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Kalpin Uplift

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Image
—Geologic map of the central part of the Kalpin uplift. Structure is derived from Landsat imagery and our field-work observations. Stratigraphy from unpublished Chinese 1:200,000 scale geological maps. Dashed box shows area of Figure 2.
Published: 01 August 1999
Figure 1 —Geologic map of the central part of the Kalpin uplift. Structure is derived from Landsat imagery and our field-work observations. Stratigraphy from unpublished Chinese 1:200,000 scale geological maps. Dashed box shows area of Figure 2 .
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1998
AAPG Bulletin (1998) 82 (1): 147–159.
... fault zone along its northwestern side. In this paper, we discuss the northern Tarim basin’s structural features, which include three main tectonic units: the Kalpin uplift, the Kuqa depression, and the North Tarim uplift along the northern margin of the Tarim basin. Structural mapping in the Kalpin...
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Image
—Series of imbricated thrust sheets overprinted by strike-slip faulting in the Kalpin uplift. (A) Structural map in the Kalpin uplift showing the geometry of deformed thrust sheets. Line AA′ marks the location of the cross section shown in Figure 4. (B) The restoration by unfaulting of F2. (C) The restoration by unfaulting of F1. The amount of strike-slip displacement is estimated to be 148 km by restoration of strike-slip structures in the uplift. F1 = Piqiang fault, F2 = Tatal-Sajinzi fault.
Published: 01 January 1998
Figure 3 —Series of imbricated thrust sheets overprinted by strike-slip faulting in the Kalpin uplift. (A) Structural map in the Kalpin uplift showing the geometry of deformed thrust sheets. Line AA′ marks the location of the cross section shown in Figure 4 . (B) The restoration by unfaulting
Image
—Landsat MSS (multispectral scanner) image of the western part of the Kalpin uplift showing the major thrusts and crosscutting Piqiang fault (AA′). Image shown is approximately 185 × 185 km in area. Location shown on figure 1.
Published: 01 August 1999
Figure 2 —Landsat MSS (multispectral scanner) image of the western part of the Kalpin uplift showing the major thrusts and crosscutting Piqiang fault (AA′). Image shown is approximately 185 × 185 km in area. Location shown on figure 1 .
Image
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
—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.
...Figure 1 —Geologic map of the central part of the Kalpin uplift. Structure is derived from Landsat imagery and our field-work observations. Stratigraphy from unpublished Chinese 1:200,000 scale geological maps. Dashed box shows area of Figure 2 . ...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1990
AAPG Bulletin (1990) 74 (4): 493–512.
... most closely resembles a miogeoclinal or platform sequence dominated by shallow-marine carbonates and shallow-marine to nonmarine siliciclastics ( Lee, 1985b ). More promising are black shales of the Middle Ordovician Saergan Formation that crop out on the Kalpin uplift ( Figure 9 ). These shales...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2024
AAPG Bulletin (2024) 108 (10): 2009–2043.
.../j.petrol.2020.106987 . He , W. , J. Li , X. Qian , and D. Zheng , 2002 , Analysis of fault structures in the Kalpin fault uplift, Tarim basin : Chinese Geology , v.  29 , no.  1 , p.  37 – 43 . He , Y. , T. Wang , L. Fang , and L. Zhao , 2021 , The 2020...
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Journal Article
Published: 12 January 2024
Canadian Journal of Earth Sciences (2024) 61 (5): 560–585.
..., the Xiaoerbulake Formation in the southeast of the Bachu Uplift zone, and the upper member of the Xiaoerbulake Formation in the Tazhong Uplift zone. In the Tarim Basin, algal-laminated dolomite occurs in the Xiaoerbulake Formation in the Kalpin area and the Bachu, Tazhong, and Tabei uplift zones...
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Journal Article
Published: 12 May 2022
Journal of the Geological Society (2022) 179 (4): jgs2021-148.
... sections in this study are located in the Kalpin Uplift of the northwestern flank of the Tarim Basin ( Fig. 1b ). The Kalpin Shuinichang (or cement plant) section (40°33.605'N, 78°56.712'E) is located about 10 km NW from Kalpin County, Aksu City ( Fig. 1b ). From the base to top, the Penglaiba...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 2003
AAPG Bulletin (2003) 87 (8): 1323–1354.
... tectonic uplift. The almost continuous upper Paleozoic successions in both the Tiekelike and Kalpin regions are therefore used as the primary basis for unraveling the sedimentary history of the basin in the late Paleozoic. Five sedimentary packages and conspicuous hiatuses between the five major...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 21 March 2025
Lithosphere (2024) 2024 (Special 15): lithosphere_2024_130.
