GRD00Q1S0

W63-162

Volcaniclastic Sediment

Unknown
None -

1

Ritter 154 › Cabinet 17 › Drawer N

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Clasts are mostly of volcanic origin. Blue copper staining in the matrix.

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Large euhedral plagioclase in a clast

2.5

plane

Large euhedral plagioclase in a clast

2.5

crossed

Texture of the matrix

2.5

plane

Texture of the matrix

2.5

crossed

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scan

crossed

-

scan

plane

GRD00Q1T0: Matrix: Angular feldspar and quartz fragments. Amphibole and opaques. Clay. Occasional quartzite clasts. Clast: Fine-grained. Large euhedral and heavily resorbed plagioclase in finer-grained plagioclase lath matrix. (C. Eichler)

N/A

N/A