XRF-data (Ca and Ti) of seismites and non-seismic induced deposits from the Dead Sea center from sediment core ICDP 5017-1
Fuente:
PANGAEA
Salvato in:
| Autori principali: | , , , , , , , , , |
|---|---|
| Natura: | Dataset Open Access |
| Lingua: | en |
| Pubblicazione: |
PANGAEA
2020
|
| Soggetti: | |
| Accesso online: | |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
|
| _version_ | 1867167678628626432 |
|---|---|
| author | Lu, Yin Moernaut, Jasper Bookman, Revital Waldmann, Nicolas D Wetzler, Nadav Agnon, Amotz Marco, Shmuel Alsop, Ian G Strasser, Michael Hubert-Ferrari, Aurélia |
| author_facet | Lu, Yin Moernaut, Jasper Bookman, Revital Waldmann, Nicolas D Wetzler, Nadav Agnon, Amotz Marco, Shmuel Alsop, Ian G Strasser, Michael Hubert-Ferrari, Aurélia |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | During 2010-2011, the ICDP recovered a 457 m long Core 5017-1 from ~300 m of water depth in the center of the Dead Sea. The cored sequence is characterized by alternating laminae of white aragonite and dark detritus (aad), gypsum, and halite. U-Th and 14C dating constrain the age of the core to 220-0 ka. The surface of the archived half of the core was scanned with the ITRAX core scanner at a resolution of 1 mm, an exposure time of 1 s, and a Chromium tube at 30 kV voltage and 30 mA current at the GFZ. Here we use the XRF data (Ca and Ti) characterizing the features of seismites and non-seismic induced deposits (gypsum, halite, mud, and aragonite-detritus laminae) from the Dead Sea center. This high-resolution dataset allows us to get a better understanding of seismogenic sedimentary processes in the Quaternary Dead Sea. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_921987 |
| institution | PANGAEA |
| language | en |
| publishDate | 2020 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | XRF-data (Ca and Ti) of seismites and non-seismic induced deposits from the Dead Sea center from sediment core ICDP 5017-1 Lu, Yin Moernaut, Jasper Bookman, Revital Waldmann, Nicolas D Wetzler, Nadav Agnon, Amotz Marco, Shmuel Alsop, Ian G Strasser, Michael Hubert-Ferrari, Aurélia Ca; Dead Sea; ICDP; seismogenic sedimentary processes; turbidites; XRF scanning During 2010-2011, the ICDP recovered a 457 m long Core 5017-1 from ~300 m of water depth in the center of the Dead Sea. The cored sequence is characterized by alternating laminae of white aragonite and dark detritus (aad), gypsum, and halite. U-Th and 14C dating constrain the age of the core to 220-0 ka. The surface of the archived half of the core was scanned with the ITRAX core scanner at a resolution of 1 mm, an exposure time of 1 s, and a Chromium tube at 30 kV voltage and 30 mA current at the GFZ. Here we use the XRF data (Ca and Ti) characterizing the features of seismites and non-seismic induced deposits (gypsum, halite, mud, and aragonite-detritus laminae) from the Dead Sea center. This high-resolution dataset allows us to get a better understanding of seismogenic sedimentary processes in the Quaternary Dead Sea. |
| title | XRF-data (Ca and Ti) of seismites and non-seismic induced deposits from the Dead Sea center from sediment core ICDP 5017-1 |
| topic | Ca; Dead Sea; ICDP; seismogenic sedimentary processes; turbidites; XRF scanning |
| url | https://doi.org/10.1594/PANGAEA.921987 |