Divergent metamorphism within the Namche Barwa Complex, the Eastern Himalaya, southeast Tibet, China ‐ Insights from in‐situ U‐Th‐Pb dating of metamorphic monazite

Author(s):  
Tao Peng ◽  
Axel Gerdes ◽  
Ling‐Sen Zeng ◽  
Leo J. Millonig ◽  
Richard Albert ◽  
...  
2016 ◽  
Vol 57 (71) ◽  
pp. 289-294 ◽  
Author(s):  
Phuntsho Tshering ◽  
Koji Fujita

AbstractThis study presents the first decadal mass-balance record of a small debris-free glacier in the Bhutan Himalaya, where few in situ measurements have been reported to date. Since 2003 we have measured the mass balance of Gangju La glacier, which covers an area of 0.3km2 and extends from 4900 to 5200ma.s.l., using both differential GPS surveys (geodetic method) and stake measurements (direct method). The observed mass balance ranged from –1.12 to –2.04mw.e. a–1 between 2003 and 2014. The glacier exhibited much greater mass loss than neighbouring glaciers in the eastern Himalaya and southeastern Tibet, which are expected to be sensitive to climate change due to the monsooninfluenced humid climate. Observed mass-balance profiles suggest that the equilibrium-line altitude has been higher than Gangju La glacier since 2003, implying that the entire glacier has experienced net ablation for at least the past decade.


2011 ◽  
Vol 307 (3-4) ◽  
pp. 323-333 ◽  
Author(s):  
E. Enkelmann ◽  
T.A. Ehlers ◽  
P.K. Zeitler ◽  
B. Hallet

Geology ◽  
2020 ◽  
Vol 48 (12) ◽  
pp. 1139-1143
Author(s):  
Gwladys Govin ◽  
Peter van der Beek ◽  
Yani Najman ◽  
Ian Millar ◽  
Lorenzo Gemignani ◽  
...  

Abstract The Himalayan syntaxes, characterized by extreme rates of rock exhumation co-located with major trans-orogenic rivers, figure prominently in the debate on tectonic versus erosional forcing of exhumation. Both the mechanism and timing of rapid exhumation of the Namche Barwa massif in the eastern syntaxis remain controversial. It has been argued that coupling between crustal rock advection and surface erosion initiated in the late Miocene (8–10 Ma). Recent studies, in contrast, suggest a Quaternary onset of rapid exhumation linked to a purely tectonic mechanism. We report new multisystem detrital thermochronology data from the most proximal Neogene clastic sediments downstream of Namche Barwa and use a thermo-kinematic model constrained by new and published data to explore its exhumation history. Modeling results show that exhumation accelerated to ∼4 km/m.y. at ca. 8 Ma and to ∼9 km/m.y. after ca. 2 Ma. This three-stage history reconciles apparently contradictory evidence for early and late onset of rapid exhumation and suggests efficient coupling between tectonics and erosion since the late Miocene. Quaternary acceleration of exhumation is consistent with river-profile evolution and may be linked to a Quaternary river-capture event.


Lithos ◽  
2020 ◽  
Vol 362-363 ◽  
pp. 105511
Author(s):  
Tao Peng ◽  
Ling-Sen Zeng ◽  
Li-E Gao ◽  
Axel Gerdes ◽  
Jia-Hao Gao ◽  
...  
Keyword(s):  
T Path ◽  

2021 ◽  
Author(s):  
Rong Yang ◽  
et al.

Analytical approaches used in this study, analyses parameters, and resulting data.<br>


2020 ◽  
Author(s):  
Gwladys Govin ◽  
Peter van der Beek ◽  
et al.

Methods descriptions, analytical data, and inversion results. <br>


2020 ◽  
Author(s):  
Gwladys Govin ◽  
Peter van der Beek ◽  
et al.

Methods descriptions, analytical data, and inversion results. <br>


Lithos ◽  
2018 ◽  
Vol 320-321 ◽  
pp. 454-469 ◽  
Author(s):  
Tao Peng ◽  
Ling-Sen Zeng ◽  
Li-E Gao ◽  
Axel Gerdes ◽  
Jia-Hao Gao ◽  
...  
Keyword(s):  
T Path ◽  

2018 ◽  
Vol 722 ◽  
pp. 43-52 ◽  
Author(s):  
Rong Yang ◽  
Frédéric Herman ◽  
Maria Giuditta Fellin ◽  
Colin Maden

2018 ◽  
Vol 93 (1) ◽  
pp. 393-409 ◽  
Author(s):  
R. K. Sharma ◽  
Pranay Pradhan ◽  
N. P. Sharma ◽  
D. G. Shrestha

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