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Qiulitage Anticline

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Journal Article
Journal: AAPG Bulletin
Published: 01 August 2022
AAPG Bulletin (2022) 106 (8): 1605–1623.
...Tong Wu; Xiaofei Fu; Haixue Wang; Mingxu Lu; Lingdong Meng; Lei Gong Abstract Smears are formed when faults cross-cut layered sequences. They have been observed within mudstone, shale, siltstone, carbonate, coal, and others. Gypsum smears were observed on a section of the East Qiulitage anticline...
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(A) Anatomy of outcrops in East <span class="search-highlight">Qiulitage</span> <span class="search-highlight">anticline</span> shows that many gypsum ...
Published: 01 August 2022
Figure 11. (A) Anatomy of outcrops in East Qiulitage anticline shows that many gypsum beds are smeared, including (B) continuous and (C) discontinuous beds. The two white dotted lines represent the gypsum formation boundaries, the red lines represent faults, and the values marked at the bottom
Image
(A) Profile of box-shaped <span class="search-highlight">anticline</span> in the core of the East <span class="search-highlight">Qiulitage</span> antic...
Published: 01 August 2022
Figure 2. (A) Profile of box-shaped anticline in the core of the East Qiulitage anticline, where some reverse faults developed. (B) Geological section of the East Qiulitage anticline, part of which represents the profile in (A). (C) Seismic interpretation of the East Qiulitage anticline ( Li et
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—Structural elements map of the Kuqa depression. I = Sidike structural wedg...
Published: 01 January 1998
Figure 5 —Structural elements map of the Kuqa depression. I = Sidike structural wedge subbelt; II = Yiqikelic-Kumukelimu anticline subbelt; III = Yidekeqiangali anticline subbelt; IV = Qiulitage anticline subbelt; V = Yaken anticline subbelt.
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Figure 1. A: Topographic and locality map of central Asia. B: Geological ma...
Published: 01 March 2006
Figure 1. A: Topographic and locality map of central Asia. B: Geological map of Kuche area (after Geological and Mineral Resources Bureau of Xinjiang Uygur Autonomous Region, 1993 ). C: Cross section of Yaha River valley at Qiulitage anticline. D: Shuttle Radar Topography Mission (SRTM) digital
Image
(A) A typical layered stratigraphic profile from the East <span class="search-highlight">Qiulitage</span> anticli...
Published: 01 August 2022
Figure 3. (A) A typical layered stratigraphic profile from the East Qiulitage anticline in which gypsum bed (white line) is smeared along reverse faults but an argillaceous siltstone bed is not smeared (black line). (B) Zoomed view of the gypsum bed with an argillaceous gypsum interbed smeared
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(A) Generalized map showing the location of the Tarim Basin and the study a...
Published: 01 August 2022
Figure 1. (A) Generalized map showing the location of the Tarim Basin and the study area. (B) Map of tectonic units of the Kuqa foreland basin, with the positions of the outcrop and the seismic profile of the East Qiulitage anticline marked. (C) Lithological sketch of the drill site, which
Image
Shortening magnitudes of the Kumugeliemu–<span class="search-highlight">Qiulitage</span> section along the South ...
Published: 29 September 2021
and the Xiqiu anticline. Among these belts, the Kumugeliemu–Kasangtuokai and Qiulitage belts and the Xiqiu anticline have absorbed c. 11.3 km, c. 6.7 km and c. 2.1 km of shortening, respectively.
Journal Article
Journal: AAPG Bulletin
Published: 01 December 2022
AAPG Bulletin (2022) 106 (12): 2547–2561.
..., Qiulitage Anticline, Xinjiang China BU 10608 1547 K faults, petroleum exploration, seismic methods, structural controls, tectonics, traps BU 10610 2043 A Feng Guoqui, Effects of paleoenvironment on continental shale oil enrichment and producibility in the Biyang Depression BU 10604 701...
Journal Article
Journal: Geology
Published: 01 March 2006
Geology (2006) 34 (3): 181–184.
