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Hi Shujuan,

	A xenotime-garnet Y exchange thermometer was empircially callibrated by Joe Pyle and Frank Spear some years ago (see attached).  There may be some references in either paper that are of use to you.  

								Tschau,

								    Dan





	

> On 3. Sep 2018, at 10:28, 焦淑娟 <[log in to unmask]> wrote:
> 
> Dear Daniela,
>   Thanks so much for the articles and suggestions, especially the last one in 2018, which I have not noticed before. I have compared the results mostly in the range of 20-40 from my rocks with those (46) in Hermann and Rubatto, (2003) JMG and that (22) in Rubatto et al., (2006 JP), and I think they are consistent. I am trying to compare with more other studies, especially the monazite-garnet pairs having been proven to be in equilibrium, to check for consistency.
>    Thanks so much again.
>   With my best wishes,
>   Shujuan  
> 
> 
> 
> 
> --
> 焦淑娟 博士
> Dr. Shujuan Jiao
> 中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室
> State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences
> 地址:北京市朝阳区北土城西路19号,地3楼538室, 100029
> Address:Room 538 Building 3,No. 19 Beitucheng Western Road, Chaoyang District, Beijing, 100029, China
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> 
> 
> 在 2018-09-03 15:46:18,[log in to unmask] 写道:
> Dear Dr Jiao
> Y partitioning between monazite and garnet can be found in the attached papers below. These studies refer to HT granulites
> 
> for lower T rocks, an example is in  
> 
> In all cases, the most tricky things is to establish equilibrium with independent criteria (textures, ages, other petrological constraints 鈥?)
> regards
> Daniela 
> 鈥撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€?/b>
> Prof. Daniela Rubatto
> Institute of Geological Sciences, University of Bern (Universit盲t Bern)
> Baltzerstrasse 1-3, CH-3012, SWITZERLAND
> Tel. direct +41 31 631 4770, Tel. admin +41 31 631 8781
> 鈥撯€撯€撯€撯€撯€撯€撯€?/i>
> Scientific collaborator
> Institut de Sciences de la Terre, University of Lausanne
> UNIL-Grange, Geopolis, 1015 Lausanne, SWITZERLAND
> 鈥撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€撯€?/b>
> 
>> On 3 Sep 2018, at 04:51, 鐒︽窇濞?<[log in to unmask] <mailto:[log in to unmask]>> wrote:
>> 
>>  
>> Dear colleagues,
>>    I am currently working on yttrium partitioning between possible equilibrated monazite and garnet pairs in natural ultrahigh-temperature granulites. I have gotten some insights from my samples, and I would like to compare them with the available Y partitioning between monazite and garnet in the other works or literatures.
>>  Any recommendations and suggestions will be very appreciated. Thanks so much in advance.
>>  
>> With my best wishes,
>>  Shujuan Jiao
>> 
>> 
>> 
>> 
>> 
>> 
>> --
>> 鐒︽窇濞?鍗氬+
>> Dr. Shujuan Jiao
>> 涓浗绉戝闄㈠湴璐ㄤ笌鍦扮悆鐗╃悊鐮旂┒鎵€锛屽博鐭冲湀婕斿寲鍥藉閲嶇偣瀹為獙瀹?/div>
>> State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences
>> 鍦板潃锛氬寳浜競鏈濋槼鍖哄寳鍦熷煄瑗胯矾19鍙凤紝鍦?妤?38瀹? 100029
>> Address锛歊oom 538 Building 3锛孨o. 19 Beitucheng Western Road, Chaoyang District, Beijing, 100029, China
>> 鐢佃瘽锛?10-82998538
>> Tel: +86-(0)10-82998538
>> 閭锛?a href="mailto:[log in to unmask] <mailto:[log in to unmask]>" class="">[log in to unmask] <mailto:[log in to unmask]>
>> E-mail: [log in to unmask] <mailto:[log in to unmask]>
>> 
>> 
>> 
>>  
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Daniel Harlov
Section 4.3 Chemistry and Physics of Earth Materials
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