- 7,663
- 3,708
This sample is from Honstjern:
Honstjern carbonatized damtjernite-like explosion breccia. This sample was obtained a few hundred meters away from the Tveitan carbonatized damtjernite-like explosion breccia. As before, this is a melanocratic aphanitic rock with nodular texture, many nodules have a core containing relic amphibole.
Carbonate vein and veinlets. Although the gross texture also resembles carbonatized damtjernite samples 74 Fen 50 N-6A, N-6B, and N-6C; there are significantly fewer opaques, biotite phenocrysts are absent, and chlorite is present. Many of the nodules have a complex interior structure:
Large feldspar xenocryst with amphibole inclusions, appears to have a dark carbonate reaction rim.
Groundmass is extremely fine-grained, consisting of carbonate, possibly biotite flakes, abundant apatite crystals, and innumerable minute rounded inclusions.
Edit: Ha! I forgot the mention the whole reason I selected this sample... Even though these two rocks (Honstjern and Tveitan carbonatized damtjernite-like explosion breccias) look identical and located so close to each other, K-Ar dating models place the two samples 200 million years apart. I'm not sure that puzzle was ever solved.
Honstjern carbonatized damtjernite-like explosion breccia. This sample was obtained a few hundred meters away from the Tveitan carbonatized damtjernite-like explosion breccia. As before, this is a melanocratic aphanitic rock with nodular texture, many nodules have a core containing relic amphibole.
Carbonate vein and veinlets. Although the gross texture also resembles carbonatized damtjernite samples 74 Fen 50 N-6A, N-6B, and N-6C; there are significantly fewer opaques, biotite phenocrysts are absent, and chlorite is present. Many of the nodules have a complex interior structure:
Large feldspar xenocryst with amphibole inclusions, appears to have a dark carbonate reaction rim.
Groundmass is extremely fine-grained, consisting of carbonate, possibly biotite flakes, abundant apatite crystals, and innumerable minute rounded inclusions.
Edit: Ha! I forgot the mention the whole reason I selected this sample... Even though these two rocks (Honstjern and Tveitan carbonatized damtjernite-like explosion breccias) look identical and located so close to each other, K-Ar dating models place the two samples 200 million years apart. I'm not sure that puzzle was ever solved.
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