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Rongmawa Formation

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Non-normalized kernel density estimate (KDE) plots of individual <b>Rongmawa</b> F...
in > Geology
Published: 06 September 2019
Figure 2. Non-normalized kernel density estimate (KDE) plots of individual Rongmawa Formation (southern Tibet) samples (black); composite KDEs of Xigaze Group forearc basin samples (gray) separated by geographic region ( Fig. 1 ) and proximity to trench basin samples on MDS plot ( Fig. 3 ); KDE
Image
Paired detrital zircon Hf isotopic data and U-Pb ages from our <b>Rongmawa</b> For...
in > Geology
Published: 06 September 2019
Figure 4. Paired detrital zircon Hf isotopic data and U-Pb ages from our Rongmawa Formation (southern Tibet) samples ( n = 50; pink circles) plotted on Hf evolution diagram and compared against Lhasa terrane reference data from Zhu et al. (2011) (blue symbols); 95% contour is shown for three
Image
Multidimensional scaling (MDS;  Vermeesch, 2013 ) results for all Xigaze Gr...
in > Geology
Published: 06 September 2019
Figure 3. Multidimensional scaling (MDS; Vermeesch, 2013 ) results for all Xigaze Group forearc strata and Rongmawa Formation trench basin strata (southern Tibet), with interpreted boundary (dashed line) between samples displaying local Gangdese magmatic arc provenance and samples displaying
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 23 March 2018
Lithosphere (2018) 10 (3): 446–459.
... ( Garzanti and Van Haver, 1988 ) and the Rongmawa Formation in Ngamring, south Tibet ( Cai et al., 2012 ). This may be ascribed to poor preservation owing to strong multiple deformation during tectonic accretion and final collision, and to much smaller size and only local exposure relative to the thick...
FIGURES | View All (7)
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Ternary diagrams showing the petrographic composition of turbiditic sandsto...
Published: 23 March 2018
—volcanic; Ls—sedimentary). Data for the Nindam Formation and mélange from Garzanti and Van Haver (1988) and for the Rongmawa Formation from Cai et al. (2012) .
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Tectonic map of the Lhasa terrane and Yarlung suture zone in south-central ...
in > Geology
Published: 06 September 2019
sample locations are shown in green ( Orme et al., 2015 ; Orme and Laskowski, 2016 ), whereas Rongmawa Formation (trench basin) samples are shown in pink (this study; Metcalf and Kapp, 2019 ). Major rivers and locations of towns were traced from the Esri World Topographic Map ( http://arcg.is/0r4aaH ).
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Age patterns (A–C) and Hf isotope signatures (F–H) of detrital zircons in s...
Published: 23 March 2018
), Rongmawa Formation ( Cai et al., 2012 ), Gangdese magmatic arc (E, J; Zhu et al., 2008 ; Wen et al., 2008 ; Ji et al., 2009 , and references therein), and central Lhasa magmatic rocks ( Zhu et al., 2011 and references therein) and Carboniferous–Lower Cretaceous strata ( Leier et al., 2007 ; Gehrels et
Series: Geological Society, London, Special Publications
Published: 08 October 2019
DOI: 10.1144/SP483.12
EISBN: 9781786204523
... in the siliciclastic-matrix mélange ( Fig. 3b ). The Rongmawa Formation sandstones have Cretaceous MDAs of between 90 and 85 Ma with 22–35% of the grains dated being <200 Ma ( Figs 2 , 3 & 9 ). Fig. 9. Detrital zircon U–Pb ages from sandstones in the Tethyan Himalayan strata, siliciclastic-matrix...
FIGURES | View All (14)
Journal Article
Journal: Geology
Published: 06 September 2019
Geology (2019) 47 (11): 1029–1033.
...Figure 2. Non-normalized kernel density estimate (KDE) plots of individual Rongmawa Formation (southern Tibet) samples (black); composite KDEs of Xigaze Group forearc basin samples (gray) separated by geographic region ( Fig. 1 ) and proximity to trench basin samples on MDS plot ( Fig. 3 ); KDE...
FIGURES | View All (4)