Supplementary Figure 1 and Table 1 for Cenozoic exhumation of the Qilian Shan in the northeastern Tibetan Plateau: Evidence from low-temperature thermochronology

Main Author: Wang, Weitao
Format: Dataset
Terbitan: Mendeley , 2020
Subjects:
Online Access: https:/data.mendeley.com/datasets/yhmtkdwzc7
ctrlnum 0.17632-yhmtkdwzc7.3
fullrecord <?xml version="1.0"?> <dc><creator>Wang, Weitao</creator><title>Supplementary Figure 1 and Table 1 for Cenozoic exhumation of the Qilian Shan in the northeastern Tibetan Plateau: Evidence from low-temperature thermochronology</title><publisher>Mendeley</publisher><description>Supplementary Fig.1 is apatite (U-Th)/He ages versus effective uranium content [eU] for the samples collected from the transects in the Qilian Shan region. There are no clear relationships with the effective Uranium&#xFF08;eU&#xFF09;and (U-Th)/He ages suggesting that the ages do not affect by (eU). Supplementary Table 1 is Thermal history model input table for simulations of low-temperature transects collected from the eastern Qilian Shan. For the geological constraints, the present surface temperature was set to 10 &#xB1; 10 &#xB0;C; the geothermal gradient was in the range of 30 &#xB1; 30 &#xB0;C/km. We did not impose any other temperature constraint for all modeling samples</description><subject>Supplementation</subject><type>Other:Dataset</type><identifier>10.17632/yhmtkdwzc7.3</identifier><rights>Creative Commons Attribution 4.0 International</rights><rights>http://creativecommons.org/licenses/by/4.0</rights><relation>https:/data.mendeley.com/datasets/yhmtkdwzc7</relation><date>2020-02-15T04:33:40Z</date><recordID>0.17632-yhmtkdwzc7.3</recordID></dc>
format Other:Dataset
Other
author Wang, Weitao
title Supplementary Figure 1 and Table 1 for Cenozoic exhumation of the Qilian Shan in the northeastern Tibetan Plateau: Evidence from low-temperature thermochronology
publisher Mendeley
publishDate 2020
topic Supplementation
url https:/data.mendeley.com/datasets/yhmtkdwzc7
contents Supplementary Fig.1 is apatite (U-Th)/He ages versus effective uranium content [eU] for the samples collected from the transects in the Qilian Shan region. There are no clear relationships with the effective Uranium(eU)and (U-Th)/He ages suggesting that the ages do not affect by (eU). Supplementary Table 1 is Thermal history model input table for simulations of low-temperature transects collected from the eastern Qilian Shan. For the geological constraints, the present surface temperature was set to 10 ± 10 °C; the geothermal gradient was in the range of 30 ± 30 °C/km. We did not impose any other temperature constraint for all modeling samples
id IOS7969.0.17632-yhmtkdwzc7.3
institution Universitas Islam Indragiri
affiliation onesearch.perpusnas.go.id
institution_id 804
institution_type library:university
library
library Teknologi Pangan UNISI
library_id 2816
collection Artikel mulono
repository_id 7969
city INDRAGIRI HILIR
province RIAU
shared_to_ipusnas_str 1
repoId IOS7969
first_indexed 2020-04-08T08:16:26Z
last_indexed 2020-04-08T08:16:26Z
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