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Bangong-Nujiang suture zone

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Journal Article
Journal: GSA Bulletin
Published: 04 January 2021
GSA Bulletin (2021) 133 (9-10): 1875–1889.
...Jian-Jun Fan; Yaoling Niu; Yi-Ming Liu; Yu-Jie Hao Abstract Knowledge of the timing of the closure of the Meso-Tethys Ocean as represented by the BangongNujiang Suture Zone, i.e., the timing of the Lhasa-Qiangtang collision, is critical for understanding the Mesozoic tectonics of the Tibetan...
FIGURES | View All (12)
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 May 2017
Lithosphere (2018) 10 (1): 142–155.
... along the Bangong-Nujiang suture zone in south-central Tibet. Diamond grains are 100–300 µm, pale yellow and reddish-orange to colorless, commonly anhedral in habit, and range in morphology from elongated to octahedral and subhedral crystals. They display a characteristic shift in the Raman spectra...
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Image
Sedimentary model demonstrating that the Bangong-Nujiang Suture Zone (BNSZ) was in the same old land together with the Lhasa terrane (LS) and the Qiangtang terrane (QT) during the Early to Middle Triassic (T1-T2) that was rifted as a continental rift at the end of the Late Triassic (T33) (modified after Zhao et al., 2001).
Published: 27 June 2019
Figure 3. Sedimentary model demonstrating that the Bangong-Nujiang Suture Zone (BNSZ) was in the same old land together with the Lhasa terrane (LS) and the Qiangtang terrane (QT) during the Early to Middle Triassic (T 1 -T 2 ) that was rifted as a continental rift at the end of the Late Triassic
Image
Representative view of the Bangong-Nujiang Suture Zone (BNSZ) during the Triassic as the Bangong-Nujiang Ocean (BNO), which belongs to a part of the Tethys Ocean. Under this view, the Lhasa Terrane (LS) was in the northern margin of Gondwanaland while the Qiangtang Terrane had drifted across the equator during the Triassic (modified after Muttoni et al., 2009).
Published: 27 June 2019
Figure 2. Representative view of the Bangong-Nujiang Suture Zone (BNSZ) during the Triassic as the Bangong-Nujiang Ocean (BNO), which belongs to a part of the Tethys Ocean. Under this view, the Lhasa Terrane (LS) was in the northern margin of Gondwanaland while the Qiangtang Terrane had drifted
Journal Article
Journal: GSA Bulletin
Published: 07 August 2023
GSA Bulletin (2024) 136 (3-4): 1379–1394.
... of the geodynamics of the Tethyan tectonic evolution. The study of intraplate oceanic-island fragments in the BangongNujiang Suture Zone of Northern Tibet, which are remnants of the oceanic crust, is important for determining the nature and tectonic evolution of the BangongNujiang Tethyan Ocean. Here, we present...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 27 June 2019
Lithosphere (2019) 11 (5): 683–696.
...Figure 3. Sedimentary model demonstrating that the Bangong-Nujiang Suture Zone (BNSZ) was in the same old land together with the Lhasa terrane (LS) and the Qiangtang terrane (QT) during the Early to Middle Triassic (T 1 -T 2 ) that was rifted as a continental rift at the end of the Late Triassic...
FIGURES | View All (11)
Journal Article
Journal: GSA Bulletin
Published: 15 May 2023
GSA Bulletin (2024) 136 (1-2): 846–860.
...Wan-Long Hu; Qiang Wang; Gong-Jian Tang; Yue Qi; Jun Wang; Zong-Yong Yang; Peng Sun Abstract Mafic dikes are generally emplaced in extensional tectonic settings and provide key information regarding deep mantle processes and sources. The Bangong-Nujiang suture zone was formed by the collision...
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Journal Article
Journal: GSA Bulletin
Published: 10 March 2020
GSA Bulletin (2020) 132 (9-10): 2202–2220.
