e, the well locations in the DH1 Oilfield.
Published: 01 February 2019
Fig. 1. Tectonic locations of the Tarim Basin ( a ), Tabei Uplift ( b ) and Donghetang area ( c ), respectively; d , fault system and reservoir distribution of the Carboniferous Donghe sandstone in the Donghetang area; e , the well locations in the DH1 Oilfield.
Image
The variation of C1/C2+ ratios of natural gases from Tabei uplift and Tazhong uplift. JLK = Jilake, JFQ = Jiefangqu, STM = Sangtamu, LN = Lunnan, DHT = Donghetang, TZ = Tazhong.
Published: 01 May 2000
Figure 6 The variation of C 1 /C 2+ ratios of natural gases from Tabei uplift and Tazhong uplift. JLK = Jilake, JFQ = Jiefangqu, STM = Sangtamu, LN = Lunnan, DHT = Donghetang, TZ = Tazhong.
Image
—Seismic reflection profile (line K-83-23) across the Tabei uplift. T8 = bottom reflector of the Tertiary, Tg = bottom reflector of the Mesozoic, Tg4 = bottom reflector of the upper Paleozoic, Tg8 = bottom reflector of the Sinian. Kz = Cenozoic, Mz = Mesozoic, Pz2 = Upper Paleozoic, Pz1 = Lower Paleozoic, Z = Sinian, Pt = Proterozoic, Ar = Archean.
Published: 11 October 1996
Figure 18 —Seismic reflection profile (line K-83-23) across the Tabei uplift. T8 = bottom reflector of the Tertiary, Tg = bottom reflector of the Mesozoic, Tg4 = bottom reflector of the upper Paleozoic, Tg8 = bottom reflector of the Sinian. Kz = Cenozoic, Mz = Mesozoic, Pz2 = Upper Paleozoic, Pz1
Image
(A) The Tarim Basin is situated in northwestern China. The inset shows the national border of China in the South China Sea. (B) Geological map showing the structural units within the Tarim Basin. The Tabei uplift is located in the northern part of the Tarim Basin. (C) Simplified map showing the structural unit of the Tabei uplift. The Tahe oil field is located in the Akekule arch within the Tabei uplift. Several giant Paleozoic oil fields are found in the vicinity of the Tahe oil field, including the Halahatang oil field, Shunbei oil field, and Tuoputai oil field. (D) Map showing the sampling sites in this study.
Published: 01 August 2024
Figure 1. (A) The Tarim Basin is situated in northwestern China. The inset shows the national border of China in the South China Sea. (B) Geological map showing the structural units within the Tarim Basin. The Tabei uplift is located in the northern part of the Tarim Basin. (C) Simplified map
Image
(A) Geographic location of the Tarim Basin, northwestern China. (B) Map showing main tectonic units in the Tarim Basin and the location of the Tabei uplift. (C) Location of the study area on the Tabei uplift. (D) Regional map highlighting the location of tectonic faults and wells in the Tahe oil field.
Published: 01 January 2025
Figure 1. (A) Geographic location of the Tarim Basin, northwestern China. (B) Map showing main tectonic units in the Tarim Basin and the location of the Tabei uplift. (C) Location of the study area on the Tabei uplift. (D) Regional map highlighting the location of tectonic faults and wells
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2024
AAPG Bulletin (2024) 108 (7): 1193–1229.
...Figure 17. Petroleum system event chart of the Tabei uplift (modified from Q. Li et al., 2010 and Yang et al., 2020b ). Є = Cambrian; C = Carboniferous; D = Devonian; E-Q = Paleogene–Quaternary; J = Jurassic; K = Cretaceous; O = Ordovician; P = Permian; S = Silurian; T = Triassic. ...
FIGURES | View All (19)
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The Tarim Basin and study areas. (A) The tectonic components of the Tarim Basin and surrounding area (modified from Jia et al., 1998; used with permission of AAPG). “Shan” means mountains in Chinese. I = Kalpin Uplift; II = Kuqa depression; III = Tabei Uplift. (B) The study area in the central Tabei Uplift is on an anticline dipping gently south and southwest. The contours are on top of the Ordovician. Dashed line = boundary of current oil and gas play.
Published: 01 December 2011
Figure 1 The Tarim Basin and study areas. (A) The tectonic components of the Tarim Basin and surrounding area (modified from Jia et al., 1998 ; used with permission of AAPG). “Shan” means mountains in Chinese. I = Kalpin Uplift; II = Kuqa depression; III = Tabei Uplift. (B) The study area
Image
(a) Tectonic map of Tarim Basin. The Tahe Oilfield is located in the Tabei Uplift, (b) location map of Tahe Oilfield, which is marked with a red pentacle to the south of Akekule Uplift, (c) the map of study area.
Published: 22 May 2025
Figure 1 (a) Tectonic map of Tarim Basin. The Tahe Oilfield is located in the Tabei Uplift, (b) location map of Tahe Oilfield, which is marked with a red pentacle to the south of Akekule Uplift, (c) the map of study area.