.... It is arranged in multiple rows of reverse fault-anticlinal belts in the E‒W direction. Since the late Cenozoic, the Tianshan tectonic system has been reactivated, uplifted, and propagated southward [ 4 , 17 ]. Previous research has shown that the Kalpin foreland thrust belt is a typical thin-skinned nappe...
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Image
(A) Regional geological map showing the location of the two-dimensional seismic line, hydrocarbon seeps, wells, and structural map. The hydrocarbon seep data are from Gao et al. (2012). The blue line represents the regional stratigraphic framework connection. (B) Upper Neoproterozoic–middle Cambrian comparative stratigraphic framework from the Aksu-Piqiang area to the Bachu uplift. Some stratigraphic data were adapted from L. Wu et al. (2018), Zhu et al. (2020a), and G. Zhu et al. (2021). AG = Aksu Group; DQ = Dongqiaoenbrak Formation; DW = Dongwu Formation; KFTB = Kalpin fold-thrust belt; MY = Muyangtan Formation; QEG = Qiaoenbrak Group; QG = Qigebrak Formation; SG = Sugetbrak Formation; WS = Wusongger Formation; XE = Xiaoerbrak Formation; XF = Xifangshan Formation; YE = Yuertusi Formation; YU = Yuermeinak Formation.
Published: 01 October 2024
–middle Cambrian comparative stratigraphic framework from the Aksu-Piqiang area to the Bachu uplift. Some stratigraphic data were adapted from L. Wu et al. (2018) , Zhu et al. (2020a) , and G. Zhu et al. (2021) . AG = Aksu Group; DQ = Dongqiaoenbrak Formation; DW = Dongwu Formation; KFTB = Kalpin fold
Journal Article
Published: 01 March 2000
Journal of Paleontology (2000) 74 (2): 282–300.
...CHEN XU; NI YU-NAN; CHARLES E. MITCHELL; QIAO XIN-DONG; ZHAN SHI-GAO Abstract Late Ordovician rocks of the Qilang and Yingan formations from the Kalpin area in the Tarim region of western Xinjiang, China (Tarim palaeoplate) contain a moderately diverse graptolite fauna. The fauna from the Qilang...
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Journal Article
Published: 07 November 2024
Seismological Research Letters (2025) 96 (3): 1901–1910.
...Qian Guo; Yangmao Wen; Caijun Xu; Xiong Zhao Abstract The Keping fold‐and‐thrust belt (KFB), situated at the southern front of the Tianshan orogenic belt, represents a typical thin‐skinned imbricated structure resulting from the uplift and southward‐thrusting orogeny of the Tianshan. The KFB...
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Image
Profiles of structural studies, lines AA1, BB1, CC1, DD1 (after [12], [18], with additions by Li Goudu). For location of profiles see Fig. 1. 1 – concordant bedding; 2 – discordant bedding; 3 – faults; 4 – basement; 5 – direction of displacement along faults; 6 – granites; 7 – wells. Letters mark folded areas: a – Kunlun, b – Tien Shan; Roman n umerals mark structural units of the sedimentary cover: u plifts (I – North-Tarim, 11 – Central-Tarim, III – South-Tarim thick), marginal uplifts (IV – Kalpin, V – Kuruktag, VI – Tikeliktag, VII – Altuntag) , basins (VI II – Kucha, IX – Northern, X – Southwestern, XI – Southeastern).
Published: 01 October 1998
– granites; 7 – wells. Letters mark folded areas: a – Kunlun, b – Tien Shan; Roman n umerals mark structural units of the sedimentary cover: u plifts (I – North-Tarim, 11 – Central-Tarim, III – South-Tarim thick), marginal uplifts (IV – Kalpin, V – Kuruktag, VI – Tikeliktag, VII – Altuntag) , basins
Journal Article
Journal: AAPG Bulletin
Published: 01 December 2011
AAPG Bulletin (2011) 95 (12): 2061–2083.
...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...
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Journal Article
Published: 01 May 2003
Journal of Paleontology (2003) 77 (3): 430–441.
...LIU BINGLI; J. KEITH RIGBY; ZHU ZHONGDE Abstract Moderately diverse Middle Ordovician sponge faunas of Darriwilian (late Arenig to early Llanvirn) age have been discovered in outcrops in the Bachu-Kalpin area of the Tarim platform of Xinjiang, China. These are the first reported occurrences...
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Journal Article
Journal: Geophysics
Published: 03 June 2011
Geophysics (2011) 76 (4): B127–B137.
... and depressions that developed as the result of a long and complicated tectonic history ( Jia, 1997 ; Jia et al., 1998 ). The northern Tarim Basin includes three main tectonic units: the Kalpin Uplift, the Kuqa Depression, and the Tabei Uplift ( Figure 1 a). Figure 1. Location of the Tarim Basin...
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