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,
,
, James Worthington,
,
,

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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