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Qimantag Mountains

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Journal Article
Journal: Economic Geology
Published: 01 September 2014
Economic Geology (2014) 109 (6): 1787–1799.
... ( Fig. 1B ). The Qimantage area is bounded by the Qimantage Mountains to the north and the Cenozoic Kumukuli basin to the south ( Mo et al., 2007 ; Li et al., 2008 ; Gao et al., 2010 ). The Qimantage Mountains are composed mainly of intermediate to felsic intrusions. The Qimantage area...
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Journal Article
Published: 15 April 2024
Canadian Journal of Earth Sciences (2024) 61 (7): 760–776.
... , A.K. , Cao , J.H. , Chen , X.N. , Feng , Y.L. , et al. 2014 . Late Silurian to Early Devonian granitoids in the Qimantage area, east Kunlun mountains: LA-ICP-MS zircon U–Pb ages, geochemical features and geological setting . Geological Review , 60 : 201 – 215 (in Chinese...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 09 September 2021
Lithosphere (2021) 2021 (Special 1): 7705469.
... sources. The south part shows stable heavy minerals, and it may be supplied mainly by Qimantag-east Kunlun orogen and partly by Altyn Mountain. The Yueyashan district is supplied by Altyn Mountain and exposed rocks around. The evidence mentioned shows that several small-scale sedimentary basins existed...
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Journal Article
Journal: GSA Bulletin
Published: 12 July 2023
GSA Bulletin (2024) 136 (3-4): 1050–1066.
... of Xiaojianshan gabbro in Qimantage Mountain, eastern Kunlun orogenic belt : Geotectonica et Metallogenia , v. 39 , p. 1176 – 1184 [ in Chinese with English abstract ]. Argand , E. , 1924 , La tectonique de l’Asie : Proceedings of the VIIIth International Geological Congress Brussels , p. 181...
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Journal Article
Journal: GSA Bulletin
Published: 24 December 2021
GSA Bulletin (2022) 134 (9-10): 2179–2205.
... in Qimantage Mountain, Eastern Kunlun Orogenic Belt [ in Chinese with English abstract ]: Geotectonica et Metallogenia , v. 39 , no. 6 , p. 1176 – 1184 . Avouac , J.P. , Tapponnier , P. , Bai , M. , You , H. , and Wang , G. , 1993 , Active thrusting and folding along...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 27 August 2020
Lithosphere (2020) 2020 (1): 8829964.
... of the Central China Orogenic System Earth-Science Reviews 2018 186 231 261 10.1016/j.earscirev.2017.12.006 2-s2.0-85039545945 Cui M. H. Meng F. C. Wu X. K. Early Ordovician island arc of Qimantag Mountain, eastern Kunlun: evidences from geochemistry, Sm-Nd isotope and geochronology...
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Journal Article
Journal: GSA Bulletin
Published: 22 May 2023
GSA Bulletin (2024) 136 (1-2): 619–636.
... northward. A series of magmatic and metamorphic events was associated with this subduction event, as certified by the 507 ± 8 Ma Qingshuiquan granulite in the Central East Kunlun Suture zone ( He et al., 2023 ) and the 480 ± 3 Ma Yaziquan island-arc diorite in the Qimantag Mountains ( Cui et al., 2011 ; Li...
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Image
A. Location of the study area and mountain ranges (thick lines). B. A simplified regional tectonic map (modified after Li et al., 2008). I = Tarim basin; II = north Arkin-Dunhuang block; III = Arkin orogenic belt (dark gray): III-1 = Hongliugou-Lapeiquan ophiolitic mélange belt, III-2 = Mid-Arkin massif, III-3 = Apa-Mangya early Paleozoic ophiolitic mélange belt; IV = east Kunlun domain (light gray): IV-1 = northern Kunlun (Qimantage) early Paleozoic arc, IV-2 = Mid-Kunlun microcontinent, IV-3 = southern Kunlun accretionary complex; V = Bayankala fold belt; VI = Qaidam basin; VII = Qilian orogenic belt. Thick lines are fault and deformation zones, and dashed lines are inferred structures; ➀ = north Arkin deformation zone, ➁ = south Arkin deformation zone, ➂ = north Kunlun fault, ➃ = Heishan-Nalinggele fault, ➄ = Baiganhu deformation zone, ➅ = Mid-Kunlun fault, ➆ = south Kunlun deformation zone, ➇ = fault defining the northern boundary of the Qaidam basin. Areas enclosed by dotted lines are Qimantage and Kumukuli basin. C. Geologic map showing three W-Sn deposits of the Baiganhu district (modified after a map provided by the Institute of Geologic Survey of Jilin Province). D. Detailed geologic map showing the Baiganhu Main W-Sn deposit (modified after a map provided by the Institute of Geologic Survey of Jilin Province). E. Detailed geologic map showing the Bashi-Erxi W-Sn deposit (modified after a map provided by the Institute of Geologic Survey of Jilin Province). Skarns are composed of tremolite, diopside, muscovite, and quartz. Occurrences are defined by cutoff grades of 0.15 wt % WO3 and 0.1 wt % Sn. Sampling locations are shown with stars and sample numbers are depicted next to the symbols. Samples collected in the Keke-Kaerde deposit, Baiganhu Main deposit, and Bashi-Erxi deposit start with KK, BG, and BE, respectively.
