| 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 |