Paleoproterozoic ultrahigh-temperature granulite-facies metamorphism in the Sulu orogen, eastern China: Evidence from zircon and monazite in the pelitic granulite

2019 ◽  
Vol 333 ◽  
pp. 105430
Author(s):  
Haijin Xu ◽  
Hengcong Lei ◽  
Zhiwu Xiong ◽  
Junfeng Zhang
Keyword(s):  
Eastern China ◽  
Granulite Facies ◽  
Granulite Facies Metamorphism ◽  
Facies Metamorphism ◽  
Ultrahigh Temperature ◽  
Pelitic Granulite

scholarly journals Supplemental Material: Ultrahigh-temperature granulite-facies metamorphism and exhumation of deep crust in a migmatite dome during late- to post-orogenic collapse and extension in the central Adirondack Highlands (New York, USA)

2021 ◽  
Author(s):  
E.P. Metzger ◽  
et al. ◽  
M.L. Leech
Keyword(s):  
New York ◽  
Granulite Facies ◽  
Granulite Facies Metamorphism ◽  
Deep Crust ◽  
Honestly Significant Difference ◽  
Significant Difference ◽  
Facies Metamorphism ◽  
Text Figure ◽  
Tukey Honestly Significant Difference ◽  
Ultrahigh Temperature

<div>Text S1: Supplemental text. Figure S1: Cathodoluminescence images for all analyzed zircon grains. Figure S2: REE spider plots for zircon. Figure S3: Tukey honestly significant difference (HSD) for the timing of anatexis. Table S1: Cathodoluminescence images for all analyzed zircon grains. Table S2. Grossular content of garnet used to calculate the 95% confidence intervals for isopleth modeling in Figure 13. <br></div>

scholarly journals Supplemental Material: Ultrahigh-temperature granulite-facies metamorphism and exhumation of deep crust in a migmatite dome during late- to post-orogenic collapse and extension in the central Adirondack Highlands (New York, USA)

2021 ◽  
Author(s):  
E.P. Metzger ◽  
et al. ◽  
M.L. Leech
Keyword(s):  
New York ◽  
Granulite Facies ◽  
Granulite Facies Metamorphism ◽  
Deep Crust ◽  
Honestly Significant Difference ◽  
Significant Difference ◽  
Facies Metamorphism ◽  
Text Figure ◽  
Tukey Honestly Significant Difference ◽  
Ultrahigh Temperature

<div>Text S1: Supplemental text. Figure S1: Cathodoluminescence images for all analyzed zircon grains. Figure S2: REE spider plots for zircon. Figure S3: Tukey honestly significant difference (HSD) for the timing of anatexis. Table S1: Cathodoluminescence images for all analyzed zircon grains. Table S2. Grossular content of garnet used to calculate the 95% confidence intervals for isopleth modeling in Figure 13. <br></div>

scholarly journals Supplemental Material: Ultrahigh-temperature granulite-facies metamorphism and exhumation of deep crust in a migmatite dome during late- to post-orogenic collapse and extension in the central Adirondack Highlands (New York, USA)

2021 ◽  
Author(s):  
E.P. Metzger ◽  
et al. ◽  
M.L. Leech
Keyword(s):  
New York ◽  
Granulite Facies ◽  
Granulite Facies Metamorphism ◽  
Deep Crust ◽  
Honestly Significant Difference ◽  
Significant Difference ◽  
Facies Metamorphism ◽  
Text Figure ◽  
Tukey Honestly Significant Difference ◽  
Ultrahigh Temperature

<div>Text S1: Supplemental text. Figure S1: Cathodoluminescence images for all analyzed zircon grains. Figure S2: REE spider plots for zircon. Figure S3: Tukey honestly significant difference (HSD) for the timing of anatexis. Table S1: Cathodoluminescence images for all analyzed zircon grains. Table S2. Grossular content of garnet used to calculate the 95% confidence intervals for isopleth modeling in Figure 13. <br></div>

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