Fabric Code: tpr221

Erromango feldspathic non-placer

Plagioclase-rich non-placer temper, any calcareous grains appear to be reworked limeclasts, rather than modern reef detritus.

Sites:

Mineral and Rock Abundances

None (0) Minor (1) Few (2) Common (3) Frequent (4) Major (5) Very Dominant (6)
0% 0-5% 5-15% 15-30 % 30-50% 50-70% 70-100%

Name Cal. QuartzFeldspar Pyroxene Amphibole Opaques OlivineBiotite Muscovite Epidote Garnet/ SpinelIg./Met. Rocks Sed. Rocks Grog Lithics/ Region
Max 3 0 3 4 0 3 1 0 0 0 0 3 0 0 lathwork, vitric, microlitic
Min 0 0 3 3 0 1 0 0 0 0 0 3 0 0 Vanuatu

Representative slides:

Slide Site Possible OriginCal. QuartzFeldspar Pyroxene Amphibole Opaques OlivineBiotite Muscovite Epidote Garnet/ Spinel Ig./Met. Rocks Sed. Rocks Grog Lithics
WD_57_6 Ifo (Erromango) Erromango 0 0 3 4 0 3 0 0 0 0 0 3 0 0 lathwork, vitric, microlitic
WD_57_5 Ifo (Erromango) Erromango 3 0 3 3 0 1 0 0 0 0 0 3 0 0 vitric, lathwork, microlitic, limeclast

WD_57_6

62-2 has a full slide scan available. Imaged by K. Hardy and M. Leclerc, ANU.

Plagioclase-rich non-placer temper. Stream origin. Non-Lapita.


WD_57_5

Ifo62_1 Ifo62_1
Sherd 62-1 from Ifo (Erromango). Slide WD_57_5 from Dickinson Collection, Bishop Museum. x4 Magnification PPL (left) XPL (right). Scale bar: 0.5mm. High resolution image in VIMIPO (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.

Lapita sherd. Plagioclase-rich non-placer. Calcareous grains appear to be reworked limeclasts, rather than modern reef detritus. Stream origin.


References:

147 Erromango, Vanuatu, 1998 (see 177) (Dickinson, W.)

170 Erromango, Vanuatu, Nendo, Santa Cruz group, 1998 (see 177) (Dickinson, W.)

177 Erromango, Vanuatu, correction to 147 and 170, 1998 (Dickinson, W.)