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Not to beat a dead horse, but this week's issue of Science has something to say in this matter.
http://www.sciencemag.org/content/346/6212/978.short

On Mon, Nov 17, 2014 at 10:45 PM, gapais <[log in to unmask]> wrote:
Yes, The paper by Peter Molnar is actually quite clear and should have at stoped the polemic!

Concerning recent exchanges about exhumation requiring erosion, or the role of the STD in the Himalayas, may I recommand also to have a look at two papers, one old, and one quite recent:
- Duretz et al., 2010, Lithos. The paper, based on analogical modelling, shows that exhumation of lower weak crust does not require erosion (experiments were done without erosion, and the lower crust rised up to the upper crust just by « channel flow », a feature of course not suggested by numerical models…
-Gapais et al, 1992. Synconvergence spreading of the Higher Himalaya Crystalline in Ladakh. Tectonics, 11: 1045-1056. There, we argued that crustal extension, accommodated by the Zanskar shear zone, might account for the exhumation of the Higher Himala Crystalline, spreading in between an active thrust to the South (the MBT) and a major detachement to the North (please remember that the STD juxtaposes high-grade lower crustal rocks with unmetamorphosed sediments!)
A good friend wrote one day in a review of a paper that I had to edit: if you are wright, I am the Dalai Lama! (I do not remember the precise reason for this comment)
I would use this sentence with great pleasure concerning the debate on the role of climate on orogens. Eclogites do not need rain to crop out!

Cheers
Denis

Le 17 nov. 2014 à 02:21, John Suppe <[log in to unmask]> a écrit :

Dear all,
At this point in the fascinating discussion, I’m guessing that some of you might be interested in Peter Molnar’s short polemic of a few years ago…

Peter Molnar, 2009, The state of interactions among tectonics, erosion, and climate: A polemic.  GSA Today, v. 19, no.7, 44-45
www.geosociety.org/gsatoday/archive/19/7/.../i1052-5173-19-7-44.pdf
        •
        •

John

On Nov 16, 2014, at 6:12 PM, Peter D Clift <[log in to unmask]> wrote:

