Citations:tectotype

English citations of tectotype

1913, The Victorian Naturalist (Volume 29, Issue 341 - Volume 31, Issue 376), Field Naturalists Club of Victoria, page 62:
Tectotype (Chapman, 1912).—A tectotype is a specimen, fragmentary or otherwise, which is selected to elucidate the microscopic structure, internal or external, of a species or genus.
1944, Proceedings of the Royal Society of Victoria, page 231:
Chapman further states, “ A tectotype may be associated, in the case of a species, with the original types (tectoparatype), or with subsequently described specimens (tectoplesiotype).”
2010 May, David Leslie Hawksworth (compiler), Terms Used in Bionomenclature: The naming of organisms (and plant communities), Copenhagen: Global Biodiversity Information Facility, →ISBN, page 198 s.v. “tectotype”:
tectotype: (zool.) any type comprising a microscopic slide preparation or section.

1964, Report of the Twenty-second Session, India, 1964, page 41:
Early Baikalides with a granitization and metamorphism age of 1,100-1,000 m.y. include the Grenville folded zone in the east of North America (the innermost part of the Appalachian belt) and the Satpura zone in Hindustan. The concluding folding of the early Baikalides could be called Grenville folding by its Canadian tectotype.
1979, Bulletin de L'Académie Polonaise Des Sciences: Série des sciences de la terre (Volume 27), Państwowe Wydawn. Naukowe, page 35:
The Teisseyre-Tornquist zone cannot be proved to exist within the homogeneous isochronous platform plate; hence one of the basic features of Schatski's tectotype is not fulfilled.
1981, International Symposium Central European Permian: Jabłonna, April 27-29, 1978: Proceedings, Wyd. Geologiczne, page 151:
But, reviewing the tectonic and geological significance of the Teisseyre-Tornquist line in the formation of the Middle Polish swell and the adhering troughs, I feel it necessary to emphasize at this point that there is no justification to ascribe /as many Polish and foreign authors do/ to this line features of an intracontinental rift or to regard it as an aulacogen /a rift frozen in its evolution/ as this does not stand comparison with the tectotypes of these tectonic units such as the Dneper-Donets aulacogen and the Rhine graben.