Composition of chromian diopside megacryst in DSDP Leg 37 basalts (Table 2, 3)
Refractory megacrysts of olivine, plagioclase, chromian diopside and Cr-Al spinel, which were not in equilibrium with the host oceanic tholeiite on eruption, are present in samples from several dredge sites and DSDP drill sites in the Atlantic and Pacific Oceans. They have multiple origins: (1) cogn...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
1977
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.708792 https://doi.org/10.1594/PANGAEA.708792 |