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Wudaoliang Group

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Journal Article
Journal: GSA Bulletin
Published: 01 September 2008
GSA Bulletin (2008) 120 (9-10): 1326-1337.
...Wu Zhenhan; Patrick J. Barosh; Wu Zhonghai; Hu Daogong; Zhao Xun; Ye Peisheng Abstract Lacustrine strata of the Wudaoliang Group demonstrate that two vast lake complexes covered the central Tibetan Plateau during early Miocene time. The Wudaoliang Group, which is characterized by dolostone...
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Stratigraphic column showing the lower Miocene <b>Wudaoliang</b> <b>Group</b> in the Wuda...
Published: 01 September 2008
Figure 3. Stratigraphic column showing the lower Miocene Wudaoliang Group in the Wudaoliang and Beiluhe Basins. The upper half of the column was determined from core, taken in 2006 from borings as deep as 150 m, 2 km north of Wudaoliang; the lower half of the column is from sections measured
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Photographs showing lower Miocene lacustrine strata of the <b>Wudaoliang</b> <b>Group</b>...
Published: 01 September 2008
Figure 4. Photographs showing lower Miocene lacustrine strata of the Wudaoliang Group in the central Tibetan Plateau. (A) View northward toward marl in the central Beiluhe Basin. (B) View westward toward dolomitic limestone in the northern Beiluhe Basin. (C) View northward toward limestone
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PRESENT ELEVATIONS OF LACUSTRINE OUTCROPS OF <b>WUDAOLIANG</b> <b>GROUP</b> IN THE CENTRA...
Published: 01 September 2008
TABLE 1. PRESENT ELEVATIONS OF LACUSTRINE OUTCROPS OF WUDAOLIANG GROUP IN THE CENTRAL TIBETAN PLATEAU
Journal Article
Published: 01 November 2001
Journal of Sedimentary Research (2001) 71 (6): 971-984.
... was deposited during the first four stages 56.0-52.0, 52.0-43.0, 43.0-38.2, and 38.2-31.5 Myr; the Yaxicuo Group comprises stage 5, 31.5-30.0 Myr; the Wudaoliang Group covered the entire basin during the last stage, ∼ 23.0 to ∼ 16.0 Myr. The strata of the Fenghuoshan and Yaxicuo groups were strongly deformed...
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Journal Article
Journal: Lithosphere
Published: 18 April 2019
Lithosphere (2019) 11 (4): 524-550.
... ), and is composed of the basal Cretaceous-Eocene Fenghuoshan Group and Tuotuohe Group, the overlying Yaxicuo Group, and the capping Wudaoliang Group ( Liu and Wang, 2001 ; Li et al., 2018 ). Together, the Cenozoic strata exceed ∼5800 m in thickness ( Liu and Wang, 2001 ) and extend from the Tanggula Shan northward...
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EXTENT OF EARLY MIOCENE LAKE BASINS COVERED BY LACUSTRINE DEPOSITS OF THE W...
Published: 01 September 2008
TABLE 2. EXTENT OF EARLY MIOCENE LAKE BASINS COVERED BY LACUSTRINE DEPOSITS OF THE WUDAOLIANG GROUP IN THE CENTRAL TIBETAN PLATEAU
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Histograms showing angles of dip of Cenozoic strata in the central Tibetan ...
Published: 01 September 2008
Figure 5. Histograms showing angles of dip of Cenozoic strata in the central Tibetan Plateau. (A) Wudaoliang Group. (B) Yaxicuo Group. (C) Fenghuoshan Group.
Journal Article
Journal: GSA Bulletin
Published: 01 July 2008
GSA Bulletin (2008) 120 (7-8): 847-876.
... Shan Group ( Fig. 15 ) ( Liu et al., 2001 , 2003 ). The second stage involves lacustrine deposition of the Miocene Wudaoliang Formation (mostly limestone) ( Figure 15 ), which is flat-lying to gently folded over intensely folded Paleogene strata below ( Leeder et al., 1988 ; Liu et al., 2001 , 2003...
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Diagram showing present elevation range of outcrops of the lower Miocene la...
Published: 01 September 2008
Figure 6. Diagram showing present elevation range of outcrops of the lower Miocene lacustrine Wudaoliang Group along the Golmud-Lhasa Highway of the central Tibetan Plateau. Dots represent field locations determined by the global positioning system (GPS). Most outcrops represented are <10 km
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Correlation of measured stratigraphic sections of Cenozoic sediments in the...
