Supplementary figure 1, sample location with Maximum depositional age, and Zircon U-Pb analyses : Evidence for Late Triassic crustal suturing of the Central and Southern Pamir

Published: 31 March 2020| Version 1 | DOI: 10.17632/s3rfym3mdt.1
Contributors:
Dustin Villarreal,
Alexander Robinson,
Barbara Carrapa,
James Worthington,
James Chapman,
Ilhomjon Oimahmadov,
Mustafo Gadoev

Description

Sup Fig. 1. Calculated R2 crossplot statistical comparison values between the Lokzun Group flysch, Darbasatash Group, and Northern Pamirs’ Karakul-Mazar using Saylor and Sundell’s (2016) DZstats. An R2 crossplot value greater than 0.70±0.10 suggest that the samples are related and have a common source. Note that sample DV 8-08-16_3, which has a distinct late Proterozoic-early Paleozoic population, is associated with R2 crossplot values that lie below this range. Table 1 DR1-Sample Location and MDA contains the location and maximum depositional age for samples in the manuscript:Evidence for Late Triassic crustal suturing of the Central and Southern Pamir Table 2 DR2-Zircon U-Pb analyses contains data collected from the samples used in the manuscript: Evidence for Late Triassic crustal suturing of the Central and Southern Pamir

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