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Published in 2017 at "American Mineralogist"
DOI: 10.2138/am-2017-6091
Abstract: Abstract Many Fe-Ti oxide bodies associated with anorthosite suites and with some tholeiitic plutonic bodies have cross-cutting relationships with their host rocks suggesting that they may have been emplaced as oxide melts. Pure Fe-Ti oxides…
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Keywords:
oxide melts;
carbon;
exist probably;
oxide magmas ... See more keywords