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Silicate Liquid Immiscibility within the Crystal Mush: Evidence from Ti in Plagioclase from the Skaergaard Intrusion

Abstract:

A key target in the study of layered intrusions is to constrain the liquid line of descent of the magma. However, the evolution of the interstitial liquid is rarely considered, and its liquid line of descent is often assumed to be equivalent to that of the bulk magma. Because of extensive sub-solidus and diffusional changes that occur in slowly cooled rocks, clues to the composition of the interstitial liquid can only be obtained using very slowly diffusing trace elements and components. This...

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Publication status:
Published

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Publisher copy:
10.1093/petrology/egq076
Journal:
JOURNAL OF PETROLOGY More from this journal
Volume:
52
Issue:
1
Pages:
147-174
Publication date:
2011-01-01
DOI:
EISSN:
1460-2415
ISSN:
0022-3530
Language:
English
Keywords:
Pubs id:
pubs:184896
UUID:
uuid:8cc6815c-a9c6-48e3-80f8-052d099549d1
Local pid:
pubs:184896
Source identifiers:
184896
Deposit date:
2012-12-19

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