A frozen oceanic crystal mush

نویسندگان

چکیده

The processes driving the evolution of crystal mushes are often documented in complex systems where crystallization, assimilation, magma replenishment and mixing occur concurrently generally overprinted by compaction deformation. Documenting characteristics an undisturbed mush is thus upmost importance; it highlights initial conditions with which proceed. We here present structure composition oceanic through detailed petro-structural chemical study metre-scale intrusions from Mid-Atlantic Ridge. Textures, bulk-rock mineral compositions indicate closed-system crystallization primitive melts, dissolution–precipitation reactions subsequent These frozen record simplest possible small-scale can be used as a baseline to pinpoint impact on systems. Any divergence this reference results occurring concomitantly progressive closure magmatic system.

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ژورنال

عنوان ژورنال: Terra Nova

سال: 2023

ISSN: ['0954-4879', '1365-3121']

DOI: https://doi.org/10.1111/ter.12655