Basalts from DSDP Sites 248, 249, 250 and 251 in the southwestern Indian Ocean formed in a complex tectonic region affected by the separation of Africa and South America. The different ages and variable geochemical features of these DSDP basalts probably reflect this tectonic complexity. For example, Site 251 on the flanks of the Southwest Indian Ridge is represented by normal MORB which probably originated at the Southwest Indian Ridge. Site 250 in the Mozambique Basin includes an older incompatible- element enriched unit which may represent basalt associated with the Prince Edward Fracture Zone; the upper unit is normal MORB. Basalts at Site 248 also in the Mozambique Basin are geochemically very unlike MORB and have strong continental af...
The Mozambique Ridge (MozR), a prominent basement high in the southwestern Indian Ocean, consists of...
A comparison of geochemical and Sr-Nd-Pb isotopic compositions for Deccan Continental Flood Basalts ...
Basalts forming the floor of the Indian Ocean are geochemically distinct from those of the Atlantic ...
The Mozambique Ridge (120-140 Ma old) is a submarine plateau located in the southwest Indian Ocean. ...
Leg 115 of the Ocean Drilling Program recovered basalts from four locations along the hotspot track ...
The SO-232 cruise took place in April-May 2014 at the Mozambique Ridge, a presumably 120-140 Ma-old ...
A comparison of new and published geochemical characteristics of magmatism in the western and easter...
DSDP Leg 82 drilled nine sites to the southwest of the Azores Islands on the west flank of the Mid-A...
The Mozambique Ridge (MOZR) is one of several bathymetric highs formed in the South African gateway ...
Basement rocks were recovered at four sites on Leg 115 along the Reunion hotspot track in the wester...
The Mozambique Ridge, a prominent basement high in the southwestern Indian Ocean, consists of four m...
The Rodrigues Ridge is a linear east-west trending volcanic ridge, located between 18°S and 20°S in ...
The Mozambique Ridge, a prominent basement high in the southwestern Indian Ocean, consists of four m...
During Deep Sea Drilling Project Leg 73 (South Atlantic), basaltic pillow lava, flows, and sills wer...
Deep Sea Drilling Project Leg 74 drilled basement on the Walvis Ridge at Sites 525, 527, and 528. Th...
The Mozambique Ridge (MozR), a prominent basement high in the southwestern Indian Ocean, consists of...
A comparison of geochemical and Sr-Nd-Pb isotopic compositions for Deccan Continental Flood Basalts ...
Basalts forming the floor of the Indian Ocean are geochemically distinct from those of the Atlantic ...
The Mozambique Ridge (120-140 Ma old) is a submarine plateau located in the southwest Indian Ocean. ...
Leg 115 of the Ocean Drilling Program recovered basalts from four locations along the hotspot track ...
The SO-232 cruise took place in April-May 2014 at the Mozambique Ridge, a presumably 120-140 Ma-old ...
A comparison of new and published geochemical characteristics of magmatism in the western and easter...
DSDP Leg 82 drilled nine sites to the southwest of the Azores Islands on the west flank of the Mid-A...
The Mozambique Ridge (MOZR) is one of several bathymetric highs formed in the South African gateway ...
Basement rocks were recovered at four sites on Leg 115 along the Reunion hotspot track in the wester...
The Mozambique Ridge, a prominent basement high in the southwestern Indian Ocean, consists of four m...
The Rodrigues Ridge is a linear east-west trending volcanic ridge, located between 18°S and 20°S in ...
The Mozambique Ridge, a prominent basement high in the southwestern Indian Ocean, consists of four m...
During Deep Sea Drilling Project Leg 73 (South Atlantic), basaltic pillow lava, flows, and sills wer...
Deep Sea Drilling Project Leg 74 drilled basement on the Walvis Ridge at Sites 525, 527, and 528. Th...
The Mozambique Ridge (MozR), a prominent basement high in the southwestern Indian Ocean, consists of...
A comparison of geochemical and Sr-Nd-Pb isotopic compositions for Deccan Continental Flood Basalts ...
Basalts forming the floor of the Indian Ocean are geochemically distinct from those of the Atlantic ...