...Figure 1. A: Topographic and locality map of central Asia. B: Geological map of Kuche area (after Geological and Mineral Resources Bureau of Xinjiang Uygur Autonomous Region, 1993 ). C: Cross section of Yaha River valley at Qiulitage anticline. D: Shuttle Radar Topography Mission (SRTM) digital...
FIGURES
Journal Article
Journal: Geology
Published: 01 November 2009
Geology (2009) 37 (11): 1051–1054.
... on the Kuchetawu section (41°55.097′N, 83°03.280′E), which is part in the Qiulitag anticline, exposed (transect X–Y, Fig. 1A ) by the southward-flowing Kuqa River ( Fig. 1A ). Field investigations indicate that in this section the Qiulitag anticline is an overturned fold, consisting of steep strata in the core...
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Journal Article
Published: 29 September 2021
Journal of the Geological Society (2022) 179 (2): jgs2021-029.
... and the Xiqiu anticline. Among these belts, the Kumugeliemu–Kasangtuokai and Qiulitage belts and the Xiqiu anticline have absorbed c. 11.3 km, c. 6.7 km and c. 2.1 km of shortening, respectively. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1998
AAPG Bulletin (1998) 82 (1): 147–159.
...Figure 5 —Structural elements map of the Kuqa depression. I = Sidike structural wedge subbelt; II = Yiqikelic-Kumukelimu anticline subbelt; III = Yidekeqiangali anticline subbelt; IV = Qiulitage anticline subbelt; V = Yaken anticline subbelt. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1999
AAPG Bulletin (1999) 83 (8): 1279–1283.
..., and Hongqi structural zones are composed of a series of right-step en echelon normal faults. Quite a few new gas fields have been found in the structures of these zones ( Jia et al., 1997 ). Near the core of South Qiulitag anticline, an orogen-parallel sinistral strike-slip fault cuts off the anticline...
FIGURES
Journal Article
Published: 26 September 2022
Seismological Research Letters (2022)
... H.‐B. 2020 . Study on paleo‐seismic events in trenches of the eastern qiulitage anticlinal belt , Seismol. Geol. 42 , no.  5 , 1039 , doi: 10.3969/j.issn.0253-4967.2020.05.002 . Zubovich A. V. Wang X. Q. Scherba Y. G. Schelochkov G. G. Reilinger R. Reigber C...
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Journal Article
Journal: GSA Bulletin
Published: 21 October 2022
GSA Bulletin (2022)
... the evaporite horizon near the base of the Cambrian carbonate section (Qiulitage Group, Figs. 1 and 4). Length of shortening is determined by the equation: l = | lfinal linitial| (1) where l is the change in length, lfinal is postdeformation length, and linitial is pre-deformation length. Maximum...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2016
AAPG Bulletin (2016) 100 (2): 191–212.
... in the Kuqa depression. The initially charged oil in the sandstone reservoirs was subsequently displaced by gas at circa 3–2 Ma through fault activation at the edge of the anticline trap. The overpressure evolution for the K 1 bs reservoir sandstone in the Kela-2 gas field indicates that the apparent...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 09 March 2021
Lithosphere (2021) 2021 (1): 8895823.
...., interlimb angle) [ 35 ], it can be found that there are only two types of folds in the Keshen area, which are gentle fold with interlimb angle within the range of 180°–120° and open fold with interlimb in range of 120°–70° (Figure 1 (b)). The Keshen anticline is cut transversely by a series of gently...
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Journal Article
Journal: Interpretation
Published: 23 July 2020
Interpretation (2020) 8 (4): SP81–SP93.
... zone, Huomatu anticline zone, Hu’an anticline zone, and the Fukang fault zone ( He et al., 2004 ; Gao et al., 2010 ). Multiple stages of tectonic movements have created a series of northward-thrusting faults and fault-related folds in the thrust belt ( Guo et al., 2011 ). Figure 1...
Journal Article
Journal: Geosphere
Published: 16 March 2022
Geosphere (2022) 18 (3): 1138–1151.
.... Cross-profile of the Kelasu Section. In this study, we focus only on the northern flank of Kasangtuokai Anticline, corresponding to Section B in Zhang et al. (2015) . In this study, the sampling strategy was designed for magnetostratigraphy of the Cenozoic sediments on the northern flank...
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