Published: 01 September 2014
Fig. 1 A. Location of the study area and mountain ranges (thick lines). B. A simplified regional tectonic map (modified after Li et al., 2008 ). I = Tarim basin; II = north Arkin-Dunhuang block; III = Arkin orogenic belt (dark gray): III-1 = Hongliugou-Lapeiquan ophiolitic mélange belt, III-2
Image
A. Location of the study area and mountain ranges (thick lines). B. A simplified regional tectonic map (modified after Li et al., 2008). I = Tarim basin; II = north Arkin-Dunhuang block; III = Arkin orogenic belt (dark gray): III-1 = Hongliugou-Lapeiquan ophiolitic mélange belt, III-2 = Mid-Arkin massif, III-3 = Apa-Mangya early Paleozoic ophiolitic mélange belt; IV = east Kunlun domain (light gray): IV-1 = northern Kunlun (Qimantage) early Paleozoic arc, IV-2 = Mid-Kunlun microcontinent, IV-3 = southern Kunlun accretionary complex; V = Bayankala fold belt; VI = Qaidam basin; VII = Qilian orogenic belt. Thick lines are fault and deformation zones, and dashed lines are inferred structures; ➀ = north Arkin deformation zone, ➁ = south Arkin deformation zone, ➂ = north Kunlun fault, ➃ = Heishan-Nalinggele fault, ➄ = Baiganhu deformation zone, ➅ = Mid-Kunlun fault, ➆ = south Kunlun deformation zone, ➇ = fault defining the northern boundary of the Qaidam basin. Areas enclosed by dotted lines are Qimantage and Kumukuli basin. C. Geologic map showing three W-Sn deposits of the Baiganhu district (modified after a map provided by the Institute of Geologic Survey of Jilin Province). D. Detailed geologic map showing the Baiganhu Main W-Sn deposit (modified after a map provided by the Institute of Geologic Survey of Jilin Province). E. Detailed geologic map showing the Bashi-Erxi W-Sn deposit (modified after a map provided by the Institute of Geologic Survey of Jilin Province). Skarns are composed of tremolite, diopside, muscovite, and quartz. Occurrences are defined by cutoff grades of 0.15 wt % WO3 and 0.1 wt % Sn. Sampling locations are shown with stars and sample numbers are depicted next to the symbols. Samples collected in the Keke-Kaerde deposit, Baiganhu Main deposit, and Bashi-Erxi deposit start with KK, BG, and BE, respectively.
Published: 01 September 2014
Fig. 1 A. Location of the study area and mountain ranges (thick lines). B. A simplified regional tectonic map (modified after Li et al., 2008 ). I = Tarim basin; II = north Arkin-Dunhuang block; III = Arkin orogenic belt (dark gray): III-1 = Hongliugou-Lapeiquan ophiolitic mélange belt, III-2
Journal Article
Journal: GSA Bulletin
Published: 22 August 2022
GSA Bulletin (2023) 135 (3-4): 1034–1052.
... elevation model showing the location of the East Kunlun orogenic belt in Central China orogenic system and Tibetan Plateau. (B) Schematic map showing the tectonic division and ophiolitic mélanges in East Kunlun orogenic belt (modified after Dong et al., 2018b ). QXM—Qimantag-Xiangride ophiolitic mélange...
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Journal Article
Journal: Interpretation
Published: 10 December 2018
Interpretation (2019) 7 (1): T1–T19.
