A xenolith with green monoclinic pyroxene in the andesite from Misumi-dake, Kumamoto Pref
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چکیده
منابع مشابه
The Origin of Co-Magmatic Andesite Enclaves in the Rabor Miocene Pyroxene Andesites, SE Kerman, Iran: Insights from Textural and Mineralogical Composition
The Miocene pyroxene andesite lava flows are exposed in southeastern edge of Urumieh Dokhtar Magmatic assemblage in Iran. The hypocrystalline andesite in parts contain conspicuous co-magmatic igneous enclaves which are dark grey and occur mostly as spherical and occasionally as ribbon shapes with some showing chilled margins. Petrographic study shows that the ribbon type enclaves have been form...
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چکیده ندارد.
15 صفحه اولDake-wa : Exhaustifying Assertions
Following the structure meaning approach (c.f. [3,4]), I argued in [5] that the prosodic peak of Contrastive-marking creates a partition of the asserted proposition into B (background) and F (Focus). The morphological wa-marking then introduces the Con operator that takes the structured meaning as its argument and yields a conventional implicature. The Contrastive-marked sentence presupposes th...
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Grossmanite, Ca(Ti,Mg,Ti)AlSiO6 with an end-member formula CaTiAlSiO6, is a new member of the Ca clinopyroxene group, where the trivalent cations are dominant in the M1 site with Ti3+ being the dominant trivalent cation. It occurs as micrometer-sized crystals along with spinel and perovskite in a melilite host in Ca-,Al-rich refractory inclusions from the Allende meteorite. The mean chemical co...
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ژورنال
عنوان ژورنال: The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists
سال: 1949
ISSN: 0021-4825,1883-0765
DOI: 10.2465/ganko1941.33.62