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SAMPLE INFO : 09KCNYE012A1

Sample ID:	09KCNYE012A1
Station ID:	09KCNYE012A1
Latitude:	52.179903
Longitude:	-175.525825
Datum:	NAD83
Date Sampled:	2009-06-14
Field Lithology:	Gabbroic

Text Description:
Several fragments from a large block w/ notably abundant interstitial melt and melt along channels - which become fracture surfaces. Melt appears to be in zones up to several mm wide. Question is: what is relation of this melt to erupted magma/scoria/pumice? Is melt bleeding out of these bodies and comint straight to surface or is there another magma zone in between? Or is athe pumice magma acting as the transporter - the bus itself - and thus must have deeper source even though it is more silicic?

References:

Petrologic and geochemical tracers of magmatic movement in volcanic arc systems: case studies from the Aleutian Islands and Kamchatka, Russia

Geology of Kasatochi volcano, Aleutian 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
09KCNYE012A1	52.179903	-175.525825	Nye, C. J.	2009-06-14		Kasatochi		Beach landing site on western edge of middle of three NW rocky points.	Several fragments from a large block w/ notably abundant interstitial melt and melt along channels - which become fracture surfaces. Melt appears to be in zones up to several mm wide. Question is: what is relation of this melt to erupted magma/scoria/pumice? Is melt bleeding out of these bodies and comint straight to surface or is there another magma zone in between? Or is athe pumice magma acting as the transporter - the bus itself - and thus must have deeper source even though it is more silicic?	09KCNYE012A1				Whole-rock	41.4107804	1.345529062	20.47558385	12.1537007	0.128520514	8.571321243	13.96955251	1.695253922	0.230975262	0.018792529	99.0920403	8831	XRF		12.1537007			0.109698824	1.413551561	62.70902272	399.220588	0.921106497	3.042804165	0.650078797	4.109096648	1.786759415	0.741368058	2.562715046	0.462445171	2.912258262	0.620332198	1.609790474	0.212013409	1.244827031	0.184509147	15.39268106	15.25403791	0.465551333	0.695384049	0.034910163	1.734396905	0.106090395	0.060107401	47.05994139	552	6.9			34.6	23.2	53.7	18.7					8831	ICPMS: 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; XRF: V, Cr, Ni, Cu, Zn, Ga;

SAMPLE LOCATION

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