nepheliniticadj.

Brit.

/ˌnɛfəlᵻˈnɪtɪk/, U.S.

/ˈˌnɛfələˈnɪdɪk/

Origin: Formed within English, by derivation. Etymons: nephelinite n., -ic suffix.

Etymology: < nephelinite n. + -ic suffix; compare -itic suffix.

Geology.

Containing, resembling, or characteristic of nephelinite.

ΘΚΠ

the world > the earth > structure of the earth > constituent materials > rock > igneous rock > [adjective] > trap > basalt > other basaltic

palagonitic1867

tachylitic1888

tephritic1889

nephelinitic1909

spilitic1911

tholeiitic1922

shoshonitic1937

ankaramitic1971

1909 J. P. Iddings Igneous Rocks I. ii. ii. 386 Rocks rich in feldspar have a trachytic texture; those rich in nephelite have a nephelinitic texture.

1944 C. Palache et al. Dana's Syst. Mineral. (ed. 7) I. 733 Pegmatites of the contact zone of the nephelinitic intrusive of the Chibina tundra, Kola.

1993 Jrnl. Petrol. 34 119 Evolved alkaline liquids can be derived through extensive crystal fractionation of parental basanitic or nephelinitic magmas.

This entry has been updated (OED Third Edition, September 2003; most recently modified version published online March 2022).

单词	nephelinitic
释义	nepheliniticadj. Brit. /ˌnɛfəlᵻˈnɪtɪk/, U.S. /ˈˌnɛfələˈnɪdɪk/ Origin: Formed within English, by derivation. Etymons: nephelinite n., -ic suffix. Etymology: < nephelinite n. + -ic suffix; compare -itic suffix. Geology. Containing, resembling, or characteristic of nephelinite. ΘΚΠ the world > the earth > structure of the earth > constituent materials > rock > igneous rock > [adjective] > trap > basalt > other basaltic palagonitic1867 tachylitic1888 tephritic1889 nephelinitic1909 spilitic1911 tholeiitic1922 shoshonitic1937 ankaramitic1971 1909 J. P. Iddings Igneous Rocks I. ii. ii. 386 Rocks rich in feldspar have a trachytic texture; those rich in nephelite have a nephelinitic texture. 1944 C. Palache et al. Dana's Syst. Mineral. (ed. 7) I. 733 Pegmatites of the contact zone of the nephelinitic intrusive of the Chibina tundra, Kola. 1993 Jrnl. Petrol. 34 119 Evolved alkaline liquids can be derived through extensive crystal fractionation of parental basanitic or nephelinitic magmas. This entry has been updated (OED Third Edition, September 2003; most recently modified version published online March 2022). < adj.1909
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