Abyssal tholeiites from the Oceanographer Fracture Zone |
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Authors: | David Walker Tsugio Shibata Stephen E DeLong |
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Institution: | (1) Hoffman Laboratory, Harvard University, 02138 Cambridge, Massachusetts, USA;(2) Department of Earth Sciences, Okayama University, Tsushima, 700 Okayama, Japan;(3) Department of Geological Sciences, State University of New York at Albany, 12222 Albany, New York, USA |
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Abstract: | Unusual effects have been discovered in the major element phase relations of basalts from the Oceanographer Fracture Zone
(OFZ) which suggest that magma mixing of primitive basalt with the differentiation residue of a previous batch of primitive
magma has occurred. These effects include a reversal in mineral crystallization sequence which cannot happen during normal
differentiation processes or be explained by any plausible change in physical conditions. This unusual effect is encountered
as a result of curvature in composition space of the liquid-line-of-descent equilibria involving olivine, plagioclase, and
high-calcium clinopyroxene. Mixing of magmas at different stages of their evolution produces mixtures that do not lie on the
curved liquid-line-of-descent. Observation of such anomalous compositions in the OFZ suite supplements accumulating petrographic
and trace-element geochemistry evidence that magma mixing is an important petrogenetic process.
Mixing of fractionated residual liquids can produce mixtures which are either superheated or supercooled depending on the
sense of ‘thermal curvature’ of the liquid-line-of-descent. Both senses are encountered in the tholeiitic system, and this
effect may exert a qualitative control on the crystallization texture of the mixture.
A comparison of approximately 2,000 abyssal tholeiite compositions to the experimental liquid-line-of-descent reveals that
erupted differentiates which would be expected from advanced fractionation are scarce. Just this sort of phenomenon (the ‘perched’
steady state) was proposed by O'Hara (1977) as an earmark of the operation of a continuously fractionating magma chamber into
which fresh magma is periodically remixed. |
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