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Jinxi Belt

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Location and paleoenvironmental reconstruction of the Ordos Basin, its tect...
Published: 13 September 2018
Fig. 1. Location and paleoenvironmental reconstruction of the Ordos Basin, its tectonic architecture, and the location of well W100 ( Yuan et al. 2017 ). I, Yimeng uplift; II, West margin thrust belt; III, Tianhuan depression; IV, Yishan slope; V, Jinxi flexure belt; VI, Weibei uplift. [Colour
Journal Article
Journal: Economic Geology
Published: 01 January 2004
Economic Geology (2004) 99 (1): 199–202.
... of the major tectonic domains of Xinjiang Province in northwest China, namely the Altay orogen and the Tianshan orogen, both part of the great Central Asian orogenic belt or Altaid orogenic collage. The belt extends from the Urals in the east and north, eastward across Asia to China, and forms a series...
Journal Article
Published: 01 September 2012
Bulletin of Canadian Petroleum Geology (2012) 60 (3): 158–165.
... (SINOPEC), and China National Offshore Oil Corporation (CNOOC) for the period 1960–2009. Located in central China, Ordos Basin is divided into six geological structural units: the Yimeng Uplift, Jinxi Fold Belt, Yishan Slope, Tianhuan Depression, Western Thrust Belt, and Wei River Uplift ( Fig. 1...
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Journal Article
Journal: AAPG Bulletin
Published: 15 October 2019
AAPG Bulletin (2019) 103 (10): 2343–2367.
...., 2006 ; Zeng and Li, 2009 ). Modern tectonic features and basement characteristics of the Ordos Basin permit its division into six tectonic units, namely, the Yimeng uplift, Jinxi fault-fold belt, Yishan slope, Tianhuan depression, Western thrust belt, and Weibei uplift ( Yang et al., 2006...
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Journal Article
Journal: Interpretation
Published: 08 February 2017
Interpretation (2017) 5 (2): SF81–SF98.
... this basin into several primary tectonic units: Western Thrust Belt, Tianhuan Depression, Yishan Slope, Jinxi Flexural Fold Belt, Yimeng Uplift, and Weibei Uplift. The Yishan Slope has simple structures and low angle dips and is the major tectonic unit (Figure  1 ). Figure 1. (a) Tectonic units...
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Journal Article
Published: 13 September 2018
Canadian Journal of Earth Sciences (2019) 56 (1): 47–59.
...Fig. 1. Location and paleoenvironmental reconstruction of the Ordos Basin, its tectonic architecture, and the location of well W100 ( Yuan et al. 2017 ). I, Yimeng uplift; II, West margin thrust belt; III, Tianhuan depression; IV, Yishan slope; V, Jinxi flexure belt; VI, Weibei uplift. [Colour...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1996
AAPG Bulletin (1996) 80 (7): 1110–1133.
... axis on the west side of the basin ( Figure 1 ). The Ordos basin can be divided into six different structural units ( Figure 1 ). (1) The Jinxi folded zone is composed of five north-south- and northeast-southwest-trending zones of brachy-axis folds from north to south. (2) The Shanbei slope...
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Journal Article
Journal: Interpretation
Published: 10 December 2018
Interpretation (2019) 7 (1): T67–T82.
..., Tianhuan depression, Yishan slope, Jinxi flexure belt, and Weibei uplift ( Yang et al., 2005 ). The block under investigation is in the transitional region between the Yishan slope and the Yimeng uplift, which reaches an elevation of 1300–1600 m (Figure  1b ), and the main data sources of this study...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1986
AAPG Bulletin (1986) 70 (4): 377–395.
... generally into a south belt and a north belt. In China, the north belt corresponds approximately to the Kunlun foldbelt and the south belt to the Himalayan foldbelt ( Figure 2 ). Medial massifs occur between them. Continental accretion developed mainly from north to south and, in turn, developed...
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Journal Article
Published: 09 April 2019
Canadian Journal of Earth Sciences (2019) 56 (10): 1027–1040.
... ) ( Fig. 1B ). Internally, it can be further divided into six tectonic units, designated the Yimeng Uplift, Western Thrust Belt, Tianhuan Depression, Yishan Slope, Jinxi Flexure Belt, and the Weibei Uplift ( Fig. 1B ). The Western Thrust Belt and the Tianhuan Depression are separated by large faults along...
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Journal Article
Journal: Economic Geology
Published: 01 March 2005
Economic Geology (2005) 100 (2): 405–413.
