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Published in 2020 at "Lithos"
DOI: 10.1016/j.lithos.2020.105373
Abstract: Abstract Mafic microgranular enclaves (MMEs) are commonly formed during magma mixing and usually record contrasting physicochemical diagenetic characteristics relative to their host rocks. We present a finding that some MMEs from the Cretaceous Qianjia pluton,…
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Keywords:
host granites;
diagenetic conditions;
magma mixing;
magma ... See more keywords