G109 0669A001D01007009001 0001 DIV Aphyric basalt Variolitic to microlitic Unit 1, pillow or flow interior,(cont.) Fine Olivine Tr Tr 0.3-0.6 Subhedral Plagioclase Olivine Clinopyroxene Mesostasis Opaques 29 3 11 54 0.5 29 3 11 54 0.5 51 0.05-0.2 < 0.1 ? 3-10 mirons Magnetite Acicular, bunches Euhedral, skeletal Radiating, plumose ? Anhedral-euhedral Radiating. Associated with rare ol nucleus of plag. L/W = 10-30. Generally attached to plag. Rare small grain associated with radiating plag. Product of glass devitrification. Rare euhedral crystals. Dark brown, isotropic with plag and cpx crystallites. Tiny grains distributed in the mesostasis. Vesicles 1.5 0.2-0.8 Even Rounded to irregular Miaroles in alteration halos are more commonly filled with clays than the vesicles. Empty in fresh mesostasis. Clays Carbonate Fe hydroxide 2 Tr 0.5 Mesostasis Miaroles Mesostasis Yellow birefringent clay. Aragonite, radiating. SEM photo tacken before sectioning. Both red and opaque varieties. HALO ZONE 34 mm wide Yellow clay: Strongly colored. Almost cryptocrystalline. Low birefringence. Occurs mainly as homogeneous partial fillings of miaroles. These fillings are up to 3.5 mm in extent,with groundmass plag, cpx, ol, and titanomagnetite projecting into the clay. Clay has botryoidal, locally radiate growth structure. The same clay also forms partial replacements of brown mesostasis-(?)glassy component. Replacment of mesostasis ocassionally nearly complete. Orange-red clay: Trace amounts, mainly as miarole lining. Transitioned between yellow clay and ref Few hydroxide. Red Fe hydroxide: Occurs mainly in fractures, lining vesicles and forming the central parts of miarole fillings. Vesicle linings up to 50m. Cracks < 10m wide locally spacedat 100m intervals. Occasionally occursas 330 - 50m grains attached to miarole walls, then overgrown by yellow clay. In one case, a bleb of Fe hydroxide attached to a miarole wall is continuous with a 31m thick Fe hydroxide veinlet.Cont. in main commentsWHERE SAMPLED CONTINUED: cut perpendicular to dark halo. SECONDARY MINERAL COMMENTS CONTINUED: Opaque Fe hydroxide; Occurs as central parts of two or three miarole linings. Point count of halo zone; 26 yellow clay (5%), 7 red Fe hydroxides (1.5%), 1 opaque Fe hydroxide (Tr), and 466 primary phases. Central zone (fresh); Traces of orange to red Fe hydroxide, mainly near vesicle walls. Radiating aggregates of aragonite (biaxial, low 2V, extreme birefringence) in large (5 mm), irregular miarole (also containing hopper ol). This and a smaller aragaonite-filled miarole are in connection with the halo zone. MAIN COMMENTS: Rare ol phenocrysts are rather microphenocrysts. Mesostasis is cryptocrystalline to microcrystalline with plag,cpx and ol microlites. this section might represent a coarser equivalent of Section 669A-1D-1 (Piece 2, 11-13 cm). N G109 0669A001D01011013002 0001 DIV Aphyric basalt Intergranular (felty) Unit 1, pillow or flow interior Microcrystalline to fine Olivine 0.5 0.5 0.2-0.4 Euhedral-subhedral Some embayment. Some glass inclusions. Olivine Plagioclase Clinopyroxene Mesostasis Opaques 5 26 39 21 4.5 7 26 40 21 5.5 < 0.1 < 0.1 0.1-0.3 ? << 0.1 Magnetite, sulfides Euhedral,quenched Acicular, hopper Anhedral, plumose ? Anhedral Radiating, swallow tail. Radiating, spherulites. Christmas-tree texture, product of glass devitrification. Dark brown with some cpx and plag crystallites. Very minute grains in mesostasis or cpx. Vesicles 2 0.2-0.4 Even Clays, Fe hydroxide Rounded or irregular Clays Fe hydroxide 3 1 Vesicles, miaroles, ol, cpx Opaques Yellow. Replaces olivine and clinopyroxene (staining). Reddish brown to red. Individual granules. groundmass continued: Segregation vesicle, % present = Tr, % original = Tr, size = 0.2-0.5 mm, morphology = rounded, comment = mostly devitrified glass. N G109 0669A001D01011012002 0001 DIV Aphyric basalt Spherulitic to variolitic Unit 1, pillow or flow interior Microcrystalline Olivine Tr Tr -2.5 Anhedral Yellow hydroxide attached to the phenocryst. Plagioclase Olivine Clinopyroxene Mesostasis Opaques 34 6 33 22 2 35 6 33 24 2 < 0.6 < 0.1 < 0.4 ? microns Magnetite Bundles, hopper, Euhedral,swallowtail Radiating, plumose ? Anhedral Morphology continued: acicular. COMMENTS: Radiating. Associated with cpx or attached ol. Attached to plag. Christmas-tree shape. Forms spherulites with plag or in the mesostasis. Dark brown, isotropic. Investigation under reflected light reveals plag and cpx crystallites. Minute grains distributed in the mesostasis only. Vesicles 2 0.05-0.8 Even Fe hydroxide Irregular Fe hydroxide 2 Vesicles, mesostasis Yellow to reddish brown. Associated with plag, cpx, and ol or randomly distributed in the groundmass. The granules are attached to the crystals or interfingered with cpx. Actual interval is from 11-13 cm, however the preceeding thin section had the same ID. Ol phenocrysts are in fact microphenocrysts. These are, however, different from quenched ol grains. Mesostasis is cryptocrystalline with recognizable cpx and plag in a radiating pattern. Segregation vesicles consisting of minute crystals of plag + cpx + cryptocrystalline material constitute approximately 1% of the rock. N