Published: 01 November 2001
Figure 3 Correlation of measured stratigraphic sections of Cenozoic sediments in the Hoh Xil basin: A) and B) the Lower Eocene to Lower Oligocene Fenghuoshan Group; C) the Lower Oligocene Yaxicuo Group; D) the Lower Miocene Wudaoliang Group. The correlation among sections is based mainly
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Correlation of measured stratigraphic sections of Cenozoic sediments in the...
Published: 01 November 2001
Figure 3 Correlation of measured stratigraphic sections of Cenozoic sediments in the Hoh Xil basin: A) and B) the Lower Eocene to Lower Oligocene Fenghuoshan Group; C) the Lower Oligocene Yaxicuo Group; D) the Lower Miocene Wudaoliang Group. The correlation among sections is based mainly
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Correlation of measured stratigraphic sections of Cenozoic sediments in the...
Published: 01 November 2001
Figure 3 Correlation of measured stratigraphic sections of Cenozoic sediments in the Hoh Xil basin: A) and B) the Lower Eocene to Lower Oligocene Fenghuoshan Group; C) the Lower Oligocene Yaxicuo Group; D) the Lower Miocene Wudaoliang Group. The correlation among sections is based mainly
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Cross sections across valleys of the Tuotuohe River (A) and the Chumaerhe R...
Published: 01 September 2008
Figure 8. Cross sections across valleys of the Tuotuohe River (A) and the Chumaerhe River (B), which is a tributary of the Tongtianhe River. T 2 and T 1 —river terraces; Q 3–4 —late Pleistocene–Holocene sand and gravel; N 1wd —lower Miocene lacustrine strata of Wudaoliang Group; E 3yx —Oligocene
Journal Article
Journal: GSA Bulletin
Published: 10 October 2017
GSA Bulletin (2017) 130 (3-4): 499-521.
... stratigraphic units were recognized. From old to young, they are: Fenghuoshan, Yaxicuo, and Wudaoliang ( Fig. 2 ; Zhang and Zheng, 1994 ; Liu and Wang, 2001 ; C.S. Wang et al., 2008 ). The Fenghuoshan Group (includes three subunits, not distinguished in this study) is dominated by sandstone and conglomerate...
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Stratigraphy of the Hoh Xil Basin, showing major stratigraphic units and se...
Published: 10 October 2017
Figure 2. Stratigraphy of the Hoh Xil Basin, showing major stratigraphic units and selected sections in the East (Fenghuoshan Group, Yaxicuo Formation, and Wudaoliang Formation) and West Hoh Xil (Kangtuo Formation and Suonahu Formation) subbasins, respectively. See Figure 1B for section
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Field photographs from the central-north Tibet displaying important geologi...
Published: 18 April 2019
of the Tuotuohe Group sandstone sample WC072817-6. (G-H) Outcrops of the Yaxicuo Group and Wudaoliang Group sandstone samples WC072717-3 and WC072717-1, respectively. (I) Depositional contact between the Lower Xiaganchaigou Formation and Paleozoic rocks exposed in the Eastern Kunlun Range along the southern
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Field photographs from the central-north Tibet displaying important geologi...
Published: 18 April 2019
of the Tuotuohe Group sandstone sample WC072817-6. (G-H) Outcrops of the Yaxicuo Group and Wudaoliang Group sandstone samples WC072717-3 and WC072717-1, respectively. (I) Depositional contact between the Lower Xiaganchaigou Formation and Paleozoic rocks exposed in the Eastern Kunlun Range along the southern
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP301.12
EISBN: 9781862395497
... surface. The planation surfaces, as ‘reference planes’, suggest an increasing rate of uplift of the Tibetan Plateau during the Cenozoic. Recent research ( Wu et al. 2006 ) indicates that there were large lakes, indicated by lacustrine deposits of the Lower Miocene Wudaoliang Group (23.5–16.0 Ma; 20–5 Ma...
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Journal Article
Journal: Geosphere
Published: 01 April 2016
Geosphere (2016) 12 (2): 632-643.
... , The periglacial environment ( second edition ): London , Longman Group Limited , 341 p. Jin , H.J. , Yu , Q.H. , Wang , S.L. , Lü , L.Z. , 2008 , Changes in permafrost environments along the Qinghai-Tibet engineering corridor induced by anthropogenic activities and climate warming...
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