Patrick J Wrinn
Biographic Data
| ID | 5628230 |
|---|---|
| NAME | Patrick J Wrinn |
| GIVEN NAMES | Patrick J |
| FAMILY NAME | Wrinn |
| SIGNATURE | WRINN P J |
| AFFILIATIONS | University of Arizona |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 104 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2003 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 3 |
A micromorphological and mineralogical study of site formation processes at the late Pleistocene site of Obi‐Rakhmat, Uzbekistan
Site formation processes at the Late Pleistocene rockshelter deposit of Obi‐Rakhmat were reconstructed through soil micromorphology and Fourier transform infrared spectroscopy (FTIR). The entire sequence has undergone limited diagenesis and is well preserved. The base of the stratified sequence represents a karstic setting with intermittent, low‐energy deposition of autochthonous gravitational debris and anthropogenic material in a wet, muddy env…
New hominin remains from Uzbekistan
ESR Dating of Tooth Enamel From Aterian Levels at Mugharet el ‘Aliya (Tangier, Morocco)
New hominin remains from Uzbekistan
ESR Dating of Tooth Enamel From Aterian Levels at Mugharet el ‘Aliya (Tangier, Morocco)
A micromorphological and mineralogical study of site formation processes at the late Pleistocene site of Obi‐Rakhmat, Uzbekistan
Site formation processes at the Late Pleistocene rockshelter deposit of Obi‐Rakhmat were reconstructed through soil micromorphology and Fourier transform infrared spectroscopy (FTIR). The entire sequence has undergone limited diagenesis and is well preserved. The base of the stratified sequence represents a karstic setting with intermittent, low‐energy deposition of autochthonous gravitational debris and anthropogenic material in a wet, muddy env…
ESR Dating of Tooth Enamel From Aterian Levels at Mugharet el ‘Aliya (Tangier, Morocco)
New hominin remains from Uzbekistan
A micromorphological and mineralogical study of site formation processes at the late Pleistocene site of Obi‐Rakhmat, Uzbekistan
Site formation processes at the Late Pleistocene rockshelter deposit of Obi‐Rakhmat were reconstructed through soil micromorphology and Fourier transform infrared spectroscopy (FTIR). The entire sequence has undergone limited diagenesis and is well preserved. The base of the stratified sequence represents a karstic setting with intermittent, low‐energy deposition of autochthonous gravitational debris and anthropogenic material in a wet, muddy env…
Geology (3 works) · Paleontology (3 works) · Pleistocene-Era Hominins and Archaeology (3 works) · Archaeology (2 works) · Cave (2 works) · Geography (2 works) · Geology and Paleoclimatology Research (2 works) · Mousterian (2 works) · Pleistocene (2 works) · Alluvium (1 work)