> Dear Christopher
>
> Thanks for your views and comments which I almost entirely agree with. I am not arguing that you have to believe in channel flow in order to believe in the idea that climate partly controls orogenic structure, via the medium of erosion. It is just one example of how that sort of process could work. Focused erosion would also result in deep exhumation in a wedge type model too. I am not qualified to judge between the two myself but it does seem hard to imagine deep exhumation with strong erosion, particularly in a compressional setting. There are clearly some exceptions but generally I think this must be so. Once you you accept that exhumation is governed by erosion and differential exhumation must result in faulting then it would follow that the location of major faults bounding zones of contrasting exhumation are at least partly driven by climatic patterns and/or river drainage patterns. We don’t need channel flow to believe that
>
> best wishes
> Peter
>
>
>> On Nov 15, 2014, at 6:04 AM, Christopher Spencer <[log in to unmask]> wrote:
>>
>> Dear Peter,
>>
>> I would like to take this opportunity to enter the foray. Channel flow is a model. To say that "Channel Flow only works when..." assumes the model is correct. And simply because the channel flow model calls for an erosive driver does not have anything to do with reality. Data constrain models which inform our conclusions and not the other way around. Models are generated to elucidate the temporal and spacial relationships between various complex variables and boundary conditions. In theory, the initial conditions should be based on data collected in nature and the results of the model should be testable through the collection of more focused data. Channel flow, by the authors own admission is a "conceptual model" and cannot be tested, or as Becky put it, "Imagine flying in a conceptual airplane?" Quantification of a conceptual model (as is done with channel flow) is often seen as a window into unknown or a "proof of concept". and despite the apparent agreement with a few first-order tectonic features we must remember that science cannot prove any concept and yet it is our prerogative to disprove models and move on.
>> The dogma that has surrounded the channel flow models is (at least to my young mind) unprecedented in the field of geodynamics and tectonics. Never has a near religious fervor surrounded a model for which several (seemingly ignored) alternatives have been produced with the aim to disprove the model of channel flow. There remain many observations called for in the model that are unseen in reality, e.g. the lack of arc/suture/ophiolitic material in the Greater Himalaya, for how could a midcrustal channel originate underneath Tibet and pierce the suture zone without incorporating any of this material.
>> Before claiming that because we don't see it in the model and therefore it cannot be true, let us (re)evaluate the viability of the model and its ability to explain what nature has revealed at the surface.
>>
>> Respectfully,
>> Christopher Spencer
>>
>> ____
>> Postdoctoral researcher
>> NERC Isotope Geoscience Laboratories
>> Keyworth, UK NG125GG
>>
>> On Sat, Nov 15, 2014 at 9:20 AM, Peter D Clift <[log in to unmask]> wrote:
>> I just wanted the chance to reply to some of Mike’s points
>>>
>>> First the MCT (and STD) are not active faults; they were during the Miocene but are they not active now
>>
>> That’s true but there is evidence that thrust faulting is focused by erosion patterns in the recent past and could have done so during the Miocene too
>>
>>> (likewise Channel flow, the exhumation of a layer of partially melted mid-crust in the Himalaya during the Miocene is probably not active now). The active faults are along the southern boundary of the Himalaya (MBT, MFT).
>>
>> Indeed, but that does not mean that the MCT was not climatically located when it was active, Indeed it is hard to see how it could not have been since the Channel Flow only works when erosion removes the shallower rocks allowing the channel to flow.
>>>
>>> Second Rainfall most certainly did not control initiation of the MCT (or the STD). Tectonics controlled this, not Rain.
>>
>> That is not the way that the Channel Flow model is described.  The channel onlu flows because of the gravitational potential caused by the thicker than normal crust but no exhumation would occur without the erosion along the mountain front.
>>
>>> Earthquakes generally initiate faults and most earthquakes initiate from above the brittle-ductile transition and at depths down to ~30-40 km and propagate up through the brittle crust. The MCT and STD initiated well down into the ductile mid-lower crust.
>>> You are surely not saying that rain/climate penetrates down there (I hope!).
>>
>> I might be.  To be precise I am arguing that stresses caused by surface processes (erosion) result in rock uplift which has be compensated for throughout the crust. At shallow levels this results in faulting by these must extend to ductile shear zones at depth. It is only the focused erosion that allows the Greater Himalayan slab to flow so without that erosion there would be no large thrust like the MCT (or STD). This is why we only see these structures on the wet south side of Tibet and not on the north side.
>>
