Balneaves
Soil Thin Sections
Bibliographic Data
| ID | 11003310 |
|---|---|
| Authors | Donald A Davidson (corresponding author), Donald Davidson |
| Year | 1992 |
| Volume | 58 |
| Issue | S2 |
| Pages | 23-25 |
| Publication date | 1992-01-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Proceedings of the Prehistoric Society (JOURNAL) |
| Journal identifiers | ISSN: 0079-497X • E-ISSN: 2050-2729 |
| Publisher | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/s0079497x00079172 |
| OpenAlex | W2945533053 |
| Language | EN |
1. Structure: partially accommodated channels (0.16 to 0.80mm in width) above the pan; no aggregates; fewer channels below the pan; channel pattern - straight to curved; vughs (spherical to elongate, not normally connected) 0.4 to 0.8mm in diameter and are not orientated and have random pattern: above pan channels and vughs partially connected; pellicular grain microstructure - weakly developed. 2. Mineral components: coarse fraction: quartz grains range in size from silt to fine/medium sand (
Biotite · Composite material · Geomorphology · Grain size · Isotropy · Microstructure · Mineralogy · Optics · Physics · Plagioclase · Quartz · Silt · Geology · Geotechnical and construction materials studies · Landslides and related hazards · Materials Science
| Highly cited | No |
|---|