Supplementary data for 'Zircon perspectives on the age and origin of evolved S-type granites from the Cornubian Batholith, Southwest England'.
Dataset
- William Daniel Smith (Creator)
- Dr James Darling (Creator)
- Dr Dean Bullen (Creator)
- Stephanie Lasalle (Creator)
- Inês Filipa Gonçalves Martins Pereira (Creator)
- Hugo Souza Moreira (Creator)
- Connor James Allen (Creator)
- Simon Tapster (Creator)
Description
Supplementary data are available on the publisher's webapage (10.1016/j.lithos.2019.03.025 ) and are reproduced here after the embargo period (ends 25/03/20):
Supplementary Figure 1. a. LA-ICP-MS Tera-Wasserburg diagram of BG zircon cores and rims from Blackenstone Quarry, with regression line fixed at 0.85 after Stacey & Kramers (1975) model, presented ages are weighted averages. b. LA-ICP-MS Tera-Wasserburg diagram of BG zircon cores and rims from Lee Moor. c. Results from concordant analysis obtained from CA-ID-TIMS analysis of Blackenstone BG zircon grains. Here it is presented with calculated and weighted average ages. d. Results from concordant analysis obtained from CA-ID-TIMS analysis of Lee Moor TG.
Supplementary Table 1. Whole-rock geochemistry for samples used for this study.
Supplementary Table 2. LA-ICP-MS U-Pb zircon geochronology dataset for granites at Crownhill.
Supplementary Table 3. LA-ICP-MS U-Pb monazite geochronology dataset for BG at Crownhill.
Supplementary Table 4. CA-ID-TIMS U-Pb zircon geochronology dataset for granites at Crownhill.
Supplementary Table 5. Representative dataset for LA-ICP-MS zircon trace element analysis, including the Ti-in-Zrn thermometer [1] (Watson & Harrison, 1983).
Supplementary Figure 1. a. LA-ICP-MS Tera-Wasserburg diagram of BG zircon cores and rims from Blackenstone Quarry, with regression line fixed at 0.85 after Stacey & Kramers (1975) model, presented ages are weighted averages. b. LA-ICP-MS Tera-Wasserburg diagram of BG zircon cores and rims from Lee Moor. c. Results from concordant analysis obtained from CA-ID-TIMS analysis of Blackenstone BG zircon grains. Here it is presented with calculated and weighted average ages. d. Results from concordant analysis obtained from CA-ID-TIMS analysis of Lee Moor TG.
Supplementary Table 1. Whole-rock geochemistry for samples used for this study.
Supplementary Table 2. LA-ICP-MS U-Pb zircon geochronology dataset for granites at Crownhill.
Supplementary Table 3. LA-ICP-MS U-Pb monazite geochronology dataset for BG at Crownhill.
Supplementary Table 4. CA-ID-TIMS U-Pb zircon geochronology dataset for granites at Crownhill.
Supplementary Table 5. Representative dataset for LA-ICP-MS zircon trace element analysis, including the Ti-in-Zrn thermometer [1] (Watson & Harrison, 1983).
Date made available | 25 Mar 2019 |
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Publisher | Elsevier BV |
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Smithetal2019_SFig1_1_s2.0_S0024493719301252_mmc1.docx
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Related information
Outputs
Zircon perspectives on the age and origin of evolved S-type granites from the Cornubian Batholith, Southwest England
Research output: Contribution to journal › Article › peer-review
ID: 13785128