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Great Bank of Guizhou

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2017
AAPG Bulletin (2017) 101 (4): 553-562.
...Brian M. Kelley; Daniel J. Lehrmann; Meiyi Yu; Marcello Minzoni; Paul Enos; Xiaowei Li; Kimberly V. Lau; Jonathan L. Payne ABSTRACT The Late Permian to Late Triassic Great Bank of Guizhou (GBG) in southwest China is one of the few isolated carbonate platforms in the world that exposes...
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Journal Article
Journal: PALAIOS
Published: 01 August 2006
PALAIOS (2006) 21 (4): 325-343.
...JONATHAN L. PAYNE; DANIEL J. LEHRMANN; SHANNON CHRISTENSEN; JIAYONG WEI; ANDREW H. KNOLL Abstract The Great Bank of Guizhou (GBG) is an isolated Late Permian to Late Triassic carbonate platform in the Nanpanjiang Basin of Guizhou Province, southwest China. A faulted syncline exposes a cross section...
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Journal Article
Journal: PALAIOS
Published: 01 February 2006
PALAIOS (2006) 21 (1): 63-85.
... extinction on the Great Bank of Guizhou (GBG)—an isolated Late Permian to Late Triassic carbonate platform in south China. Exposure of a two-dimensional cross-section of the platform permits the comparison of faunal patterns along an environmental gradient from shallow to deep water. The diverse Late Permian...
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Journal Article
Published: 01 March 1998
Journal of Sedimentary Research (1998) 68 (2): 311-326.
...Daniel J. Lehrmann; Wei Jiayong; Paul Enos Abstract The Great Bank of Guizhou (GBG) is an exceptionally well exposed isolated Triassic platform in the Nanpanjiang Basin of South China. The platform is exhumed with its depositional profile preserved and is dissected by a faulted syncline...
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Reconstruction of key development stages of the <b>Great</b> <b>Bank</b> of <b>Guizhou</b> at Bi...
Published: 01 April 2017
Figure 3. Reconstruction of key development stages of the Great Bank of Guizhou at Bianyang with vertical exaggeration removed. Modified from Kelley (2014) . (A) Initiation and low-relief bank stages. (B) Aggrading and steepening stage. (C) Prograding reef stage. (D) High-relief escarpment stage.
Image
Macroscopic characteristics of oolites from the <b>Great</b> <b>Bank</b> of <b>Guizhou</b> (GBG)...
Published: 01 August 2012
Figure 8 Macroscopic characteristics of oolites from the Great Bank of Guizhou (GBG). (A) Outcrop photograph of dolomitized oolite with herringbone cross-beds in the lower part of the platform interior dolo-oolite at the Dajiang section. Reversing current directions indicating tidal currents
Image
Restored cross sections of the <b>Great</b> <b>Bank</b> of <b>Guizhou</b> illustrating Late Perm...
Published: 01 March 2007
Figure 15 Restored cross sections of the Great Bank of Guizhou illustrating Late Permian to Late Triassic evolution. Cross section is from the northwest-trending syncline that dissects the platform ( Figure 3 for location). For stratigraphic data, see Lehrmann et al. (1998) . (A) Lower Triassic
Image
Detailed geologic maps.  A ) <b>Great</b> <b>Bank</b> of <b>Guizhou</b> (GBG).  B ) The Pingguo ...
in > PALAIOS
Published: 01 July 2015
Fig. 2.— Detailed geologic maps. A ) Great Bank of Guizhou (GBG). B ) The Pingguo area of the Chongzuo‐Pingguo platform (CPP). Locations of maps are shown in Figure 1 . Field localities are as follows: RB = Rungbao, LB = Langbai, DJ = Dajiang, HP = Heping, DW = Dawen, DJW = Dongjiawan, XB
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Stratigraphic correlation between Meishan and the <b>Great</b> <b>Bank</b> of <b>Guizhou</b> (GB...
Published: 01 May 2009
Figure 1. Stratigraphic correlation between Meishan and the Great Bank of Guizhou (GBG), illustrating local discordance in conodont ranges implied by correlation based upon the mass-extinction horizon and δ 13 C stratigraphy. Conodont ranges as reported by Payne et al. (2007) , Jiang et al
Image
FIGURE 6 —Basal Triassic facies in the <b>Great</b> <b>Bank</b> of <b>Guizhou</b>. See  Fig. 2A ...
in > PALAIOS
Published: 01 April 2003
FIGURE 6 —Basal Triassic facies in the Great Bank of Guizhou. See Fig. 2A for locations. Fossil types indicated as follows: g=gastropod, b=bivalve, f=fusulinid, r= Renalcis . (A) Close up of wavy bedding with stromatolitic appearance in calcimicrobial framestone at Dajiang. Hammer for scale. (B
Journal Article
Journal: AAPG Bulletin
Published: 01 August 2012
AAPG Bulletin (2012) 96 (8): 1389-1414.
