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Aheqi fault zone

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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1998
AAPG Bulletin (1998) 82 (1): 147–159.
...Dong Jia; Huafu Lu; Dongsheng Cai; Shimin Wu; Yangshen Shi; Chuming Chen ABSTRACT The rhombus-shaped Tarim basin in northwestern China is controlled mainly by two left-lateral strikeslip systems: the northeast-trending Altun fault zone along its southeastern side and the northeast-trending Aheqi...
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—Simplified Cenozoic tectonic map of the Tarim basin and the adjacent area showing the transpressional structural features under the sinistral movements of both the Altun fault zone and the Aheqi fault zone.
Published: 01 January 1998
Figure 1 —Simplified Cenozoic tectonic map of the Tarim basin and the adjacent area showing the transpressional structural features under the sinistral movements of both the Altun fault zone and the Aheqi fault zone.
Image
—Tectonic scheme of the northern margin of the Tarim basin. Along the Aheqi fault zone, the Kalpin uplift encounters transpressional tectonic processes to form a complicated strike-slip fault-propagation fold at the western restraining bend of the Aksu arc. The Kuqa depression shows the transtensional tectonic process to form a pull-apart basin (Baicheng basin) at the eastern releasing bend of the arc. AF = Aksu fault, YF = Yulgun fault.
Published: 01 January 1998
Figure 2 —Tectonic scheme of the northern margin of the Tarim basin. Along the Aheqi fault zone, the Kalpin uplift encounters transpressional tectonic processes to form a complicated strike-slip fault-propagation fold at the western restraining bend of the Aksu arc. The Kuqa depression shows
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1999
AAPG Bulletin (1999) 83 (8): 1279–1283.
... of the Aheqi fault zone. Although the Nikolaeev line is cut by the Talas-Fergana dextral fault north of Kashi, the Talas-Fergana fault does not terminate the Aheqi fault. The Carboniferous limestone of south Tianshan thrusted southward over the Mesozoic and Tertiary strata of the Tarim basin, showing...
FIGURES
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(A) Sketch map of eastern Eurasia (modified from Jahn, 2004), which shows the location of the study area. CAOB—Central Asian orogenic belt; EEC—East European craton; QQ—Qaidam Qinling. (B) Tectonic divisions of the Tianshan orogen (modified from Alexeiev et al., 2015). (C) Geological map of the Chinese segment of the Tianshan orogen (modified from XBGMR, 1993). Abbreviations of the major faults: BF—Baluntai fault, NLF—Nalati fault, MTSZ—Main Tianshan shear zone. Abbreviations of the localities cited in the text: ah—Aheqi, at—Aertengkesi, c—Changawuzi, g—Gangou, gl—Guluogou, k—Kulehu, ks—Kokshal, m—Mishigou, ms—Misibulake, mk—Mandalek, n—Nalati, s—Serikeyayilake, w—Wuwamen, t—Tonghuashan, and y—Yushugou.
Published: 29 August 2017
) Geological map of the Chinese segment of the Tianshan orogen (modified from XBGMR, 1993 ). Abbreviations of the major faults: BF—Baluntai fault, NLF—Nalati fault, MTSZ—Main Tianshan shear zone. Abbreviations of the localities cited in the text: ah—Aheqi, at—Aertengkesi, c—Changawuzi, g—Gangou, gl—Guluogou
Journal Article
Journal: GSA Bulletin
Published: 29 August 2017
GSA Bulletin (2018) 130 (1-2): 284–306.
...) Geological map of the Chinese segment of the Tianshan orogen (modified from XBGMR, 1993 ). Abbreviations of the major faults: BF—Baluntai fault, NLF—Nalati fault, MTSZ—Main Tianshan shear zone. Abbreviations of the localities cited in the text: ah—Aheqi, at—Aertengkesi, c—Changawuzi, g—Gangou, gl—Guluogou...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 21 March 2025
Lithosphere (2024) 2024 (Special 15): lithosphere_2024_130.
... should be the residue of the colluvial wedge. The overall NEE-trending Maidan fault controls the northern margin of the Aheqi Valley, and this fault is a complex fault zone composed of multiple branching structures ( Figure 2 ). Since the beginning of historical seismic record, the seismic...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2011
AAPG Bulletin (2011) 95 (12): 2061–2083.
... strike-slip fault system in the south and Aheqi strike-slip fault zone in the north. The distant Indian–Tibet collision provides a north–south compressional component to the basin. Under the influence of the left-lateral movement of these two fault systems during the Cenozoic, the northeast and southwest...
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Journal Article
Published: 01 March 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (1): 83–100.
... deposits are developed on the east and south of the slope. During this period, intra-platform shoals were mainly distributed in three zones, i.e. the Tabei area, both sides of the Tazhong trough, and the surrounding areas of the Mazhatage Fault ( Fig. 10a ). In the Tabei area, intra-platform shoals...
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Journal Article
Journal: GSA Bulletin
Published: 21 September 2023
GSA Bulletin (2024) 136 (5-6): 2195–2213.
... from XGSC, 2007 ). The black boxes show the locations of sampled areas shown in Figure 2 . AYB—Aqishan-Yamansu belt; BF—Baluntai fault; CAOB—Central Asian Orogenic Belt; DLF—Dalabute fault; KMF—Kelameili fault; MTSZ—Main Tianshan shear zone; NF—Nalati fault; NTS—North Tianshan suture; STS—South...
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