Computer Code: |
PLPD |
Preferred Map Code: |
PLP |
Status Code: |
Index Level |
Age range: |
Ediacaran Period (AD)
— Ediacaran Period (AD) |
Lithological Description: |
A highly porphyritic dacite, with abundant large phenocrysts of white plagioclase and less commonly, green-grey quartz in a dark grey, fine-grained groundmass. |
Definition of Lower Boundary: |
Not seen. |
Definition of Upper Boundary: |
Grades upwards to peperite breccia, interleaved with volcaniclastic sandstone of the Bardon Hill Volcanic Complex. |
Thickness: |
At least 50 m, possibly up to 200 m thick. |
Geographical Limits: |
Bardon Hill Quarry, Western Charnwood Forest. |
Parent Unit: |
Bardon Hill Volcanic Complex (BDHV)
|
Previous Name(s): |
Unnamed dacite [Obsolete Name and Code: Use PLPD]
(-3615)
|
Alternative Name(s): |
none recorded or not applicable
|
Stratotypes: |
Type Area |
The northern face of Bardon Hill Quarry, near Coalville. |
Reference(s): |
Worssam, B C and Old, R A, 1988. Geology of the country around Coalville. Memoir of the British Geological Survey, Sheet 155 (England and Wales) |
Carney, J N. 1999. Revisiting the Charnian Supergroup: new advances in the understanding of old rocks. Geology Today, Vol. 15, 221-229. |
Carney, J N. 2000. The geology of Bardon Hill and Whitwick quarries in Charnwood Forest, north-west Leicestershire. British Geological Survey Technical Report, WA/00/62. |
Carney, J N and Pharaoh, T C. 2000. Bardon Hill, 40-43. In: Precambrian Rocks of England and Wales, Geological Conservation Review Series No. 20. (Peterborough: Joint Nature Conservation Committee.) |
1:50K maps on which the lithostratigraphical unit is found, and map code used: |
E155
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