... belt, southern India— Biswajit Mishra, Nabarun Pal, and Amit Basu Sarbadhikari 1 The Jinxi–Yelmand high-sulfidation epithermal gold deposit, western Tianshan, Xinjiang province, P.R. China— Xiao Long, Nick Hayward, Graham Begg, Fu Minlu, Wang Fangzheng, and Franco Pirajno 17 Geochemistry...
Journal Article
Journal: Economic Geology
Published: 01 January 2020
Economic Geology (2020) 115 (1): 79–100.
..., called postcollisional- or Dabie-type porphyry Mo deposits, has been proposed, in particular for the occurrences within the Dabie-Qinling orogenic belt (e.g., Chen et al., 2017 ). Although much has been learned in the past few decades about the nature of ore-forming melts in Climax-type porphyry Mo...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2012
AAPG Bulletin (2012) 96 (7): 1173–1195.
... depression, Yishan ramp, Jinxi flexural belt, and Weibei uplift. The Daniudi gas field, the focus of this article, which is located in the northeastern Yishan ramp, has an area of approximately 775 mi 2 (∼2003 km 2 ; Figure 1 ). Figure 1 Regional index map showing the study area. (A) Structural...
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Journal Article
Journal: AAPG Bulletin
Published: 15 January 2020
AAPG Bulletin (2020) 104 (1): 205–226.
..., located in northcentral China, covers an area of more than 370,000 km 2 (>143,000 mi 2 ) ( Shi et al., 2011 ; Jiang et al., 2018 ) ( Figure 1A, B ). The elevation of this flat basin is higher in the east than in the west. The basin consists of six tectonic units: the Yimeng uplift, the Jinxi folding...
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Journal Article
Journal: AAPG Bulletin
Published: 15 December 2019
AAPG Bulletin (2019) 103 (12): 2835–2859.
... is located at the interface between China’s eastern and western structural domains and is the second largest sedimentary basin in China ( Yang et al., 2005 , 2017 ). The entire basin can be subdivided into six structural units: the Tianhuan depression, the Yimeng uplift, the Jinxi fault-fold belt...
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Journal Article
Journal: Interpretation
Published: 27 June 2017
Interpretation (2017) 5 (4): SP27–SP39.
... tectonic characteristics, the basin can be subdivided into six regional tectonic units: the Weibei Uplift in the south margin, Yishan Slope in the middle of the basin, Yimeng Uplift in the north part, Jinxi fault-fold belt in the eastern margin, Western thrust belt, and Tianhuan Depression in the western...
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Journal Article
Journal: Interpretation
Published: 05 January 2018
Interpretation (2018) 6 (1): T175–T190.
... Margin Thrust Belt, Tianhuan Depression, Yishan Ramp, Jinxi Flexural Fold Belt, and Weibei Uplift ( Yao et al., 2013 ; Yang et al., 2015b ). The southeastern Ordos Basin is located in the south of the Yishan Ramp and known as one important area for shale-gas exploration bounded by the Yellow River...
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Journal Article
Published: 10 August 2017
Canadian Journal of Earth Sciences (2017) 54 (12): 1228–1247.
... with convergent margins, and (3) a Late Triassic to Early Cretaceous intraplate remnant craton basin ( Yang et al. 2005 ). Tectonically, the basin is divided into six structural units: the Yimeng Uplift, the Western Edge Fold-Thrust Belt, the Tianhuan Depression, the Yishan Slope, the Weibei Uplift, and the Jinxi...
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Journal Article
Journal: AAPG Bulletin
Published: 15 November 2019
AAPG Bulletin (2019) 103 (11): 2573–2596.
... depression and Jinxi fault–fold unit in the east, Yishan slope in the central part of the basin, Western thrust belt, and Weibei uplift in the south ( Figure 1 ) ( Yang et al., 2008 ; Jiang et al., 2012 ; Liu et al., 2014 ; Lyu et al., 2016 ; Wang et al., 2017 ). The Ordos Basin is polycyclic, having...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2016
AAPG Bulletin (2016) 100 (6): 969–1002.
... Formation; E 2 s 4 - E 1 k = the fourth member of Shahejie Formation to Kongdian Formation; E 3 d = Dongying Formation; JX1-1E-1 = Jinxi 1-1E-1; N 1 g = Guantao Formation; N 2 m 1 -Q = the first member of Minghuazhen Formation to Quaternary; N 2 m 2 = the second member of Minghuazheng Formation; QK17-1-1...
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