In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 19, No. 11 ( 2018-11), p. 4433-4443
Kurzfassung:
Glacial dissolution of magnetite caused glacial‐interglacial cyclicity in magnetic properties of the North Pacific sediments Magnetite dissolution during glacials was triggered by poorly ventilated glacial deep waters Poorly ventilated glacial deep waters extended up to water depths of ~2,500 m in the North Pacific
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2018GC007735
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2018
ZDB Id:
2027201-7