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Yalong River

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Figure 6. Li Qui <b>River</b>, tributary of <b>Yalong</b> <b>River</b>. (A) LANDSAT satellite im...
Published: 01 November 2007
Figure 6. Li Qui River, tributary of Yalong River. (A) LANDSAT satellite image. (B) Simplified geologic map derived from “Geologic map of the Tibetan Plateau and adjacent areas,” compiled by Chengdu Institute of Geology and Mineral Resources and Chinese Geological Survey (map scale 1:1,500,000). (C
Image
View of Mahe colluvium in the <b>Yalong</b> <b>River</b> valley. The elevation of the mou...
Published: 01 November 2012
Figure 2 View of Mahe colluvium in the Yalong River valley. The elevation of the mountain ridge shown in this figure is about 3,730 m a.s.l., and Mahe colluvium covers an area upslope from 2,350 m a.s.l. to 3,200 m a.s.l. The light horizontal lines across the colluvium are footpaths.
Journal Article
Published: 17 February 2020
Journal of the Geological Society (2020) 177 (4): 843–854.
... the Jianchuan Basin suggest contrasting distal v. local sources, respectively. Similarly, muscovite data of the Yuanmou Basin suggest a derivation of sediments from the Yalong River, but the characteristics of the Pliocene cobbles (palaeocurrent and subrounded cobbles) suggest that these sediments are locally...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2010
Lithosphere (2010) 2 (1): 50–63.
... to the present. Apatite He and zircon He data from the middle transect (Yalong River), collected ∼225 km SSW of the Dadu data, indicate that rapid river incision of ∼0.34 ± 0.02 km/m.y. began prior to ca. 14 Ma and continued until the early Quaternary, when it increased, likely in response to local uplift...
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Journal Article
Journal: GSA Bulletin
Published: 05 June 2020
GSA Bulletin (2021) 133 (1-2): 199–211.
...-element analyses, these U-Pb ages support provenance from the Songpan-Ganzi and southern Longmenshan terranes to the north. Thus, the Paleo-Xigeda lake was fed by south-flowing paleo-Dadu and paleo-Yalong rivers during Plio-Pleistocene time. Pliocene tectonic activity on the Xianshuihe-Daliangshan...
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Image
Reconstruction of the Palaeo-Yangtze <b>River</b>. ( a ) In the pre-Pliocene, prio...
Published: 17 February 2020
Fig. 8. Reconstruction of the Palaeo-Yangtze River. ( a ) In the pre-Pliocene, prior to capture, the Palaeo-Jinsha and Palaeo-Yalong rivers flowed into the Palaeo-Red River. ( b ) After capture in the Pliocene, the Palaeo-Jinsha and Palaeo-Yalong rivers were redirected to flow east to form
Image
Figure 2. Longitudinal <b>river</b> profiles of the Dadu <b>River</b> (A) and <b>Yalong</b> Rive...
Published: 01 November 2007
Figure 2. Longitudinal river profiles of the Dadu River (A) and Yalong River (B), extracted from ∼90-m resolution Shuttle Radar Topography Mission (SRTM) data. In areas where SRTM data are missing within the river gorge, the profile is inferred from adjacent points. Solid-gray lines drawn above
Journal Article
Journal: GSA Bulletin
Published: 01 November 2007
GSA Bulletin (2007) 119 (11-12): 1462–1476.
...Figure 6. Li Qui River, tributary of Yalong River. (A) LANDSAT satellite image. (B) Simplified geologic map derived from “Geologic map of the Tibetan Plateau and adjacent areas,” compiled by Chengdu Institute of Geology and Mineral Resources and Chinese Geological Survey (map scale 1:1,500,000). (C...
FIGURES | View All (10)
Journal Article
Journal: GSA Bulletin
Published: 01 September 2011
GSA Bulletin (2011) 123 (9-10): 1966–1987.
... sediments deposited on the older plateau surface suggest that rapid denudation occurred from the Miocene to Holocene. Other evidence of significant Cenozoic denudation comes from river valleys, in particular, the Yalong River valley, where incision was initiated in the Oligocene to Miocene (28–12 Ma...
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Journal Article
Published: 01 November 2012
Environmental and Engineering Geoscience (2012) 18 (4): 357–369.
