AVO Sample Information

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SAMPLE INFO : 91CND36

Sample ID:	91CND36
Station ID:	91CND36
Latitude:	58.830151
Longitude:	-153.47529
Datum:	NAD83
Date Sampled:	1991-01-01
Sample Type 1:	Lava

Text Description:
Another sample of host lava from the same flow as 91CND33. Porphyritic andesite. About 30% phenocrysts of millimeter-sized plagioclase, sub-millimeter-sized pyroxene and sparse olivine in a groundmass of microphenocrysts and microlite-rich glass and microcrystalline material.

References:

Geochemistry of some Quaternary lavas from the Aleutian Arc and Mt. Wrangell

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
91CND36	58.830151	-153.47529	Nye, C. J.	1991-07-26		Douglas			Another sample of host lava from the same flow as 91CND33. Porphyritic andesite. About 30% phenocrysts of millimeter-sized plagioclase, sub-millimeter-sized pyroxene and sparse olivine in a groundmass of microphenocrysts and microlite-rich glass and microcrystalline material.	91CND36	Lava			Whole-rock	60.98	0.605	17.22		0.109	3.74	6.78	3.79	1.238	0.095	101	13291	XRF		5.44			0.52088	35	364	262	3	41	2.81575	12.39384	3.38693	0.90046	3.71268	0.65574	4.1584	0.865	2.37142	0.36761	2.36115	0.37884	24	112	2.2	2.87636	0.1415	1	3	1.45565	20	151	46			22	48	59	16					13291	ICPMS: Cs, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Hf, Ta, U; XRF: Rb, Ba, Sr, La, Ce, Y, Zr, Nb, Pb, Th, Sc, V, Cr, Ni, Cu, Zn, Ga;

SAMPLE LOCATION

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