High-pressure anatectic paragneisses from the Namche Barwa, Eastern Himalayan Syntaxis: Textural evidence for partial melting, phase equilibria modeling and tectonic implications

详细信息    查看全文

• 作者：C. Guilmette^a ; ^{carl.guilmette.1@ulaval.ca} ; A. Indares^b ; R. Hé ; bert^a
• 关键词：High-P granulite ; Kyanite ; THERMOCALC ; Pseudosection ; Anatexis
• 刊名：Lithos
• 出版年：2011
• 出版时间：May 2011
• 年：2011
• 卷：124
• 期：1-2
• 页码：66-81
• 全文大小：8418 K

文摘

Rare kyanite-bearing anatectic paragneisses are found as boudins within sillimanite-bearing paragneisses of the core of the Namche Barwa Antiform, Tibet. In the present study, we document an occurrence from the NW side of the Yarlung Zangbo River. These rocks mainly consist of the assemblage garnet + K-feldspar + kyanite ± biotite + quartz + rutile ± plagioclase with kyanite locally pseudomorphed by sillimanite.

The documented textures are consistent with the rocks having undergone biotite-dehydration melting in the kyanite stability field, under high-P granulite facies conditions, and having experienced melt extraction. However textures related to melt crystallization are ubiquitous both in polymineralic inclusions in garnet and in the matrix, suggesting that a melt fraction had remained in these rocks.

Phase equilibria modelling was undertaken in the NCKFMASTHO system with THERMOCALC. P–T pseudosections built with the bulk compositions of one aluminous and one sub-aluminous paragneiss samples predict a biotite–kyanite–garnet–quartz–plagioclase–K-feldspar–liquid–rutile ± ilmenite field, in which biotite-dehydration melting occurs, located in the P–T range of ~ 800–875 °C and ~ 10–17 kbar. In addition, the topologies of these pseudosections are consistent with substantial melt loss during prograde metamorphism. A second set of P–T pseudosections with melt-reintegrated model bulk compositions were thus constructed to evaluate the effect of melt loss. The integration of textural information, precise mineral modes, mineral chemistry, and phase equilibria modelling allowed to constrain a P–T path where the rocks are buried to lower crustal depths at peak P–T conditions higher than 14 kbar and 825 °C, possibly in the order of 15–16 kbar and 850 °C, followed by decompression and cooling to P–T conditions of around 9 kbar and 810 °C, under which the remaining melt was solidified. The implications for granite production at the NBA and for Himalayan tectonic models are discussed.