...Figure 8 Macroscopic characteristics of oolites from the Great Bank of Guizhou (GBG). (A) Outcrop photograph of dolomitized oolite with herringbone cross-beds in the lower part of the platform interior dolo-oolite at the Dajiang section. Reversing current directions indicating tidal currents...
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Journal Article
Journal: PALAIOS
Published: 01 March 2016
PALAIOS (2016) 31 (3): 118-121.
... roads and for quarrying. The Permian–Triassic outcrops of the Great Bank of Guizhou have been extensively sampled by multiple geological field teams. The Dajiang outcrop has been drilled and cut with rock saws very extensively along the trail where field trip groups go up through and examine...
FIGURES
Journal Article
Journal: PALAIOS
Published: 01 July 2015
PALAIOS (2015) 30 (7): 529-552.
...Fig. 2.— Detailed geologic maps. A ) Great Bank of Guizhou (GBG). B ) The Pingguo area of the Chongzuo‐Pingguo platform (CPP). Locations of maps are shown in Figure 1 . Field localities are as follows: RB = Rungbao, LB = Langbai, DJ = Dajiang, HP = Heping, DW = Dawen, DJW = Dongjiawan, XB...
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Journal Article
Published: 01 May 2015
Journal of Sedimentary Research (2015) 85 (5): 419-444.
...Marcello Minzoni; Daniel J. Lehrmann; Erich Dezoeten; Paul Enos; Paul Montgomery; Adrian Berry; Yanjiao Qin; Yu Meiyi; Brooks B. Ellwood; Jonathan L. Payne A bstract : The Yangtze Platform drowned and was buried by pelagic facies and siliciclastic turbidites in western Guizhou Province during...
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Journal Article
Journal: PALAIOS
Published: 01 April 2003
PALAIOS (2003) 18 (2): 138-152.
...FIGURE 6 —Basal Triassic facies in the Great Bank of Guizhou. See Fig. 2A for locations. Fossil types indicated as follows: g=gastropod, b=bivalve, f=fusulinid, r= Renalcis . (A) Close up of wavy bedding with stromatolitic appearance in calcimicrobial framestone at Dajiang. Hammer for scale. (B...
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Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2417
..., ( Tong Jinnan et al., 2004 ). One of the most complete, best documented, and most precisely dated Scythian sections in the world, thus a potential GSSP, lies at the margin of the isolated Great Bank of Guizhou, within the Nan-panjiang Basin on the Yangtze Craton ( Montgomery et al., 2000 ; Martin et al...
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Lithostratigraphy and chemostratigraphy of the Dajiang section, <b>Great</b> <b>Bank</b> ...
Published: 25 January 2018
Figure 2. Lithostratigraphy and chemostratigraphy of the Dajiang section, Great Bank of Guizhou, South China. EPME—end-Permian mass extinction; PTB—Permian-Triassic boundary; EP2—Early Triassic mass extinction; PDB—Peedee belemnite; I .— Isarcicella . Data were previously published in Payne et
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(A) Restored cross sections of the Early Triassic of the <b>Great</b> <b>Bank</b> of Guiz...
Published: 01 August 2012
Figure 7 (A) Restored cross sections of the Early Triassic of the Great Bank of Guizhou ( Figure 2 for location). For stratigraphic data, see Lehrmann et al. (1998) . Sb = sequence boundary; Dw = Dawen; Dj = Dajiang. (B) Stratigraphic correlation of dolo-oolite across the platform interior
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Figure  1 —Locations of the Dajiang and Bianyang sections, southern <b>Guizhou</b>...
Published: 01 September 2009
Figure 1 —Locations of the Dajiang and Bianyang sections, southern Guizhou Province, Southwest China. Early Triassic paleogeographic map of the Great Bank of Guizhou as modified from Lehrmann et al. (2001)
Journal Article
Journal: Geology
Published: 01 January 2007
Geology (2007) 35 (1): e136-e137.
.../G22827A.1 . Lehrmann D.J. Payne J.L. Enos P. Montgomery P. Wei J. Yu Y. Xiao J. Orchard M.J. 2005 , Field Excursion 2: Permian-Triassic boundary and a Lower-Middle Triassic boundary sequence on the Great Bank of Guizhou, Nanpanjiang basin, southern Guizhou Province...
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