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SAMPLE INFO : Barth_1956_12

Sample ID:	Barth_1956_12
Station ID:	Barth_1956_12
Latitude:	56.58
Longitude:	-169.63
Datum:	NAD83
Date Sampled:	1948-01-01
Sample Type 1:	Lava

Text Description:
Sample of a vesicular, columnar flow or sill of aphyric olivine basalt. The rock consists of large, randomly oriented laths of plagioclase forming an irregular meshwork filled with olivine, augite, apatite, and magnetite, the latter being in large measure a reaction product of olivine; indeed, the olivine has the properties of pure forsterite, indicating that the fayalite component has been used up in the reaction.

References:

Geology and petrology of the Pribilof Islands, Alaska

GEOCHEM DATA

StationID	Latitude	Longitude	Geologist	DateVisited	Age Info	Volcano	Eruption	Location Description	Text Description	Sample ID	Sample Type 1	Sample Type 2	Final Unit	Material	SiO2	TiO2	Al2O3	FeOT	MnO	MgO	CaO	Na2O	K2O	P2O5	Total-majors	REF majors	METH majors	Fe2O3/Fe203T orig	FeO/FeOT orig	Volatiles csv	METH volatiles	Cs	Rb	Ba	Sr	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	Y	Zr	Nb	Hf	Ta	Pb	Th	U	Sc	V	Cr	Fe	Co	Ni	Cu	Zn	Ga	Mo	As	Na	K	Ref trace1	METH trace1	Rb	Ba	Sr	La	Ce	Nd	Sm	Eu	Gd	Dy	Er	Yb	Lu	Y	Zr	Nb	Pb	Th	U	Sc	Ti	V	Cr	Ni	Cu	Zn	Ga	Ref trace2	METH trace2	Light csv	Halogen csv	other major csv	other lile csv	other ree csv	other hfse csv	other hpe csv	other tm csv	other misc csv
Barth_1956_12	56.58	-169.63	Barth, T. F. W.	1948-01-01		St. George volcanic field		Between Zapadni Bay and Red Bluffs, St. George Island	Sample of a vesicular, columnar flow or sill of aphyric olivine basalt. The rock consists of large, randomly oriented laths of plagioclase forming an irregular meshwork filled with olivine, augite, apatite, and magnetite, the latter being in large measure a reaction product of olivine; indeed, the olivine has the properties of pure forsterite, indicating that the fayalite component has been used up in the reaction.	Barth_1956_12	Lava			Whole-rock	47.3	2.1	15	11.8	0.2	10.2	9	2.8	1	0.33	99.5	301	RAPIDA	7.6	4.8

SAMPLE LOCATION

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