Rock magnetic identification and geochemical process models of greigite formation in Quaternary marine sediments from the Gulf of Mexico (IODP Hole U1319A)
A 160 m mostly turbiditic late Pleistocene sediment sequence (IODP Expedition 308, Hole U1319A) from the Brazos-Trinity intraslope basin system off Texas was investigated with paleo- and rock magnetic methods. Numerous layers depleted in iron oxides and
|Collections||ANU Research Publications|
|Source:||Earth and Planetary Science Letters|
|01_Fu_Rock_magnetic_identification_2008.pdf||3.29 MB||Adobe PDF||Request a copy|
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