Guardado en:
| Autores principales: | , , , , |
|---|---|
| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
1990
|
| Materias: | |
| Acceso en línea: | https://doi.org/10.1594/PANGAEA.746033 |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| _version_ | 1867171360253411328 |
|---|---|
| author | Hieke, Werner Glacon, Georgette Hasegawa, Shiro Müller, Carla Peypouquet, Jean Pierre |
| author_facet | Hieke, Werner Glacon, Georgette Hasegawa, Shiro Müller, Carla Peypouquet, Jean Pierre |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Twenty-three sediment intervals from top of Site 650 down to 510 m below seafloor have been studied. Their thicknesses vary between 0.25 m and about 40 m. The studied deposits are turbidites or parts of them except one which is interpreted as an ash-fall layer. The composition of the turbidites signalizes sources from shallow water/coastal areas as well as from deep water levels. Repeated mobilization and displacement seems to have been common. Volcaniclastic material is the dominant component of the whole studied part of Site 650 sedimentary sequence. Ashfall deposits as well as normal open marine sediments are rare. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_746033 |
| institution | PANGAEA |
| language | en |
| publishDate | 1990 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Benthic foraminifera and ostracoda in ODP Hole 107-650A Hieke, Werner Glacon, Georgette Hasegawa, Shiro Müller, Carla Peypouquet, Jean Pierre 107-650A; DRILL; Drilling/drill rig; Joides Resolution; Leg107; Ocean Drilling Program; ODP; Tirreno Sea Twenty-three sediment intervals from top of Site 650 down to 510 m below seafloor have been studied. Their thicknesses vary between 0.25 m and about 40 m. The studied deposits are turbidites or parts of them except one which is interpreted as an ash-fall layer. The composition of the turbidites signalizes sources from shallow water/coastal areas as well as from deep water levels. Repeated mobilization and displacement seems to have been common. Volcaniclastic material is the dominant component of the whole studied part of Site 650 sedimentary sequence. Ashfall deposits as well as normal open marine sediments are rare. |
| title | Benthic foraminifera and ostracoda in ODP Hole 107-650A |
| topic | 107-650A; DRILL; Drilling/drill rig; Joides Resolution; Leg107; Ocean Drilling Program; ODP; Tirreno Sea |
| url | https://doi.org/10.1594/PANGAEA.746033 |