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Linzhou Basin

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A composite column of Cretaceous strata in the <b>Linzhou</b> <b>Basin</b> showing strati...
Published: 08 April 2020
Figure 3. A composite column of Cretaceous strata in the Linzhou Basin showing stratigraphic range of measured sections. Black dots indicate samples for detrital zircon U–Pb analysis; shown for each are the youngest single grain age (YSG) and the YC1σ(2+) age [mean average of the youngest cluster
Image
Sedimentary features of Lower Cretaceous strata in the <b>Linzhou</b> <b>Basin</b>. Strat...
Published: 08 April 2020
Figure 7. Sedimentary features of Lower Cretaceous strata in the Linzhou Basin. Stratigraphic position of each photo is shown beside the stratigraphic logs in Figure 4 . (A) Calcareous nodules in red mudstone; (B) planar cross stratification; (C) trough cross stratification; (D) unidirectional
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Schematic diagrams show sedimentary and provenance evolution of the Cretace...
Published: 08 April 2020
Figure 12. Schematic diagrams show sedimentary and provenance evolution of the Cretaceous Linzhou Basin. Broad arrows indicate transport direction of sediments. Detailed explanation is given in text (see “Sedimentary and Provenance Evolution of the Linzhou Basin” section).
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Comparisons of the Cretaceous strata in the Xigaze forearc <b>basin</b>, <b>Linzhou</b> B...
Published: 01 July 2015
Figure 14. Comparisons of the Cretaceous strata in the Xigaze forearc basin, Linzhou Basin, southern Nima Basin, Selin Co Basin, and Coqen Basin (this study). The strata and time scale in ordinate are referred to in An et al. (2014) , Leier et al. (2007a) , DeCelles et al. (2007b) , and Zhang
Journal Article
Journal: GSA Bulletin
Published: 08 April 2020
GSA Bulletin (2020) 132 (11-12): 2432–2454.
...Figure 3. A composite column of Cretaceous strata in the Linzhou Basin showing stratigraphic range of measured sections. Black dots indicate samples for detrital zircon U–Pb analysis; shown for each are the youngest single grain age (YSG) and the YC1σ(2+) age [mean average of the youngest cluster...
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Series: Geological Society, London, Special Publications
Published: 08 October 2019
DOI: 10.1144/SP483.14
EISBN: 9781786204523
... in the Linzhou Basin was active from 60.2 to 52.3 Ma, rather than 69–44 Ma as previously estimated. During 120–75 Ma, Gangdese Batholith magmatism migrated from south to north, arguing against rollback of the downgoing, north-dipping Neo-Tethyan oceanic lithosphere for the generation of the 90 ± 5 Ma magmatic...
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Age and LBF biozone distribution of mid-Cretaceous limestones from the Xiga...
Published: 01 April 2017
Figure 14.  Age and LBF biozone distribution of mid-Cretaceous limestones from the Xigaze basin, the Linzhou basin and the Coqen basin in the Lhasa terrane. Sample numbers correspond to those in Figures 2 – 6 .
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(A) Geological map of the study area (after the Chinese 1:250,000 Lhasa geo...
Published: 08 April 2020
Figure 2. (A) Geological map of the study area (after the Chinese 1:250,000 Lhasa geological map). (B) Geological map of the Linzhou Basin (after He et al., 2007 ) showing locations of measured sections.
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Tectonic subsidence and sedimentation rate in the Lower Cretaceous of the L...
Published: 08 April 2020
Figure 9. Tectonic subsidence and sedimentation rate in the Lower Cretaceous of the Linzhou Basin. The data set used for calculations is provided in Table DR2 (see footnote 1 ); method after Allen and Allen (2005) . The long-term eustatic curve is from Haq (2014) .
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Stratigraphic and facies comparisons are shown for Cretaceous strata in the...
Published: 30 October 2020
Figure 10. Stratigraphic and facies comparisons are shown for Cretaceous strata in the Xigaze Forearc Basin ( An et al., 2014 ), Linzhou Basin ( Leier et al., 2007a ), Coqen Basin ( Sun et al., 2015a ), Selin Co Basin ( Zhang et al., 2011 ), Nima Basin ( Kapp et al., 2007a ; Lai et al., 2019a
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Cretaceous paleogeographic evolution and topographic growth of the Lhasa bl...