...Yue Tang; Qing-Guo Zhai; Sun-Lin Chung; Pei-Yuan Hu; Jun Wang; Xu-Chang Xiao; Biao Song; Hai-Tao Wang; Hao-Yang Lee Abstract The Meso-Tethys was a late Paleozoic to Mesozoic ocean basin between the Cimmerian continent and Gondwana. Part of its relicts is exposed in the BangongNujiang suture zone...
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Journal Article
Published: 30 October 2019
Journal of Sedimentary Research (2019) 89 (10): 1039–1054.
... of the Tibetan Plateau before the India-Eurasia collision. The timing of the Lhasa–Qiangtang collision was mainly constrained by the ophiolite and magmatic rocks in previous studies, with only limited constraints from the sedimentary rocks within and adjacent to the BangongNujiang suture zone. In the middle...
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Image
(A) Immobile incompatible element discrimination diagram showing the magmatic data of the intraplate oceanic-island fragments in the Bangong–Nujiang Suture Zone; (B–F) chondrite-normalized rare earth element variation for the magmatic rocks of the intraplate oceanic-island fragments in the Bangong–Nujiang Suture Zone; (G–K) primitive mantle–normalized multi-element variation patterns for the magmatic rocks of the intraplate oceanic-island fragments in the Bangong–Nujiang Suture Zone; (L) diagram of εNd(t) versus initial 87Sr/86Sr showing the magmatic samples of intraplate oceanic-island fragments preserved in the Bangong–Nujiang Suture Zone, where (t) refers to the eruption ages (modified from Meng et al., 2015, and Zhong et al., 2017). OIB—oceanic-island basalt; MORB—mid-oceanic-ridge basalt; DMM—depleted MORB mantle; EM—enriched mantle; LCC—lower continental crust; GLOSS—global subducting sediment.
Published: 07 August 2023
Figure 5. (A) Immobile incompatible element discrimination diagram showing the magmatic data of the intraplate oceanic-island fragments in the BangongNujiang Suture Zone; (B–F) chondrite-normalized rare earth element variation for the magmatic rocks of the intraplate oceanic-island fragments
Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1202–1222.
... basin (31°00′–32°40′, 84°30′–87°05′) in central Tibet, which crosses the southern margin of the Qiangtang block, the Bangong-Nujiang suture zone, and the northern half of the Lhasa block, is characterized by up to 5000 m of continental-marine clastic-carbonate sediments and is ideally positioned...
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Journal Article
Journal: GSA Bulletin
Published: 16 February 2023
GSA Bulletin (2023) 135 (11-12): 2849–2867.
.... In this study, we present geological, geochronological, geochemical, and zircon isotopic data from Cretaceous magmatic rocks and combine these with previously published data within the central Bangong-Nujiang suture zone in the north-central Tibetan Plateau. The integrated data update the regional tectonic...
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Journal Article
Journal: GSA Bulletin
Published: 02 June 2020
GSA Bulletin (2021) 133 (1-2): 134–148.
... two episodes of Early Jurassic gabbros from the Kaqiong terrane, a microblock within the BangongNujiang suture zone. Early gabbros (ca. 197–191 Ma) appear as lenses in the basement complex and were overprinted by amphibolite/granulite-facies metamorphism at ca. 180 Ma. Later undeformed hornblende...
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Image
Geographic and geologic setting of the Labuco area. (A) Tectonic outline of the Tibetan Plateau (ovals with numerals). (B) Simplified geological map showing the ophiolitic rocks within the Bangong-Nujiang suture zone of central Tibet (Wang et al., 2013; Zhu et al., 20015). (C) Geological map of the Labuco area. Abbreviations: BNSZ—Bangong-Nujiang suture zone; IYZSZ—Indus–Yarlung Zangbo suture zone; JSSZ—Jinsha suture zone; LSSZ—Longmu Tso–Shuanghu suture zone. Age data sources: Wu et al. (2016).
Published: 01 March 2018
Figure 1. Geographic and geologic setting of the Labuco area. (A) Tectonic outline of the Tibetan Plateau (ovals with numerals). (B) Simplified geological map showing the ophiolitic rocks within the Bangong-Nujiang suture zone of central Tibet ( Wang et al., 2013 ; Zhu et al., 20015). (C
Journal Article
Journal: GSA Bulletin
Published: 12 January 2024
GSA Bulletin (2024) 136 (7-8): 3243–3260.
