Data for: Multi-stage evolution of the Xuhuai rift: Insights from the occurrence and compositional profiles of doleritic sills in the southeastern margin of the North China Craton
| Main Author: | Peng, Peng |
|---|---|
| Other Authors: | SU, Xiangdong |
| Format: | Dataset |
| Terbitan: |
Mendeley
, 2020
|
| Subjects: | |
| Online Access: |
https:/data.mendeley.com/datasets/539sw4tr8b |
| ctrlnum |
0.17632-539sw4tr8b.1 |
|---|---|
| fullrecord |
<?xml version="1.0"?>
<dc><creator>Peng, Peng</creator><title>Data for: Multi-stage evolution of the Xuhuai rift: Insights from the occurrence and compositional profiles of doleritic sills in the southeastern margin of the North China Craton</title><publisher>Mendeley</publisher><description>The chemical data measured from the Pingshan sill is presented in Supplementary Table S1. The variations in composition of intercumulus and cumulus clinopyroxene present an almost M-shaped profile. Some of the clinopyroxene grains is always normally zoned, with high Mg# (and En) cores passing into low Mg# (and En) rims with compositional differences of up to 19 % (10 % for En). Although clinopyroxene have variable compositions (Wo37.7-47.6En34.5-47.7Fs9.8-26.6) and Mg# (0.57-0.83), with relatively low TiO2 (0.5-1.3 wt%), MnO (0.1-0.5 wt%) and Na2O (0.2-0.7 wt%) contents, it should be noted that clinopyroxene with highest Mg# [Mg/(Mg+Fe2+)] and En at 39 m, 20 m and 11.5 m height. It is difficultly attributed the crossover levels for En and Mg# in clinopyroxene from this sill to mechanical sorting of clinopyroxene crystals in a single magma injection.</description><subject>Geochemistry</subject><subject>Mineralogy</subject><subject>Igneous Petrology</subject><contributor>SU, Xiangdong</contributor><type>Other:Dataset</type><identifier>10.17632/539sw4tr8b.1</identifier><rights>Attribution-NonCommercial 3.0 Unported</rights><rights>https://creativecommons.org/licenses/by-nc/3.0</rights><relation>https:/data.mendeley.com/datasets/539sw4tr8b</relation><date>2020-03-31T18:51:42Z</date><date>2020-03-17T00:00:00Z</date><recordID>0.17632-539sw4tr8b.1</recordID></dc>
|
| format |
Other:Dataset Other |
| author |
Peng, Peng |
| author2 |
SU, Xiangdong |
| title |
Data for: Multi-stage evolution of the Xuhuai rift: Insights from the occurrence and compositional profiles of doleritic sills in the southeastern margin of the North China Craton |
| publisher |
Mendeley |
| publishDate |
2020 |
| topic |
Geochemistry Mineralogy Igneous Petrology |
| url |
https:/data.mendeley.com/datasets/539sw4tr8b |
| contents |
The chemical data measured from the Pingshan sill is presented in Supplementary Table S1. The variations in composition of intercumulus and cumulus clinopyroxene present an almost M-shaped profile. Some of the clinopyroxene grains is always normally zoned, with high Mg# (and En) cores passing into low Mg# (and En) rims with compositional differences of up to 19 % (10 % for En). Although clinopyroxene have variable compositions (Wo37.7-47.6En34.5-47.7Fs9.8-26.6) and Mg# (0.57-0.83), with relatively low TiO2 (0.5-1.3 wt%), MnO (0.1-0.5 wt%) and Na2O (0.2-0.7 wt%) contents, it should be noted that clinopyroxene with highest Mg# [Mg/(Mg+Fe2+)] and En at 39 m, 20 m and 11.5 m height. It is difficultly attributed the crossover levels for En and Mg# in clinopyroxene from this sill to mechanical sorting of clinopyroxene crystals in a single magma injection. |
| id |
IOS7969.0.17632-539sw4tr8b.1 |
| 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 |
2020-04-08T08:30:39Z |
| last_indexed |
2020-04-08T08:30:39Z |
| recordtype |
dc |
| _version_ |
1686587757567148032 |
| score |
17.538404 |