Hi Ijaz,
You may be interested in our paper (and its progeny in poster form) on strain partitioning and mass transport in obliquely convergent orogens (like the Himalayan syntaxes):
Whipp, D. M., Jr, Beaumont, C., & Braun, J. (2014). Feeding the “aneurysm”: Orogen-parallel mass transport into Nanga Parbat and the western Himalayan syntaxis. Journal of Geophysical Research: Solid Earth, 119(6), 5077–5096. - https://dx.doi.org/10.1002/2013JB010929
Whipp, D. M. & Beaumont, C. (2016) Orogen-parallel mass transport along the arcuate Himalayan front into Nanga Parbat and the western Himalayan syntaxis. EGU General Assembly 2016. - http://presentations.copernicus.org/EGU2016-9744_presentation.pdf
Let me know if you’re not able to access them.
Best,
Dave Whipp
> On 29 Aug 2016, at 10:34, Ijaz Ahmad <[log in to unmask]> wrote:
>
> Dear All
>
> I want to know about the recent numerical modelling techniques / computational methods being employed on kinematics of oroclinal syntaxis.
> Example: 1. Hazara-Kashmir Syntaxis, Pakistan
> 2. Nanga-Parbat Syntaxis, Pakistan
>
> Regards
>
> ijaz
--
David M. Whipp
Assistant Professor | Dept. of Geosciences and Geography | Univ. of Helsinki
+358 (0)2 941 51617 | www.helsinki.fi/geo/staff/whipp/ | @HUGeodynamics
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