Luis Fernando Ramírez, David Peña, Bernardo Ortíz, Freddy Buitrago. Invenciones modernas.

Programas, proyectos y red de portales

Dr. David Atkinson

Dr. Atkinson was the fourth President of Brock University. He was President from 1997 - 2005.

Dr. David McCarthy

Professor of Computer Science.

David Shemilt

Pictured here is Brock swimmer, and Olympian, David Shemilt on June 7, 1984.

David Shemilt

Brock's David Shemilt dives into the pool in June of 1984

Geology of the Gander Group, Gander River Ultramafic Belt and Davidsville Group in the Jonathan's Pond - Weir's Pond Area, northeast Newfoundland /

The study area is situated in NE Newfoundland between Gander Lake and the north coast and on the boundary between the Gander and Botwood tectonostratigraphic zones (Williams et al., 1974). The area is underlain by three NE trending units; the Gander Group, the Gander River Ultramafic Belt (the GRUB) and the Davidsville Group. The easternmost Gander Group consists of a thick, psammitic unit composed predominantly of psammitic schist and a thinner, mixed unit of semipelitic and pelitic schist with minor psammite. The mixed unit may stratigraphically overlie the psammitic unit or be a lateral facies equivalent of the latter. No fossils have been recovered from the Gander Group. The GRUB is a terrain of mafic and ultramafic plutonic rocks with minor pillow lava and plagiogranite. It is interpreted to be a dismembered ophiolite in thrust contact with the Gander Group. The westernmost Davidsville Group consists of a basal conglomerate, believed deposited unconformably upon the GRUB from which it was derived, and an upper unit of greywacke and slate, mostly of turbidite origin, with minor limestone and calcareous sandstone. The limestone, which lies near the base of the unit, contains Upper Llanvirn to Lower Llandeilo fossils. The Gander and Davidsville Groups display distinctly different sedimentological , structural and metamorphic histories. The Gander Group consists of quartz-rich, relatively mature sediment. It has suffered three pre-Llanvirn deformations, of which the main deformation, Dp produced a major, NE-N-facing recumbent anticline in the southern part of the study area. Middle greenschist conditions existed from D^ to D- with growth of metamorphic minerals during each dynamic and static phase. In contrast, the mineralogically immature Davidsville Group sediment contains abundant mafic and ultramafic detritus which is absent from the Gander Group. The Davidsville Group displays the effects of a single penetrative deformation with localized D_ and D_ features, all of which can be shown to postdate D_ in the Gander Group. Rotation of the flat Gander S- into a subvertical orientation near the contact with the GRUB and the Davidsville Group is believed to be a Davidsville D^ feature. Regional metamorphism in the Davidsville Group is lower greenschist with a single growth phase, MS . These sedimentological, structural and metamorphic differences between the Gander and Davidsville Groups persist even where the GRUB is absent and the two units are in contact, indicating that the tectonic histories of the Gander and Davidsville Groups are distinctly different. Structural features in the GRUB, locally the result of multiple deformations, may be the result of Gander and/or Davidsville deformations. Metamorphism is in the greenschist facies. Geochemical analyses of the pillow lava suggest that these rocks were formed in a back-arc basin. Mafic intrusives in the Gander Group appear to be the result of magraatism separate from that producing the pillow lava. The Gander Group is interpreted to be a continental rise prism deposited on the eastern margin of the Late Precambrian-Lower Paleozoic lapetus Ocean. The GRUB, oceanic crust possibly formed in a marginal basin to the west, is believed to have been thrust eastward over the Gander Group, deforming the latter, during the pre-Llanvirnian, possibly Precambrian, Ganderian Orogeny. The Middle Ordovician and younger Davidsville Group was derived from, and deposited unconformably on, this deformed terrain. Deformation of the Davidsville Group occurred during the Middle Devonian Acadian Orogeny.

The application of gas liquid chromatography to the simultaneous analysis of sugars and sugar phosphates in biological samples /|nby David J. LeBlanc. -- 260 St. Catharines [Ont. : s. n.],

A study was undertaken' to determine the applicability of gas liquid chromatography to the simultaneous analysis of sugars and sugar phosphates from biological samples. A new method of silylation involving dimethylsulfoxide, hexamethyldisilazane, trimethylchlorosilane and cyclohexane (1:0.2:0.1:1) which rapidly silylated sugars and sugar phosphates was developed. Subsequent chromatography on a 5% SE-52 column gave good resolution of the sugar and sugar phosphate samples. Sugar phosphates decomposed during chromatography and were lost at the 7 x 10-3 ~mole level. Acidic ethanol extraction of yeast samples revealed background contamination from the yeast sample, the culture medium and the silylation reagents which would further limit the level of detection obtainable with the glc for sugars in biological samples to the 3 x 10-4 ~mole level.

David Dorey Fonds, 1983-1985

David Dorey, a Brock University student in 1993, was past president of the Unemployed Action Alliance. In 1993 he donated the fonds to Brock University Archives. The Unemployed Action Alliance was organized in 1983 with support from the St. Catharines and District Labour Council. The aims of the group were to unify the interests of unemployed people for greater benefit in finding employment, retraining and lobbying the provincial government.

David William Smith House correspondence, 1798 [transcription]

The correspondence from D.W. [David William] Smith to President Peter Russell regarding Smith’s desire to sell a certain piece of property in Newark (now Niagara-on-the-Lake, Ont.) to be used as a location for a common grammar school. The notice gives a description of the building situated on the property as being adaptable for the use of a school. The Board of Survey convened in December 1798 to examine Smith’s property and gave an appropriate valuation of the properties and buildings Smith was offering for sale. Smith was the deputy surveyor general of lands for Upper Canada.

David Skene-Melvin papers, 1918, 1995, n.d.

David Skene-Melvin, literary historian and bibliographer, donated his extensive collection of books on Crime, Mystery and Detective fiction to the Popular Culture Program at Brock University in July 2001. The donation forms a significant part of the Skene-Melvin Collection of Crime, Mystery and Detective Fiction, James A. Gibson Library, Brock University.

Welland Canal Survey of Lands Jonathan Clendenning 1826

Survey map and description of Jonathan Clendenning's land created by The Welland Canal Company. Included is two written descriptions of the land along with two drawings of the land. Noteable features for the first (small) map include; line between the Clendennan and Sanderson properties, line between Clendennan and Steward properties, canal. Noteable features for map #2 (large map)include; numerous surrounding farms, roads. Surveyor notes are seen in pencil on both the maps. The deed for the land is dated August 23, 1826.Pages 49-51

Welland Canal Survey of Lands David Thompson Esquire

Survey map and description of David Thompson's land created by The Welland Canal Company. Included is a written description of the land along with a drawing of the land. Noteable features include; line between Widow McAlpine and Thompson's land. The land contains 9 acres, 3 roads, 11 perches and 2 acres partly drained.