G111 0504B142R01006008001A0151 CMS Moderately plagioclase clinopyroxene phyric basalt Intergranular, subophitic Unit 151 Fine Plagioclase Clinopyroxene 8 1 8 1 0.2-2.0 1-2 An 54 Diopside/Augite Euhedral, tabular Subhedral Occur as glomerocrysts and single crystals. Sometimes together with cpx. Strained (wavy extinction). Minor alteration to actinolite along cleavage traces. Occurs as glomerocrysts with plag. Plagioclase Clinopyroxene Olivine Magnetite 35 30 none 1 41 36 3 1 150 microns75 microns 75 microns 35 microns An 45 Euhedral, bladed Subhedral Subhedral Subhedral Replaced in part by chlorite(?), clays. Replaced in part by clays(?), actinolite(?). Replaced by chlorite, talc, clays(?). Vesicles 0 Clays Chlorite Actinolite Sphene Magnetite Pyrite(?) Talc Chlorite, actinolite9 4 3 Tr 8 0.2 0.8 Tr Plag. Olivine, plag. Cpx Magnetite(?) Olivine, cpx Olivine Olivine, cpx Veins Plag replaced, especially in vugs. Especially in vugs. Especially in vugs. Minor veins, 50 micron wide, of chlorite, actinolite, and possibly quartz, occur in the section. Although the rock is generally fine grained, it has a patchy appearance with patches or "vugs" up to 2 mm in which alteration minerals, chlorite, magnetite, and clays, are concentrated. Magnetite concentration in the matrix occurs around radiating plag laths and may represent devitrification of original glassy mesostasis. Y G111 0504B142R01009012001R0152 DIV Highly plagioclase clinopyroxene olivine phyric basalt Chilled margin, hypohyaline Chilled margin, unit 152 Glass + phenocrysts. Hyaline. Olivine Plagioclase Clinopyroxene 5 20 7 9 20 7 < 0.5-2.5 < 0.1-2.8 < 0.5-2.5 Fo 85 An 65(??) Augite/diopside Salitic Euhedral-subhedral Euhedral Euhedral, resorbed Altered to 1) Mixed-layer clays + talc + magnetite; 2) Chlorite + talc + magnetite + actinolite. Single crystals or glomerocrysts. Glass inclusions in centers. Glomerocrysts with plag, and single crystals. Reaction with glass; 0.05 mm rims. Glass inclusions up to 50 microns. Basal twins common. Glass Plagioclase 0 2 53 12 ? 20 microns ? Euhedral Now smectite + chlorite + oxides. Microlites. Vesicles 0 Clays Chlorite Actinolite Sphene Quartz Oxides Talc Chlorite 25 19.1 0.2 (?) (?) 21.5 0.2 Tr Ol, matrix Ol, matrix Ol Ol, matrix Ol Veins ~ 2% replacing ol. ~ 1% replacing ol. Replaces ol together with chlorite. Mainly magnetite and hematite. Replaces groundmass. Replaces ol. Chlorite filled fracture (0.5 mm) with quartz + minor actinolite + possible sulfide. Phenocrysts of plag, plag + cpx, and plag + ol commonly occur in glomerocrysts. Cpx + ol are resorbed in places. Plag + cpx commonly have glass inclusions, 40-80 microns. Ol alteration occcured first along crystal margins and then along fractures. Phenocrysts are often broken. Chilled margin: Pyrite intergrown with chalcopyrite, chalcopyrite inclusions in pyrite, pyrite intergrown with magnetite, small pyrrhotite inclusions in pyrite. Thin section is taken at contact between two basaltic dike units. Unit 152 is clearly chilled compared to unit 151. Unit 152 shows altered glassy contact, 2 mm wide, grading into altered glassy mesostasis with microlites of plag. Oxide + smectite + chlorite alteration. Intrusion permissive since no rip-ups of older unit in chill. Cpx in reaction relationship with glass; resorbed margins and numerous glass inclusions. Plag phenocrysts (core An 65) show normal zoning towards outside third of crystals. Also have glass inclusions in centers. N G111 0504B142R01009012001B0151 CMS Moderately plagioclase clinopyroxene phyric basalt Subophitic (diabasic) Contact unit 151 Fine to aphanitic Plagioclase Clinopyroxene 6 <1 6 <1 0.3-1.0 0.5 An 45 Euhedral-subhedral Euhedral Zone Marginal 1/10 of crystals. Glomerocrysts. Only one phenocryst represented. Appears fresh. Plagioclase Clinopyroxene Oxides 45 25 2 50 42 2 <0.1-0.5 0.1 <0.1-0.2 An 40 Augite Magnetite(?) Acicular, bladed Stubby, subhedral Anhedral Altered in part to clays (+/- talc?). Altered to oxides/chlorite/clays. Vesicles 0 Clays Chlorite Actinolite Sphene Oxides 6 6 <2 <1 7 Cpx, plag Cpx Cpx (?) Cpx Alteration predominantly of groundmass cpx, and some plag. Alteration of groudmass cpx. Cpx in groudmass replaced in part. Somewhat patchy distribution. Small, euhedral, high relief crystals, possibly sphene in groudmass. Patchy. Occurs with chlorite in some aggregates, ~ 20-30% altered. These patches ~ 1 mm. Slightly finer grain size. Generally due to alteration of cpx. Unit 151. This thin section is problably not representative of the unit. Thre is no record of ol phenocrysts which are described in the lithological description. Likewise for cpx. Plag phenocrysts problably underestimated in lithological description. In so far as plag concerned, almost seriate porphyritic since maximum groundmass plag is larger than minimum phenocryst. See 111-504B-142R-1 (Piece 1A, 6-8 cm). Note: patchy clots of oxides + chlorite + clays +/- actinolite may represent altered areas of finer groundmass. N G111 0504B142R01101104015 0153 DIV Moderately plagioclase clinopyroxene olivine phyric basalt basaltic Cataclatsic (30-40% clasts) Contact between dike + breccia unit 153 Very fine to fine Olivine Plagioclase Clinopryoxene < 1 4 < 1 < 1 6 < 1 40 2(?) 8 ? ? ? ? ? ? ? ? Minor alteration to clays, chlorite. Minor alteration to chlorite, actinolite. Altered to actinolite +/- chlorite(?). Some monor alteration to sphene. Vesicles 0 Clays Chlorite Actinolite Pyrite 2.5 3 3 < 1 Plag Cpx, ol Ol Ol Minor replacement of plag. minor amounts in plag Minor replacement of groundmass cpx. Pseudomorphs after olivine. Very minbor alteration of ol. Groundmass is fine grained (microlitic texture), and essentially looks like porphyritic volcanic basalt. This could be due to sample proximity to chilled margin of dike. the amount of matrix alteration is difficult to estimate, probably ~ 5%. N G111 0504B150R01113115022A0167 DIV Sparsely plagioclase olivine phyric basalt Subophitic Unit 167 Fine to medium Olivine Plagioclase 0 < 2 < 2 3 ? 2 ? Tabular Altered to mixed-layer clays + talc + pyrite+ actinolite. Patchy extinction. Plagioclase Clinopyroxene Opaques 35 50 < 5 35 50 5