Published: 08 April 2020
reaching the Xigaze Forearc Basin ( An et al., 2014 ). Volume volcanic detritus from the Gangdese arc was deposited in the Linzhou Basin. (C) Late Cenomanian–Early Turonian (ca. 96–90 Ma): onset of contractional deformation caused deposition of continental conglomerates (Jinzhushan and Daxiong Formations
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A  Simplified tectonic map of the Tibetan Plateau and adjacent regions, sho...
Published: 01 April 2017
of the Lhasa terrane modified from Kapp et al. (2005) . SGAT—Shiquan-Gaize-Amdo thrust; GST—Gaize–Selin Co thrust; GLT—Gugu La thrust; ST—Shibaluo thrust; ELT—Emei La thrust; GT—Gangdese thrust system; GCT—Great Counter thrust. Section 1 from the Xigaze Basin; Sections 2 and 3 from the Linzhou Basin; Sections
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(A) Tectonic framework of the Tibetan Plateau (adapted from  Kapp et al., 2...
Published: 30 October 2020
—Bangong-Nujiang Suture Zone; SNMZ—Shiquan River-Nam Tso Mélange Zone; LMF—Luobadui-Milashan Fault; IYZSZ—Indus-Yarlung Zangbo Suture Zone; STDS—South Tibetan Detachment System; TZB—Tangza Basin; CQB—Coqen Basin; NMB—Nima Basin; XFB—Xigaze Forearc Basin; SCB—Selin Co Basin; BGB—Baingoin Basin; LZB—Linzhou
Journal Article
Published: 01 April 2017
Journal of Foraminiferal Research (2017) 47 (2): 188–207.
...Figure 14.  Age and LBF biozone distribution of mid-Cretaceous limestones from the Xigaze basin, the Linzhou basin and the Coqen basin in the Lhasa terrane. Sample numbers correspond to those in Figures 2 – 6 . ...
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Journal Article
Published: 01 June 2021
Russ. Geol. Geophys. (2021) 62 (6): 666–684.
... model age is 928–1042 Ma, and the crustal model age is 1394–1601 Ma. Theoretical research on the Gangdese Belt Linzizong volcanic rocks has intensified in recent years, and interest in contemporaneous intrusions has grown. For example, granite porphyry at the western margin of the Linzhou Basin...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2015
GSA Bulletin (2015) 127 (7-8): 1001–1020.
...Figure 14. Comparisons of the Cretaceous strata in the Xigaze forearc basin, Linzhou Basin, southern Nima Basin, Selin Co Basin, and Coqen Basin (this study). The strata and time scale in ordinate are referred to in An et al. (2014) , Leier et al. (2007a) , DeCelles et al. (2007b) , and Zhang...
FIGURES | View All (14)
Journal Article
Journal: GSA Bulletin
Published: 30 October 2020
GSA Bulletin (2021) 133 (5-6): 1283–1300.
...Figure 10. Stratigraphic and facies comparisons are shown for Cretaceous strata in the Xigaze Forearc Basin ( An et al., 2014 ), Linzhou Basin ( Leier et al., 2007a ), Coqen Basin ( Sun et al., 2015a ), Selin Co Basin ( Zhang et al., 2011 ), Nima Basin ( Kapp et al., 2007a ; Lai et al., 2019a...
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Maps of the sampled regions. (A) Regional Landsat image of the Tibetan Plat...
Published: 14 September 2017
Figure 1. Maps of the sampled regions. (A) Regional Landsat image of the Tibetan Plateau (adapted from Currie et al., 2016 ). (B) Geologic map of the Linzhou-Penbo region, including the Nianbo type section. Map is based on and geochronology is sourced from Ding et al. (2014) and He et al
Journal Article
Journal: Geology
Published: 01 March 2017
Geology (2017) 45 (3): 215–218.
...: Paleoelevation record from the Paleocene–Eocene Linzhou Basin : Earth and Planetary Science Letters , v. 392 , p. 250 – 264 , doi:10.1016/j.epsl.2014.01.045. Fang , A.M. , Yan , Z. , Liu , X.H. , Pan , Y.S. , and Li , J.L. , 2005 , The flora of the Liuqu formation in South Tibet...
Journal Article
Journal: Economic Geology
Published: 01 January 2009
Economic Geology (2009) 104 (1): 127–136.
... , Geochronology, geochemistry and implications of Au-mineralized porphyries in the Linzhou basin, Gangdese belt, Tibet , in Mao , J. , and Bierlein , F.P. , eds., Meeting the Global Challenge: Proceedings of the Eighth Biennial SGA Meeting , Beijing, China , August 18–21, 2005, Springer-Verlag...
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