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• W3036108775 endingPage "962" @default.
• W3036108775 startingPage "935" @default.
• W3036108775 abstract "Abstract Robust quantification of pressure ( P )–temperature ( T ) paths for subduction‐related HP/UHP metamorphic rocks is fundamental in recognizing spatial changes in both the depth of detachment from the down‐going plate and the thermal evolution of convergent margin sutures in orogenic belts. Although the Chinese southwestern (SW) Tianshan is a well‐known example of an accretionary metamorphic belt in which HP/UHP metabasites occur in voluminous host metasedimentary schists, information about the P–T evolution of these rocks in the eastern segment is limited, precluding a full understanding of the development of the belt as a whole. In this study at Kekesu in the eastern segment of the SW Tianshan, we use microstructural evidence and phase equilibrium modelling to quantify the peak and retrograde P–T conditions from two lawsonite‐bearing micaschists and an enclosed garnet–epidote blueschist; for two of the samples we also constrain the late prograde P–T path. In the two micaschist samples, relics of prograde lawsonite are preserved in quartz inclusions in garnet, whereas in the metabasite, polymineralic aggregates included in garnet are interpreted as pseudomorphs after lawsonite. For garnet micaschist TK21, which is mainly composed of garnet, phengite/paragonite, albite, chlorite, quartz and relict lawsonite, with accessary rutile, titanite and ilmenite, the maximum P–T conditions for the peak stage are 18.0–19.0 kbar at 480–485°C. During initial exhumation, the retrograde P–T path passed through metamorphic conditions of 15.0–17.0 kbar at 460–500°C. For garnet–glaucophane micaschist TK33, which is mainly composed of garnet, glaucophane, phengite/paragonite, albite, chlorite, quartz, relict lawsonite and minor epidote, with accessary titanite, apatite, ilmenite and zircon, the maximum P conditions for the peak stage are >24.0 kbar at 400–500°C. During exhumation, the P–T path passed through metamorphic conditions of 17.5–18.5 kbar at 485–495°C and 14.0–17.5 kbar at 460–500°C. For garnet–epidote blueschist TK37, which is mainly composed of garnet, glaucophane, epidote, phengite, chlorite, albite and quartz, with accessary titanite, apatite, ilmenite, zircon and calcite, the prograde evolution passed through metamorphic conditions of ~20.0 kbar at ~445°C to P max conditions of ~21.5 kbar at 450–460°C and T max conditions of 19.5–21.0 kbar at 490–520°C. During exhumation, the rock passed through metamorphic conditions of 17.5–19.0 kbar at 475–500°C, before recording P–T conditions of <17.5 kbar at <500°C. These results demonstrate that maximum recorded pressures for individual samples vary by as much as 6 kbar in the eastern segment of the SW Tianshan, which may suggest exhumation from different depths in the subduction channel. Furthermore, the three samples record similar P–T paths from ~17.0 to 15.0 kbar, which suggests they were juxtaposed at a similar depth along the subduction interface. We compare our new results with published information from eclogites in the same area before considering the wider implications of these data for the orogenic development of the belt as a whole." @default.
• W3036108775 created "2020-06-25" @default.
• W3036108775 creator A5015954930 @default.
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• W3036108775 date "2020-07-28" @default.
• W3036108775 modified "2023-10-14" @default.
• W3036108775 title "<i>P–T</i> evolution and tectonic significance of lawsonite‐bearing schists from the eastern segment of the southwestern Tianshan, China" @default.
• W3036108775 cites W1514033991 @default.
• W3036108775 cites W1603705388 @default.
• W3036108775 cites W1785387093 @default.
• W3036108775 cites W1786391451 @default.
• W3036108775 cites W1898464489 @default.
• W3036108775 cites W1964375195 @default.
• W3036108775 cites W1968582097 @default.
• W3036108775 cites W1975507462 @default.
• W3036108775 cites W1976291585 @default.
• W3036108775 cites W1976304054 @default.
• W3036108775 cites W1977875524 @default.
• W3036108775 cites W1982585529 @default.
• W3036108775 cites W1986848325 @default.
• W3036108775 cites W1988430692 @default.
• W3036108775 cites W1989878389 @default.
• W3036108775 cites W1990381508 @default.
• W3036108775 cites W1995350298 @default.
• W3036108775 cites W1995549485 @default.
• W3036108775 cites W1997842666 @default.
• W3036108775 cites W2002242075 @default.
• W3036108775 cites W2009436180 @default.
• W3036108775 cites W2014800383 @default.
• W3036108775 cites W2014845614 @default.
• W3036108775 cites W2017299458 @default.
• W3036108775 cites W2017649324 @default.
• W3036108775 cites W2019572890 @default.
• W3036108775 cites W2027759127 @default.
• W3036108775 cites W2028882528 @default.
• W3036108775 cites W2031981361 @default.
• W3036108775 cites W2035045796 @default.
• W3036108775 cites W2040771319 @default.
• W3036108775 cites W2044092813 @default.
• W3036108775 cites W2046264604 @default.
• W3036108775 cites W2047550028 @default.
• W3036108775 cites W2049953934 @default.
• W3036108775 cites W2051916584 @default.
• W3036108775 cites W2052655466 @default.
• W3036108775 cites W2059015933 @default.
• W3036108775 cites W2060048441 @default.
• W3036108775 cites W2066122879 @default.
• W3036108775 cites W2068295421 @default.
• W3036108775 cites W2078120948 @default.
• W3036108775 cites W2082867332 @default.
• W3036108775 cites W2094908107 @default.
• W3036108775 cites W2096160261 @default.
• W3036108775 cites W2100411277 @default.
• W3036108775 cites W2106158525 @default.
• W3036108775 cites W2124087345 @default.
• W3036108775 cites W2126440321 @default.
• W3036108775 cites W2128912555 @default.
• W3036108775 cites W2131817581 @default.
• W3036108775 cites W2137588825 @default.
• W3036108775 cites W2146803029 @default.
• W3036108775 cites W2169483319 @default.
• W3036108775 cites W2216920053 @default.
• W3036108775 cites W2279053128 @default.
• W3036108775 cites W2302377861 @default.
• W3036108775 cites W2312102088 @default.
• W3036108775 cites W2462542673 @default.
• W3036108775 cites W2514574042 @default.
• W3036108775 cites W2583448077 @default.
• W3036108775 cites W2611324195 @default.
• W3036108775 cites W2625888985 @default.
• W3036108775 cites W2793317135 @default.
• W3036108775 cites W2795918872 @default.
• W3036108775 cites W2802441917 @default.
• W3036108775 cites W2805502766 @default.
• W3036108775 cites W2808439377 @default.
• W3036108775 cites W2808713057 @default.
• W3036108775 cites W2810467636 @default.
• W3036108775 cites W2889037811 @default.
• W3036108775 cites W2900287790 @default.
• W3036108775 cites W2921607632 @default.
• W3036108775 cites W2965822114 @default.
• W3036108775 cites W2986435098 @default.
• W3036108775 cites W4240273548 @default.
• W3036108775 doi "https://doi.org/10.1111/jmg.12555" @default.
• W3036108775 hasPublicationYear "2020" @default.
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