>>> The climatic differences between the two Himalayan syntaxes are enormous, both are controlled entirely by tectonic processes with maximum compressive stress in all directions accounting for the rapid vertical exhumation of rocks and the young metamorphic ages in the syntaxes. The big rivers (Bhramaputra in the east; Indus in the west) cut at right angles across both syntaxes, across the areas of high uplift and exhumation. The rivers have nothing whatever to do with the rock uplift (or surface uplift) of either syntaxis. Tectonics control these structures entirely.
>>
>> I agree that tectonic forces are responsible for driving the rock uplift but without the erosional influence I don’t see how you would explain the deep exhumation unless you think there are large extensional faults in the syntaxes too.
>>>
>>> It rains like hell in the Amazon (and in Oxford sometimes) but I see no major MCT type fault induced here.
>>
>> No of course not because we need rock uplift as well as erosion to generate significant exhumation and thus the development of major faults. However, rock uplift in the absence of erosion does not cause exhumation which is a signature feature of the Greater Himalaya
>>
>>> Rainfall has nothing to do with mountain building. Tectonics make mountains and rain etc erodes them away.
>>
>> I don’t agree with that at all. Compressional tectonics causes crustal thickening and both rock and surface uplift but without erosion, modulated by climate there is no exhumation until the orogenic belt experiences large scale gravitational collapse.Thus Tibet is the product of plate tectonic forces but the Greater Himalayas are only possible in the form that we know them because of surface processes
>>
>>> Likewise in the Karakoram exhumation of kyanite and sillimanite grade rocks formed at depths of 12 kbar or more are not controlled by glaciation. Glaciers eroded the top 5-10 km of present day topography but they cannot be responsible for exhumation of deep crustal rocks from 12 kbar.
>>
>> Then the exhumation must be caused by other erosional processes unless you think that normal faulting is dominating. I would curious to know why you think that glaciers only account for 5-10 km of erosion. If the rocks were metamorphosed at 12 km then you have to remove that overburden to get them exposed. That seems to require either extensional faulting or erosion.  You choose.
>>
>>> Greenland, Northern North America and Siberia are covered in huge ice sheets and glaciers, theres no active mountain building going on there.
>>>
>> No, because there is no significant rock uplift to drive deep exhumation
>>
>>> Whatever induced the Asian monsoon (Tibetan plateau uplift?) and when noone really knows, but for sure the Himalaya are the northern barrier to the monsoonal rainfall today.
>>
>> Indeed they are
>>
>>> Rock exhumation rates are pretty similar along the length of the Greater Himalaya (and timing too)
>>
>> This I do not agree with. Ar-Ar cooling ages are generally younger in the east than in the western Greater Himalaya. To my mind this is because the Channel Flow is faster in the east than the west, driven by the heavier rain fall I would suggest.
>>
>>> but in the east it is wet and rainy and in the west (Ladakh, Zanskar, Nanga Parbat) dry.
>>
>> We are really only talking about Zanskar here, and that has some of the oldest cooling ages in the Greater Himalaya because it is drier and there exhumes more slowly that the eastern ranges
>>
>>> Thus in my opinion Tectonics initiates and controls rock uplift
>>
>> I agree 100%
>>
>>> and ductile shear zones, faults and mountain building along the Himalaya, not Rain, Glaciers or Climate.
>>
>> This I do not agree with. Tectonics can do all those things but surface processes can play a role too in focusing where rock uplift occurs and thus where large faults that allow deep exhumation develop. Without surface processes, modulated by climate there can be little exhumation in compression systems.
>> best wishes. I am enjoying the debate
>> Peter
>>
>>
>> ======================
>>
>> Peter D. Clift
>> Charles T. McCord Chair in Petroleum Geology,
>> Department of Geology and Geophysics,
>> E235 Howe-Russell-Kniffen Geoscience Complex
>> Louisiana State University,
>> Baton Rouge, LA 70803,
>> USA
>>
>> Tel: +1 225-578-2153
>> Fax: +1 225-578-2302
>> Email: [log in to unmask]
>>
>> http://www.geol.lsu.edu/pclift/pclift/Home.html
>>
>> Attend AGU Chapman meeting "Evolution of the Asian monsoon and its impact on landscape, environment and society”, June 15-19th 2015, Hong Kong
>>
>> http://www.geol.lsu.edu/pclift/Monsoon_AGU_Chapman_Meeting/Welcome.html
>>
>>
>
>
>
> ======================
>
> Peter D. Clift
> Charles T. McCord Chair in Petroleum Geology,
> Department of Geology and Geophysics,
> E235 Howe-Russell-Kniffen Geoscience Complex
> Louisiana State University,
> Baton Rouge, LA 70803,
> USA
>
> Tel: +1 225-578-2153
> Fax: +1 225-578-2302
> Email: [log in to unmask]
>
> http://www.geol.lsu.edu/pclift/pclift/Home.html
>
> Attend AGU Chapman meeting "Evolution of the Asian monsoon and its impact on landscape, environment and society”, June 15-19th 2015, Hong Kong
>
> http://www.geol.lsu.edu/pclift/Monsoon_AGU_Chapman_Meeting/Welcome.html
>


Denis Gapais
Géosciences Rennes
UMR 6118 CNRS
Université de Rennes 1
35042 Rennes cedex
France
phone 33 2 23 23 67 36
mobile 33 6 20 01 58 69
fax 33 2 23 23 60 97