A compositionally nearly steady-state magma chamber at the Costa Rica rift: evidence from basalt glass and mineral data, Deep Sea Drilling Project sites 501, 504, and 505.

J. H. Natland; A. C. Adamson; C. Laverne; W. G. Melson; T. O'Hearn

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A compositionally nearly steady-state magma chamber at the Costa Rica rift: evidence from basalt glass and mineral data, Deep Sea Drilling Project sites 501, 504, and 505.

Natland J
Adamson A
Laverne C
et al.

Initial Reports of the D.S.D.P. (1983) 69 811-858

DOI: 10.2973/dsdp.proc.69.154.1983

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Abstract

The compositions of glasses and phenocrysts in basalts suggest a periodically replenished axial magma chamber. Repeatedly erupted lavas had a remarkably uniform composition.-K.A.R.

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Natland, J. H., Adamson, A. C., Laverne, C., Melson, W. G., & O’Hearn, T. (1983). A compositionally nearly steady-state magma chamber at the Costa Rica rift: evidence from basalt glass and mineral data, Deep Sea Drilling Project sites 501, 504, and 505. Initial Reports of the D.S.D.P., 69, 811–858. https://doi.org/10.2973/dsdp.proc.69.154.1983

A compositionally nearly steady-state magma chamber at the Costa Rica rift: evidence from basalt glass and mineral data, Deep Sea Drilling Project sites 501, 504, and 505.

Abstract

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