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Hi Mike,

The impulse to chide you (and share it with the list) for clicking the 
"bonehead reply" button is overwhelming and irresistible. Your paper 
does sound good, however - hope nobody poaches the idea.

Cheers,  Bob T.

Michael Brown wrote:
> Dear Santosh:
>  
> Thanks for the initiative to produce a Special Volume as a tribute to 
> Miyashiro's vision and contributions to various fields in the Earth 
> Sciences.  I am interested in possibly contributing a paper with a 
> title something along the lines of "Paired Metamorphic Belts 
> Revisited".  This paper would summarize prescient features of 
> Miyashiro's original contribution in 1960, how our understanding of 
> paired metamorphic belts has evolved during the subsequent half 
> century, and how the concept may be extended back through time given 
> due consideration to increased heat production and differences in the 
> style of metamorphism.
>  
> I am very strongly motivated to contribute to this volume, since I 
> have a long-standing interest in paired metamorphic belts as well as 
> how the concept might be applied earlier in Earth history.  However, I 
> would like to know the potential time frame for producing the volume 
> to ensure that I can meet the commitment.  I look forward to hearing 
> from you further with respect to deadlines.
>  
> My possible contribution is described in more detail below.
>  
> With best regards,
> Yours sincerely,
> Mike
>  
>  
> *Paired Metamorphic Belts Revisited
> * 
> Michael Brown, Department of Geology, University of Maryland, College 
> Park, MD 20742-4211, USA
>  
> Classic paired metamorphic belts in which an inboard high dT/dP 
> metamorphic belt is juxtaposed against an outboard low dT/dP 
> metamorphic belt along a tectonic contact are found in accretionary 
> orogens of the circum-Pacific. Generally, they appear to result from 
> tectonic juxtaposition of terranes with different metamorphic facies 
> series that may or may not be exactly contemporaneous and that may or 
> may not be far-traveled. This is an inevitable consequence of the 
> difference between contemporaneous subduction, generating low dT/dP 
> blueschists and eclogites in the subduction zone and extension in an 
> arc--backarc system with formation of depositional basins, compared 
> with the timing of events such as ridge subduction or deformation and 
> thickening of the arc--backarc system, generating high dT/dP metamorphism.
> One issue to consider is whether to extend the concept of 'paired 
> metamorphic belts' more widely than accretionary orogens to 
> subduction-to-collision orogenic systems.  The modern plate tectonics 
> regime is characterized by a duality of thermal environments, the 
> subduction zone and the suture zone of subduction-to-collision 
> orogens, and the backarc or orogenic hinterland, in which contrasting 
> types of regional-scale metamorphic belts are being formed 
> contemporaneously. I consider this duality to be the hallmark of 
> one-sided subduction, and the characteristic imprint of one-sided 
> subduction in the geological record will be the broadly 
> contemporaneous occurrence of two contrasting types of metamorphism 
> reflecting this duality of thermal environments. On this basis, I 
> define paired metamorphic belts as penecontemporaneous belts of 
> contrasting type of metamorphism that record different apparent 
> thermal gradient, one warmer and the other colder, juxtaposed by plate 
> tectonics processes.
>             By this definition, the combination of granulite-ultrahigh 
> temperature metamorphism with eclogite-high-pressure granulite 
> metamorphism from the Neoarchean Era to the Neoproterozoic Era may be 
> described as a paired metamorphic belt. This extends the original 
> concept of Miyashiro (1961) beyond the simple pairing of high dT/dP 
> and low dT/dP metamorphic belts in circum-Pacific accretionary 
> orogens, and makes it more useful in the context of our better 
> understanding of the relationship between thermal regimes and tectonic 
> setting. This is particularly useful in subduction-to-collision 
> orogenic systems, where an accretionary phase is overprinted by a 
> collision phase that will be registered by the imprint of 
> penecontemporaneous low-to-intermediate dT/dP and high dT/dP 
> metamorphism in the rock record.
>  
>
>
>
> At 12:17 AM 2/12/2009, you wrote:
>>  
>>
>> Dear Colleagues,
>>
>> Students, friends and colleagues of Late Prof. Miyashiro are planning 
>> a special volume as a tribute to his vision and contributions in the 
>> various fields of Earth Sciences.
>>
>> The special volume will assemble benchmark papers on different themes 
>> including metamorphism, thermodynamics, orogeny, exhumation 
>> processes, mantle dynamics (including geophysics), volcanic rock 
>> series, ophiolites, eclogites,  and other related topics. 
>> Contributions under individual themes are expected to cover the 
>> historical outline, state-of-the-art and vision for the future. Among 
>> the contributors are Gary Ernst, Julian Pearce, Ned Brown, Surendra 
>> Saxena, Jibamitra Ganguly, Celal Sengor and Shun-ichiro Karato.
>>
>> Those who are interested to participate by contributing high quality 
>> papers to the volume as a tribute to Late Prof. Miyashiro, please 
>> e-mail us before March 10, 2009 together with the tentative title and 
>> a half page synopsis of the proposed contents.
>>
>>
>> The special volume will be brought out in the multidisciplinary 
>> geoscience journal 'Gondwana Research' published by Elsevier.
>>
>> (Journal Home Page: www.elsevier.com/locate/gr 
>> <http://www.elsevier.com/locate/gr> )
>>
>> (ScienceDirect page:  
>> http://www.sciencedirect.com/science/journal/1342937X)
>>
>>  
>> Thanks and best regards,
>>
>> Santosh
>>  
>> ________________________________________________________
>>  
>> M. Santosh
>> Professor of Geology & Editor-in-Chief, Gondwana Research
>> Department of Natural Environmental Science
>> Kochi University
>> Akebono-cho 2-5-1, Kochi 780-8520, Japan
>> Fax and phone:  +81-88-844-8278
>> E-mail: [log in to unmask] <mailto:[log in to unmask]>
>>  
>
> __________________________________________________________
>
> Michael Brown, Professor of Geology and Chair of 
> Department                
>
> Department of Geology                     
> Geology Building (#237)                   
> University of Maryland                    
> College Park                               
> MD 20742-4211                              
> USA
>                                             
> [log in to unmask]
> http: www.geol.umd.edu
> <http://www.geol.umd.edu/>Exec. asst.: 301 405 4065; Dept. office: 301 
> 405 4082; Direct line: 301 405 4080
> Direct fax: 301 314 7970; Dept. fax: 301 314 
> 9661                                                               
>
> LABORATORY FOR CRUSTAL PETROLOGY (Information at:
> http: www.geol.umd.edu/pages/faculty/BROWN/LCP/lcp.htm 
> <http://www.geol.umd.edu/pages/faculty/BROWN/LCP/lcp.htm>)
> __________________________________________________________
>

-- 

Dr. Robert J. Tracy

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