Topazfels in hornfels - Castle-an-Dinas
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Fact sheet
Description: 

This sample is part of a sedimentary xenolith that became incorporated into the late stage intrusion at Castle-an-Dinas, St Austell, Cornwall. It derived from the main St Austell granite, which was intruded during the Permian period, and was probably the result of an intrusion of the most evolved fluid remaining in the magma chamber at the end of a sequence of crystallisation. Castle-an-Dinas was the site of widespread mineralisation and was once home to Cornwall’s largest tungsten mine.

The thin section exhibits three distinct areas. The left-hand portion was originally fine-grained sedimentary layers that would have contained clay and detrital minerals such as quartz, but an influx of boron-enriched fluid has converted it to bands of tourmaline and quartz. Below the layered section is a quartz vein, and to the right of the tourmaline-rich zones is a sample of the intruding body, which crystallised to form a mixture of topaz, quartz and some small tourmaline grains.

In Place
In Time
infoImage: 
Location description: 
Castle-an-Dinas, St Austell, Cornwall
Accuracy:
Location precision: 
Good
Timescale:
Timescale: 
Permian
Ma = Millions of years ago
In Focus
Theme:

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Type:
Type: 
igneous
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