Open AccessNew insights into the origin and distribution of the DUPAL isotope anomaly in the Indian Ocean mantle from MORB of the Southwest Indian Ridge
Author(s) -
Meyzen Christine M.,
Ludden John N.,
Humler Eric,
Luais Béatrice,
Toplis Michael J.,
Mével Catherine,
Storey Michael
Publication year - 2005
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2005gc000979
Subject(s) - geology , triple junction , mantle (geology) , ridge , subduction , basalt , magnetic anomaly , mid ocean ridge , plate tectonics , oceanic crust , seafloor spreading , isotopic signature , geochemistry , tectonics , isotope , oceanography , paleontology , physics , quantum mechanics
We report new Sr, Nd, and Pb isotope data for Mid‐Ocean Ridge Basalts (MORB) dredged between 35 and 69°E along a ∼4100 km section of the Southwest Indian Ridge (SWIR), which is one of the slowest spreading ridges of the global mid‐ocean ridge system (full rate of 16 mm yr −1 ). The SWIR appears isotopically more heterogeneous than other mid‐ocean ridges over similar length scales and comparable sampling density. Isotopic variations are generally independent of ridge segmentation, and the degree of heterogeneity decreases from west to east. This decrease in heterogeneity correlates with the observed increase in axial depth and decrease in crustal thickness, commonly attributed to decreasing mantle potential temperature. Data for the easternmost SWIR in the vicinity of the Indian Triple Junction confirm that these lavas are isotopically distinct from those of the Triple Junction, the Southeast Indian Ridge, and the Central Indian Ridge, reflecting the presence of an isotopic boundary over an along‐axis distance of less than 78 km. Results for lavas from the 39–41°E section extend the isotopic range of MORB to the lowest 206 Pb/ 204 Pb values (to 16.58) yet found among oceanic islands and spreading centers worldwide and confirm their extremely anomalously high 87 Sr/ 86 Sr, 207 Pb/ 204 Pb, and 208 Pb/ 204 Pb and low 143 Nd/ 144 Nd. This extreme Indian signature does not bear any isotopic affinities with recent products of the nearby Marion hot spot. Furthermore, the presence of old subducted marine sediment as a source for the low 206 Pb/ 204 Pb component is excluded, as no sediment group has the appropriate parent‐daughter Th/Pb and U/Pb characteristics to yield such compositions, not even when dewatering subduction processes are considered. Incorporation of old subduction‐modified mantle into the MORB source does not yield high enough 207 Pb/ 204 Pb and 208 Pb/ 204 Pb to explain the features of lavas from the 39–41°E section. The unusual isotopic attributes of this section (low 206 Pb/ 204 Pb and 143 Nd/ 144 Nd and high 87 Sr/ 86 Sr, 207 Pb/ 204 Pb, and 208 Pb/ 204 Pb) are best explained by the presence of stranded lower continental crust embedded in the upper mantle. This component is also inferred to be present in MORB from other spreading centers in the Indian Ocean.