Postcollisional flow of aqueous fluid within ultrahigh-pressure eclogite in the Dabie orogen

2006 ◽  
Vol 89 (1-3) ◽  
pp. 115-118 ◽  
Author(s):  
Tian-Shan Gao ◽  
Song-Shan Wang ◽  
Bing Gong ◽  
Yuan-Bao Wu ◽  
Yong-Fei Zheng
2011 ◽  
Vol 119 (1) ◽  
pp. 15-31 ◽  
Author(s):  
Yuanbao Wu ◽  
Shan Gao ◽  
Xiaochi Liu ◽  
Jing Wang ◽  
Min Peng ◽  
...  

2009 ◽  
Vol 54 (10) ◽  
pp. 1449-1454 ◽  
Author(s):  
HuJun GONG ◽  
SaiHong YANG ◽  
Min PENG ◽  
XiaoChi LIU ◽  
WenFang JIAO ◽  
...  

Lithos ◽  
2016 ◽  
Vol 266-267 ◽  
pp. 158-181 ◽  
Author(s):  
Qiong-Xia Xia ◽  
Hao-Zheng Wang ◽  
Li-Gang Zhou ◽  
Xiao-Ying Gao ◽  
Yong-Fei Zheng ◽  
...  

2007 ◽  
Vol 25 (9) ◽  
pp. 975-989 ◽  
Author(s):  
Y.-C. LIU ◽  
S.-G. LI ◽  
X.-F. GU ◽  
S.-T. XU ◽  
G.-B. CHEN

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Simona Ferrando ◽  
Maurizio Petrelli ◽  
Maria Luce Frezzotti

Abstract The geochemical signature of magmas generated at convergent margins greatly depends on the nature of fluids and melts released during subduction. While major- and trace-elements transport capacity of ultrahigh pressure (UHP) hydrous-silicate melts has been investigated, little is known about solute enrichment and fractionation in UHP (>3.5–4 GPa) solute-rich aqueous fluids released along colder geothermal gradients. Here, we performed in situ LA-ICP-MS trace-element analyses on selected UHP prograde-to-peak fluid inclusions trapped in a kyanite-bearing quartzite from Sulu (China). The alkali-aluminosilicate-rich aqueous fluid released from the meta-sediments by dehydration reactions is enriched in LILE, U, Th, Sr, and REE. Inclusions trapped at increasing temperature (and pressure) preserve a gradual and selective trace-element enrichment resulting from the progressive dissolution of phengite and carbonate and the partial dissolution of allanite/monazite. We show that, at the investigated P-T conditions, aqueous fluids generated by dissolution of volatile-bearing minerals fractionate trace-element distinctly from hydrous-silicate melts, regardless of the source lithology. The orogenic/post-orogenic magmas generated in a mantle enriched by metasomatic processes involving either solute-rich aqueous fluids or hydrous-silicate melts released by the slab at UHP conditions can preserve evidence of the nature of these agents.


2015 ◽  
Vol 419 ◽  
pp. 158-175 ◽  
Author(s):  
Xiao-Ying Gao ◽  
Yong-Fei Zheng ◽  
Yi-Xiang Chen ◽  
Hao-Lan Tang ◽  
Wan-Cai Li

2006 ◽  
Vol 231 (1-2) ◽  
pp. 135-158 ◽  
Author(s):  
Yong-Fei Zheng ◽  
Zi-Fu Zhao ◽  
Yuan-Bao Wu ◽  
Shao-Bing Zhang ◽  
Xiaoming Liu ◽  
...  

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