AVO Sample Information

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SAMPLE INFO : 94SJP29

Sample ID:	94SJP29
Station ID:	94SJP29
Latitude:	62.43768247
Longitude:	-143.1257474
Datum:	NAD83
Date Sampled:	1994-00-00
Sample Type 1:	Lava
Sample Type 2:	Dike
Field Lithology:	Basaltic Andesite

Text Description:
Subvertical dike trending N20W and intruding into silicic material from Dome A at Site 2. Fine-grained, seriate, intergranular, altered, vesicular, holocrystalline with a matrix of mesostasis, opaque, feldspar, clinopyroxene, calcite alteration and other alteration. Plagioclase phenocrysts (An19-An56) are 1.3 - 0.05 mm; larger grains have sieve textured cores, complex zoning, embayments, and one grain has strongly poikilitic olivine or clinopyroxene. Orthopyroxene phenocrysts are 0.3 - 0.05 mm, subhedral, some have clinopyroxene rims and/or melt inclusions. Clinopyroxene phenocrysts are 0.55 - 0.5 mm. Olivine? phenocrysts are nearly completely altered.

References:

Geochemical variation in the less than 5 Ma Wrangell Volcanic Field, Alaska, with an emphasis on the Skookum Creek volcanic complex

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
94SJP29	62.43768247	-143.1257474	Preece, S. J.	1994-00-00		Skookum Creek		Nabesna B-5, T8N, R12E, S35	Subvertical dike trending N20W and intruding into silicic material from Dome A at Site 2. Fine-grained, seriate, intergranular, altered, vesicular, holocrystalline with a matrix of mesostasis, opaque, feldspar, clinopyroxene, calcite alteration and other alteration. Plagioclase phenocrysts (An19-An56) are 1.3 - 0.05 mm; larger grains have sieve textured cores, complex zoning, embayments, and one grain has strongly poikilitic olivine or clinopyroxene. Orthopyroxene phenocrysts are 0.3 - 0.05 mm, subhedral, some have clinopyroxene rims and/or melt inclusions. Clinopyroxene phenocrysts are 0.55 - 0.5 mm. Olivine? phenocrysts are nearly completely altered.	94SJP29	Lava			Whole-rock	54.88	0.78	18.1	5.64	0.15	4	8.7	3.62	1.18	0.34	98.55	55	DCP	6.13	5.64	LOI=2.58	DCP		21.2	472	623															17	95	3.1				3.8	2.2	21	162	31			59	71	60	17.6					55	XRF: Rb, Zr, Nb, Th, U, Ni, Ga; DCP: Ba, Sc, V; MX: Sr, Y, Cr, Cu, Zn;

SAMPLE LOCATION

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