... ppm, Sr/Y = 54–68), indicating that they originated from the partial melting of a thickened lower crust in a continental arc setting. Our results, in combination with a synthesis of tectonomagmatism along the Bangong-Nujiang suture zone, provide convincing evidence for subduction of an oceanic plateau...
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Journal Article
Published: 07 December 2021
Geological Magazine (2022) 159 (4): 519–534.
...Ming Zheng; Yang Song; Haifeng Li; Carl Guilmette; Juxing Tang; Qing Zhang; Zhibo Liu; Faqiao Li Abstract The BangongNujiang suture zone (BNSZ), which separates the Gondwana-derived Qiangtang and Lhasa terranes, preserves limited geological records of the BangongNujiang Ocean (BNO). The timing...
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Journal Article
Journal: GSA Bulletin
Published: 04 February 2019
GSA Bulletin (2019) 131 (7-8): 1224–1238.
...-Nujiang suture zone and its flanks, suggest that magmatic activity associated with the subduction of Bangong-Nujiang Tethyan oceanic lithosphere occurred from the Middle Triassic to Early Cretaceous. This study focused on the Dulongjiang pluton ( Fig. 1B ), a NW-SE–elongated intrusion, parallel...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 March 2018
Lithosphere (2018) 10 (2): 351–363.
...Figure 1. Geographic and geologic setting of the Labuco area. (A) Tectonic outline of the Tibetan Plateau (ovals with numerals). (B) Simplified geological map showing the ophiolitic rocks within the Bangong-Nujiang suture zone of central Tibet ( Wang et al., 2013 ; Zhu et al., 20015). (C...
FIGURES | View All (11)
Image
(A) Simplified geologic map of Tibet (modified after Pan et al., 2012; Zhu et al., 2016). JSSZ—Jinsha suture zone; NQ—Northern Qiangtang subterrane; LSSZ—Longmu Co–Shuanghu suture zone; SQ—Southern Qiangtang subterrane; BNSZ—Bangong-Nujiang suture zone; NL—Northern Lhasa subterrane; SNMZ—Shiquan River–Nam Tso mélange zone; CL—Central Lhasa subterrane; LMF—Luobadui-Milashan fault; SL—Southern Lhasa subterrane; IYZSZ—Indus–Yarlung Zangbo suture zone. (B) Geologic map of the Bangong-Nujiang suture zone (modified after Wang, et al., 2016; Zhu et al., 2016). (C) Geologic map of the Nakoulai area.
Published: 15 May 2023
Figure 1. (A) Simplified geologic map of Tibet (modified after Pan et al., 2012 ; Zhu et al., 2016 ). JSSZ—Jinsha suture zone; NQ—Northern Qiangtang subterrane; LSSZ—Longmu Co–Shuanghu suture zone; SQ—Southern Qiangtang subterrane; BNSZ—Bangong-Nujiang suture zone; NL—Northern Lhasa subterrane
Image
Plots of εNd(t) versus (87Sr/86Sr)I for mafic rocks of the Ren Co ophiolite, middle part of the Bangong–Nujiang suture zone, north-central Tibetan Plateau. Data of mafic rocks from the Bangong–Nujiang suture zone ophiolites are from Wang et al. (2016), Liu et al. (2016), and Zeng et al. (2018), the fields corresponding to mid-ocean ridge basalt (MORB) and ocean island basalt (OIB) are modified from Hofmann (2007).
Published: 10 March 2020
Figure 12. Plots of ε Nd (t) versus ( 87 Sr/ 86 Sr) I for mafic rocks of the Ren Co ophiolite, middle part of the BangongNujiang suture zone, north-central Tibetan Plateau. Data of mafic rocks from the BangongNujiang suture zone ophiolites are from Wang et al. (2016) , Liu et al. (2016