...Figure 2 View of Mahe colluvium in the Yalong River valley. The elevation of the mountain ridge shown in this figure is about 3,730 m a.s.l., and Mahe colluvium covers an area upslope from 2,350 m a.s.l. to 3,200 m a.s.l. The light horizontal lines across the colluvium are footpaths. ...
FIGURES | View All (11)
Image
Evolution of the Xigeda lake and reversal of the Middle Yangtze at the sout...
Published: 05 June 2020
Figure 8. Evolution of the Xigeda lake and reversal of the Middle Yangtze at the southern margin of Tibetan Plateau. (A) Pre- ca. 4.2 Ma ( Yao et al., 2007 ), the paleo-Yalong, Dadu, and Middle Yangtze rivers drain into the paleo–Lower Yangtze, and the paleo-Yalong river supplies Songpan-Ganze
Image
Reassessment of the detrital zircon data from  Kong  et al.  (2009) . ( a )...
Published: 17 February 2020
cluster closely together in the MDS. It should be noted that samples from the Jinsha valley plot far away from the Yalong samples, but close to that of the upper Jinsha River (Shigu sample). The red squares and yellow dots represent samples from the Jinsha River valley and modern sediments from Jinsha
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( a – c ) Muscovite geochemistry of samples from the Jianchuan Basin, Yuanm...
Published: 17 February 2020
Fig. 6. ( a – c ) Muscovite geochemistry of samples from the Jianchuan Basin, Yuanmou Basin and Panzhihua area. Muscovite Si and Mg concentration of Jinsha River near the Yuanmou Basin (JS; purple polygon), the first bend (SG; yellow polygon), the Yalong River (YLJ; light cyan polygon), Yangbi
Image
Regional topography and <b>rivers</b>. (A) Overview map of regional topography and...
Published: 01 February 2010
: horizontal scale is different for each profile. Stars indicate the locations of towns Danba (Db) and Jinchuan (Jn) on the Dadu River profile, and the confluence of the Li Qui River (LQ) with the Yalong trunk river on the Yalong River profile.
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Muscovite  40 Ar/ 39 Ar age distributions of samples from the Panzhihua and...
Published: 17 February 2020
Fig. 5. Muscovite 40 Ar/ 39 Ar age distributions of samples from the Panzhihua and Yuanmou areas. The black lines and shaded areas are respectively KDEs and PDPs of muscovites. Muscovite ages of the Yalong River are from Sun et al. (2016) . The difference in age scale (0–1000 Ma
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A: Yangtze catchment. G1–G8 indicate hydrological gauging stations in which...
Published: 01 November 2010
Figure 1. A: Yangtze catchment. G1–G8 indicate hydrological gauging stations in which sediment and discharge data were recorded. 1—Jinsha River; 2—Yalong River; 3—Dadu River; 4—Min River; 5—Tuo River; 6—Jialing River; 7—Han River; 8—Wu River; 9—Dongting Lake; 10—Poyang Lake; 11—Tai Lake. B
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Figure 3. Landslide dam sites (active  and  inferred) within the Dadu and Y...
Published: 01 November 2007
Figure 3. Landslide dam sites (active and inferred) within the Dadu and Yalong river gorges, superimposed on a shaded-relief rendering of the region. Identification based on morphology and characteristics of landslide deposits (typically >0.25 km 3 ) and landslide dam deposits (lake sediments
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Probability distribution diagrams (KDPs) of U-Pb ages of detrital zircon al...
Published: 05 June 2020
Ma zircon age peak in the Upper Yangtze and Red Rivers during the Pliocene. References for modern detrital U-Pb age distributions are for the Yalong and Dadu rivers ( Yang et al., 2012 ; He et al., 2013 ); Upper Yangtze ( van Hoang et al., 2009 ; Yang et al., 2012 ; He et al., 2013 ); Middle
Image
Oblique view northwest, along strike, of structure draped over digital elev...
Published: 01 September 2011
in the Yalong river valley in the right of the diagram (J, K, N, S).
Journal Article
Journal: GSA Bulletin
Published: 01 March 2000
GSA Bulletin (2000) 112 (3): 413–423.
... zone, there are several left-lateral stream offsets, but they are not as consistent as along the northern strand. The southern strand ends before reaching the Yalong River. Historical records since A.D. 1738 list 21 earthquakes along the Ganzi fault zone: M > 4.7 (17 events), M = 6 (3), and M...
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