A I Ortega
Biographic Data
| ID | 3807608 |
|---|---|
| NAME | A I Ortega |
| GIVEN NAMES | A I |
| FAMILY NAME | Ortega |
| SIGNATURE | ORTEGA A I |
| AFFILIATIONS | Universidad de Burgos |
| VERIFIED | No |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 72 |
| WORKS AS AUTHOR | 7 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1990 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 3 |
Comparing depositional modes of cave sediments using magnetic anisotropy
Comparison of speleothem fabrics and microstratigraphic stacking patterns in calcite stalagmites as indicators of paleoenvironmental change
Pleistocene sedimentary facies of the Gran Dolina archaeo-paleoanthropological site (Sierra de Atapuerca, Burgos, Spain)
Applying electrical resistivity tomography to the identification of endokarstic geometries in the Pleistocene Sites of the Sierra de Atapuerca (Burgos, Spain)
In this paper we have applied the electrical resistivity tomography (ERT) in order to prospect and to analyse the morphological and geological subsurface of the Torcas‐Cueva Mayor endokarst system (Sierra de Atapuerca). These works are essential to establish the development of the sedimentary infills where the Early and Middle Pleistocene archaeo‐palaeoanthropological sites of the Sierra de Atapuerca are located. The prospecting was based on the …
Characterizing the Sedimentary History of Cave Deposits, Using Archaeomagnetism and Rock Magnetism, Atapuerca (Northern Spain)
We use a combination of rock magnetism (anisotropy of magnetic susceptibility, AMS) and magnetic polarity to characterize cave deposits and as a proxy for sedimentary fabric. In three localities at the Atapuerca archaeological site (Galeria, Gran Dolina and Sala de los Cíclopes), magnetic foliation (K max /K int ) is always greater than lineation (K int /K min ), consistent with a primary, depositional, sedimentary fabric. Our results, although p…
Sima de los Huesos (Sierra de Atapuerca, Spain). The site
The Atapuerca sites and the ibeas hominids
Pleistocene sedimentary facies of the Gran Dolina archaeo-paleoanthropological site (Sierra de Atapuerca, Burgos, Spain)
The Atapuerca sites and the ibeas hominids
Applying electrical resistivity tomography to the identification of endokarstic geometries in the Pleistocene Sites of the Sierra de Atapuerca (Burgos, Spain)
In this paper we have applied the electrical resistivity tomography (ERT) in order to prospect and to analyse the morphological and geological subsurface of the Torcas‐Cueva Mayor endokarst system (Sierra de Atapuerca). These works are essential to establish the development of the sedimentary infills where the Early and Middle Pleistocene archaeo‐palaeoanthropological sites of the Sierra de Atapuerca are located. The prospecting was based on the …
Comparing depositional modes of cave sediments using magnetic anisotropy
Characterizing the Sedimentary History of Cave Deposits, Using Archaeomagnetism and Rock Magnetism, Atapuerca (Northern Spain)
We use a combination of rock magnetism (anisotropy of magnetic susceptibility, AMS) and magnetic polarity to characterize cave deposits and as a proxy for sedimentary fabric. In three localities at the Atapuerca archaeological site (Galeria, Gran Dolina and Sala de los Cíclopes), magnetic foliation (K max /K int ) is always greater than lineation (K int /K min ), consistent with a primary, depositional, sedimentary fabric. Our results, although p…
The Atapuerca sites and the ibeas hominids
Sima de los Huesos (Sierra de Atapuerca, Spain). The site
Applying electrical resistivity tomography to the identification of endokarstic geometries in the Pleistocene Sites of the Sierra de Atapuerca (Burgos, Spain)
In this paper we have applied the electrical resistivity tomography (ERT) in order to prospect and to analyse the morphological and geological subsurface of the Torcas‐Cueva Mayor endokarst system (Sierra de Atapuerca). These works are essential to establish the development of the sedimentary infills where the Early and Middle Pleistocene archaeo‐palaeoanthropological sites of the Sierra de Atapuerca are located. The prospecting was based on the …
Characterizing the Sedimentary History of Cave Deposits, Using Archaeomagnetism and Rock Magnetism, Atapuerca (Northern Spain)
We use a combination of rock magnetism (anisotropy of magnetic susceptibility, AMS) and magnetic polarity to characterize cave deposits and as a proxy for sedimentary fabric. In three localities at the Atapuerca archaeological site (Galeria, Gran Dolina and Sala de los Cíclopes), magnetic foliation (K max /K int ) is always greater than lineation (K int /K min ), consistent with a primary, depositional, sedimentary fabric. Our results, although p…
Pleistocene sedimentary facies of the Gran Dolina archaeo-paleoanthropological site (Sierra de Atapuerca, Burgos, Spain)
Comparison of speleothem fabrics and microstratigraphic stacking patterns in calcite stalagmites as indicators of paleoenvironmental change
Comparing depositional modes of cave sediments using magnetic anisotropy
Geology (7 works) · Paleontology (7 works) · Archaeology (6 works) · Cave (6 works) · Geography (6 works) · Pleistocene-Era Hominins and Archaeology (5 works) · Geology and Paleoclimatology Research (4 works) · Pleistocene (4 works) · Sedimentary rock (4 works) · Structural basin (4 works)