... by the peripheral Paleozoic orogens of the Tianshan, West Kunlun, and the Arejin Mountains ( Zhang et al., 2008 ). These orogens caused the strata within the Tarim Basin to be affected by different tectonic movements during their formation processes, which contributed to the differences in fault expressions within...
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Journal Article
Journal: GSA Bulletin
Published: 24 March 2025
GSA Bulletin (2025)
..., Petrogenesis and tectonic implications of the Late Triassic syenogranite in Qimantag area: East Kunlun Mountains: Acta Petrologica et Mineralogica, v. 37, p. 197 210 [in Chinese with English abstract]. Zhang, S., Huang, F., Xu, J., Zeng, Y., Lv, M., Su, C., Tian, Y., Tian, Y., Fan, H., and Wang, S., 2024...
Journal Article
Published: 03 October 2022
American Mineralogist (2022) 107 (10): 1968–1981.
... driven by metasomatism . Contributions to Mineralogy and Petrology , 157 , 491 – 504 . Cui , M.H. , Meng , F.C. , and Wu , X.K. ( 2011 ) Early Ordovician island arc of Yaziquan, west of Qimantag Mountain, Eastern Kunlun: evidences from geochemistry, Sm–Nd isotopes and geochronology...
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Journal Article
Published: 20 July 2022
Canadian Journal of Earth Sciences (2022) 59 (9): 566–579.
.... , Chen , X.N. , Feng , Y.L. , and Li , X. 2014 . Late Silurian to Early Devonian granitoids in the Qimantage area, East Kunlun mountains: LA-ICP-MS zircon U-Pb ages, geochemical features and geological setting . Geological Review , 60 : 201 – 215 [ in Chinese with English abstract...
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Journal Article
Published: 26 October 2021
Geological Magazine (2022) 159 (1): 153–172.
... mixed sediments is similar to that of Silurian granite in Qimantag Mountain, but is different from that of Triassic granite in this area and Palaeozoic granites in the northern Qaidam Basin (Fig.  8 c, d). On the whole, the source rocks of the fine-grained mixed sediments are Palaeozoic granites, which...
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Journal Article
Published: 09 March 2020
Canadian Journal of Earth Sciences (2020) 57 (8): 885–902.
... , Y.L. 2011 . The discovery of Early Silurian intrusive rocks in Qimantage area and its geological significance . Qinghai Science Technology , 5 : 26 – 30 . [In Chinese with English abstract.] Chen , J. , Xie , Z.Y. , Li , B. , Tan , S.X. , Ren , H. , Zhang , Q.M...
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Journal Article
Published: 01 September 2002
Petroleum Geoscience (2002) 8 (3): 279–285.
... the evolution of the basin ( Ren 1993 ; Shen et al. 1994 a , b ). The Qaidam Basin, with an area of 129 000 km 2 , is bounded by the Aljin Mountains to the northwest, the Qilian Mountains to the northeast, the Qimantager Mountains to the southeast and East Kunlun Mountains to the southwest ( Fig.1...
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Journal Article
Journal: Economic Geology
Published: 01 January 2016
Economic Geology (2016) 111 (1): 29–55.
... of boninites , in Crawford A.J. , ed., Boninites and related rocks : Unwin Hyman , p. 1 – 49 . Cui M.H. Meng F.C. Wu X.K. , 2011 , Early Ordovician island arc of Yaziquan, west of Qimantag Mountain, eastern Kunlun: Evidences from geochemistry, Sm-Nd isotope and geochronology...
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Journal Article
Published: 17 March 2023
Canadian Journal of Earth Sciences (2023) 60 (6): 672–691.
.... The EKOB was divided into four tectonic units, namely, the North Qimantag belt, the Central Kunlun belt, the Southern Kunlun belt, and the Bayanhar terrane by three ophiolitic mélange zones, from north to south: the Qimantagh–Xiangride mélange zone, Aqikekulehu–Kunzhong mélange zone, and Muztagh–Buqingshan...
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Journal Article
Published: 01 April 2020
American Mineralogist (2020) 105 (4): 479–497.
... . Cui , M.H. , Meng , F.C. , and Wu , X.K. ( 2011 ) Early Ordovician island arc of Yaziquan, west of Qimantag mountain, Eastern Kunlun: evidences from geochemistry, Sm–Nd isotope and geochronology of intermediate-basic igneous rocks. Acta Petrologica Sinica , 27 , 3365 – 3365...
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