释义 |
feld·spath·oid \-ˌthȯid\ noun (-s) Etymology: International Scientific Vocabulary feldspath + -oid : a mineral consisting of an aluminous silicate (as leucite nepheline) that has too little silica to form feldspar • feld·spath·oi·dal \| ̷ ̷ˌ ̷ ̷|thȯidəl\ adjective |