Zircon Saturation Temperature Estimates for Dalhousie Group Rhyolites

Table S4 provides zircon saturation thermometry temperature estimates in degrees Celsius for rhyolitic rocks from the Dalhousie Group. The dataset, authored by Jaroslav Dostal and shared via figshare, is a small 18.3 KB XLSX file. It was last updated in April 2026.

Use Cases

• Analyzing zircon saturation temperature (°C) estimates to infer crystallization conditions of felsic magmas.
• Correlating temperature data with specific rhyolitic rock samples from the Dalhousie Group for petrogenetic modeling.
• Using thermometry results as evidence for tectonic interpretations of the Chaleur Bay Synclinorium in northern New Brunswick.

Strengths

• Data is openly licensed under CC-BY-4.0 for reuse.
• File is in a standard, accessible XLSX format.

Limitations

• Dataset is very small at 18.3 KB, indicating a limited number of measurements or samples.
• No row count, column names, or sample data are provided, limiting immediate assessment of structure.
• Scope is highly specific to one geological group and analytical method.

Provenance

Source

Jaroslav Dostal, via figshare.

Collection Method

Zircon saturation thermometry applied to rhyolitic rock samples.

Time Range

Early Devonian period (geological).

Freshness

Last updated in April 2026.

Geography

Chaleur Bay Synclinorium, northern New Brunswick, Canada (Ganderia domain).