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Recommendations for using XRF core scanning as a tool in tephrochronology

The Holocene, 2012
X-ray fluorescence (XRF) core scanning is a relatively new arrangement of a classic analytical technique which allows for non-destructive, in situ XRF analysis of sediment cores from submillimetre resolution upwards. In this contribution we explore the use of XRF core scanning for tephrochronology based on the analysis of three gyttja-rich sediment ...
M. Kylander   +3 more
semanticscholar   +2 more sources

Chemostratigraphy of Triassic successions on the southern Barents Sea Shelf – preliminary results from XRF Core Scanning.

, 2020
The Barents Sea Shelf on the north-western corner of the Eurasian plate has a complex geological history, comprising large-scale processes controlled by plate movements, climatic variations and changing depositional environments. During the last decades,
Sigrun Maret Kvendbø Hegstad   +3 more
semanticscholar   +2 more sources

Paleoenvironmental reconstruction of the southeast Red Sea based on XRF core scanning data and complementary environmental proxies


Σε μια εποχή εντεινόμενης κλιματικής μεταβολής, η νότια Ερυθρά Θάλασσα προσφέρει ένα σπάνιο ιζηματογενές αρχείο για την αποκωδικοποίηση του τρόπου με τον οποίο τα οριακά θαλάσσια συστήματα ανταποκρίνονται στην αλληλεπίδραση υδρολογικών φαινομένων, ανόδου
Φραντζέσκα Παράσχου
semanticscholar   +2 more sources

EXTREMELY HIGH RESOLUTION XRF CORE SCANNING REVEALS THE EARLY TRIASSIC EVOLUTION OF THE WESTERN PANGAEAN MARGIN

Geological Society of America Abstracts with Programs, 2020
S. Schoepfer   +3 more
semanticscholar   +2 more sources

CONTINENTAL RESPONSES TO THE EARLY EOCENE CLIMATIC OPTIMUM: A HIGH-RESOLUTION PERSPECTIVE FROM THE GREEN RIVER FORMATION USING XRF CORE SCANNING

Geological Society of America Abstracts with Programs, 2019
Andrew P Walters   +5 more
semanticscholar   +2 more sources

Digging into Eocene hothouse climate variability: Linking X-ray fluorescence (XRF) scanning and palynology of Messel sediment cores

2021
The late early to early middle Eocene (~48 Ma) maar lake sediments of the famous Messel fossil-pit, located near Darmstadt, SW Germany, represent a prime archive for climate dynamics operating during the geologically most recent greenhouse period of the Earth.
Kaboth-Bahr , Stefanie   +5 more
openaire   +1 more source

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