Lecture 9: Oceanic Basalts

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DMM

CHUR

HIMU

EM2

EM1

From: Hofmann, Nature 385, 219-229 (1997)

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MORB OIB 143 Nd/ 144 Nd Depleted Quadrant CHUR or ε Nd Enriched Quadrant Continental Crust 87 Sr/ 86 Sr OIB MORB Continental Crust or ε Sr 650 km Transition Zone Depleted Upper Mantle Primordial Lower Mantle

DMM CHUR HIMU EM2 EM1 From: Hofmann, Nature 385, 219-229 (1997)

Page 1 and 2: Lecture 9: Oceanic Basalts
Page 3 and 4: Rb, Sr, Nd and Sm are all incompati
Page 5 and 6: Concentrate solely on oceanic basal
Page 7 and 8: MORB - Relatively homogeneous sourc
Page 9: OIB - Source La Lu LREE depleted Ba
Page 13 and 14: Eiler et al. (1996) Geochim Cosmoch
Page 15 and 16: Continental Crust
Page 17 and 18: The DUPAL Anomaly Δ7/4 > 11 Δ7/4>
Page 19 and 20: 250 N 200 150 MORB 100 50 OIB Primo
Page 21 and 22: Kárason & van der Hilst (2000) AGU
Page 23 and 24: A Numerical Model (Van Keken and Ba

Lecture 9: Oceanic Basalts

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