Contributions to Mineralogy and Petrology

, Volume 105, Issue 2, pp 197–218 | Cite as

Evolution of alkalic lavas at Haleakala Volcano, east Maui, Hawaii

Major, trace element and isotopic constraints
  • C. -Y. Chen
  • F. A. Frey
  • M. O. Garcia


The postshield and posterosional stages of Haleakala Volcano contain intercalated alkalic basalt and evolved alkalic lavas. Isotopic and incompatible element abundance ratios in the Haleakala postshield basalts changed systematically with time, providing evidence for significant temporal changes in the mantle components contributing to the magmatic sources. Specifically, a depleted, i.e. low87Sr/86Sr and high143Nd/144Nd, mantle component is more abundant in younger lavas. However, as magma-production rates decreased during the postshield and posterosional stages, basaltic melts in magma reservoirs cooled and fractionated, leading to evolved residual melts such as hawaiite. Because primary basalt compositions changed with time, the evolved Haleakala lavas formed from a range of parental compositions. However, basalts and evolved lavas of similar age and isotopic ratios (Sr and Nd) have major and trace element contents that are consistent with a crystal-fractionation model. Although alkalic basalt and hawaiite are the dominant lavas of the postshield stages of both Haleakala and Mauna Kea volcanoes, there are important differences between their lavas. For example, compositional differences between the hawaiite suites at Haleakala and Mauna Kea indicate that, on average, the evolved lavas at Haleakala formed at lower pressures. Also, at Haleakala basalts are intercalated with hawaiites, whereas at Mauna Kea basalts and hawaiites are separated by a sharp boundary. These differences probably reflect a higher magma supply rate to the Haleakala volcano.


Magma Reservoir Mantle Component Magma Supply Significant Temporal Change Young Lava 
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Copyright information

© Springer-Verlag 1990

Authors and Affiliations

  • C. -Y. Chen
    • 1
  • F. A. Frey
    • 2
  • M. O. Garcia
    • 3
  1. 1.Department of GeologyUniversity of IllinoisUrbanaUSA
  2. 2.Department of Earth, Atmospheric, and Planetary SciencesMITCambridgeUSA
  3. 3.Hawaii Institute of GeophysicsUniversity of HawaiiHonoluluUSA

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