hypabyssaladj.

/hʌɪpəˈbɪsəl/

Etymology: < German hypabyssisch (attributed by H. Rosenbusch 1891, in Tschermak's min. u. petrogr. Mittheil. XII. 386, and by W. C. Brögger Die Eruptivgesteine des Kristianiagebietes (1894) iii. 123, to Brögger, 1886): see hypo- prefix 1d.

Geology.

Of igneous rock: formed from magma which has intruded into and solidified among other rocks; intermediate between plutonic and volcanic.

ΘΚΠ

the world > the earth > structure of the earth > constituent materials > rock > igneous rock > [adjective] > hypabyssal

hypabyssal1895

1895 Mineral. Mag. 11 115 It [sc. sölvsbergite] is a true dyke-rock (‘hypabyssal’ rock).

1896 Science Progress IV. 476 Brögger has insisted on the necessity of a division intermediate between the plutonic and the volcanic, which he terms ‘hypabyssal’.

1896 Q. Jrnl. Geol. Soc. 52 613 The laccolitic rocks..would seem to belong to what Prof. Brögger calls hypabyssal.

1903 A. Geikie Text-bk. Geol. (ed. 4) 197 Dyke-rocks..which may have been injected as dykes and veins at a less distance from the surface (hypabyssal).

1924 J. G. A. Skerl tr. A. Wegener Orig. Continents & Oceans 135 Hypabyssal igneous rocks.

1926 G. W. Tyrrell Princ. Petrol. vi. 106 The hypabyssal group includes the rocks of dykes, sills, and small laccoliths, etc., which occupy an intermediate position in the crust between the deepseated plutonic bodies, and the surficial lava flows.

1951 F. J. Turner & J. Verhoogen Igneous & Metamorphic Petrol. iii. 51 Some writers recognize an intermediate (hypabyssal) class to include rocks that have crystallized at moderate depth.

1969 G. M. Bennison & A. E. Wright Geol. Hist. Brit. Isles x. 251 The Great Whin Sill is the largest hypabyssal intrusion in Britain.

This entry has not yet been fully updated (first published 1976; most recently modified version published online September 2019).

单词	hypabyssal
释义	hypabyssaladj. /hʌɪpəˈbɪsəl/ Etymology: < German hypabyssisch (attributed by H. Rosenbusch 1891, in Tschermak's min. u. petrogr. Mittheil. XII. 386, and by W. C. Brögger Die Eruptivgesteine des Kristianiagebietes (1894) iii. 123, to Brögger, 1886): see hypo- prefix 1d. Geology. Of igneous rock: formed from magma which has intruded into and solidified among other rocks; intermediate between plutonic and volcanic. ΘΚΠ the world > the earth > structure of the earth > constituent materials > rock > igneous rock > [adjective] > hypabyssal hypabyssal1895 1895 Mineral. Mag. 11 115 It [sc. sölvsbergite] is a true dyke-rock (‘hypabyssal’ rock). 1896 Science Progress IV. 476 Brögger has insisted on the necessity of a division intermediate between the plutonic and the volcanic, which he terms ‘hypabyssal’. 1896 Q. Jrnl. Geol. Soc. 52 613 The laccolitic rocks..would seem to belong to what Prof. Brögger calls hypabyssal. 1903 A. Geikie Text-bk. Geol. (ed. 4) 197 Dyke-rocks..which may have been injected as dykes and veins at a less distance from the surface (hypabyssal). 1924 J. G. A. Skerl tr. A. Wegener Orig. Continents & Oceans 135 Hypabyssal igneous rocks. 1926 G. W. Tyrrell Princ. Petrol. vi. 106 The hypabyssal group includes the rocks of dykes, sills, and small laccoliths, etc., which occupy an intermediate position in the crust between the deepseated plutonic bodies, and the surficial lava flows. 1951 F. J. Turner & J. Verhoogen Igneous & Metamorphic Petrol. iii. 51 Some writers recognize an intermediate (hypabyssal) class to include rocks that have crystallized at moderate depth. 1969 G. M. Bennison & A. E. Wright Geol. Hist. Brit. Isles x. 251 The Great Whin Sill is the largest hypabyssal intrusion in Britain. This entry has not yet been fully updated (first published 1976; most recently modified version published online September 2019). < adj.1895
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