Slide: FP_1_45

High quartz. Possibly Rewa Delta but may be indigenous Sigatoka sherds. Feldspars include K-feldspars as well as plagioclase. 1993 excavated samples.

Mineral and Rock Abundances

Fabric: tpr171 - Rewa Delta orogen

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%

Cal.	Quartz	Feldspar	Pyroxene	Amphibole	Opaques	Olivine	Biotite	Muscovite	Epidote	Garnet/ Spinel	Ig./Met. Rocks	Sed. Rocks	Grog	Lithics
0	5	4	1	2	1	0	0	0	0	0	1	2	0	microlitic, microphaneritic, argillitic, silstone, chert, quartzite, felsitic

Images

Sigatoka_v3_p8 — Sherd v3-p8 from Sigatoka (Viti Levu). Slide FP_1_45 from Petchey Collection, Auckland University. 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.

Sigatoka_v3_p8 — Sherd v3-p8 from Sigatoka (Viti Levu). Slide FP_1_45 from Petchey Collection, Auckland University. 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.

Sherd: v3-p8

None

Period: None wikidata:

Site: Sigatoka (Viti Levu)

Suspected origin site: Rewa Delta

References:

Petchey MA Thesis 1995 (Petchey, F.)