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 |
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Format: | Dataset |
Terbitan: |
Mendeley
, 2020
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Subjects: | |
Online Access: |
https:/data.mendeley.com/datasets/yhmtkdwzc7 |
ctrlnum |
0.17632-yhmtkdwzc7.3 |
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fullrecord |
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<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(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</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 |
recordtype |
dc |
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1686587415008903168 |
score |
17.538404 |