Geochemistry and Mineralogy of Basalts from the South Mid-Atlantic Ridge (18.0°–20.6°S): Evidence of a Heterogeneous Mantle Source

• Published in: Minerals (Basel) Vol. 9; no. 11; p. 659
• Main Authors: Zhong, Yun, Liu, Weiliang, Sun, Zhilei, Yakymchuk, Chris, Ren, Kefa, Liu, Jinnan, Li, Wei, Ma, Yaoliang, Xia, Bin
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.11.2019
• Subjects: Anomalies; Anorthite; Asthenosphere; Basalt; Composition; Crystallization; Depletion; Dredging; Enrichment; Fault lines; Forsterite; Fractionation; Geochemistry; Isotopes; Lava; Magma; Magma chambers; Mid-ocean ridges; Mineralogy; Olivine; petrogenesis; Plagioclase; Quality control; Reference materials; Rims; south mid-atlantic ridge; Trace elements; United States > US; China; Atlantic Ocean; Gondwana; Mid-Atlantic Ridge
• ISSN: 2075-163X; 2075-163X
• DOI: 10.3390/min9110659

The South Mid-Atlantic Ridge is a typical slow-spreading ridge that represents a modern example to understand mantle composition and the evolution of mid-ocean ridge magmatism. In this paper, we investigate basalt samples dredged from four locations along the South Mid-Atlantic Ridge ranging from 18.0° to 20.6°S. The basalts belong to the tholeiitic series and exhibit normal mid-ocean ridge basalt (N-MORB) geochemical features with variable enrichments of Rb, Th, U, and Pb and depletions of Ba and Sr relative to primitive mantle. Some samples have negative Nb–Ta anomalies whereas others have positive Na–Ta anomalies to average N-MORBs. Plagioclase phenocrysts, microphenocrysts, and microlites occur in the in the matrix; phenocrysts and microphenocrysts are bytownite and labradorite in composition. Olivine phenocrysts are forsterite (Fo87 to Fo96). Chemical zoning in phenocrysts are interpreted to record crystal fractionation and magma mixing. Cores of plagioclase phenocrysts have higher anorthite values (An72–83) and estimated crystallization temperatures (~1180–1240 °C) that may suggest a xenocrystic origin. The lower anorthite proportions of rims of plagioclase phenocrysts (An65–71) and microphenocrysts (An54–72) yield lower estimated crystallization temperatures of ~1090–1120 °C and ~980–1060 °C, respectively. Rims of plagioclase phenocrysts and microphenocrysts may be generated in different environments such as magma chambers or magma channels, respectively. The basalt samples probably originated from partial melting of a depleted mantle spinel lherzolite source with a minor contribution of enriched materials possibly derived from the Saint Helena plume and subcontinental lithospheric mantle in the asthenosphere. Variable compositions of the basalt samples suggest heterogeneous mantle that includes depleted and enriched components at the South Mid-Atlantic Ridge between 18.0°–20.6°S.