Thesis (M. Sc.)--Carleton University, 1992. Accompanying material: 2 maps and 1 chart folded in pocket. / Also available in electronic format on the Internet.

Thesis (Ph. D.)--Carleton University, 1997. / Also available in electronic format on the Internet.

Thesis (M. Sc.)--Carleton University, 2001. / Accompanying material: 2 folded maps and 2 diskettes in pocket. Includes bibliographical references (p. 276-285). Also available in electronic format on the Internet.

Thesis (Ph. D.)--University of Minnestota, 1933. / Science bulletin no. 1 of the Science museum of the Saint Paul Institute, with thesis t.p. containing "Vita", mounted on p. [2] of cover. Running title: The Ozarkian faunas of southeastern Minnesota. Six of the plates, each accompanied by lead with descriptive letterpress, not included in paging and eleven have descriptive letterpress on verso facing each plate. "Selected bibliography of references used in this study": p. 79-80.

Thesis (Ph. D.)--University of Texas at Austin, 2001. / Vita. Available also in a digital version.

Thesis (Ph. D.)--University of Wisconsin, 1970. / Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 138-149).

Thesis (Ph. D.)--University of Wisconsin--Madison, 1955. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.

Thesis (Ph.D.)--University of Delaware, 2006. / Principal faculty advisor: John C. Kraft, Dept. of Geology. Includes bibliographical references.

Thesis (Ph. D.)--University of Texas at Austin, 2000. / Vita. Five folded charts in pocket. Includes bibliographical references (leaves 316-324). Available also in a digital version from Dissertation Abstracts.

Planorbis to Turneri Zone sedimentary rocks were studied at outcrops on Skye, Raasay, Applecross, Ardnamurchan, Morvern and Mull. A proposed lithostratigraphy includes two Groups, four Formations and seventeen Members. Increased faunal diversity in Mull and Skye reflects environmental stability during the Angulata and Semicostatum Zones; low diversity in the Bucklandi and Turneri Zones signifies lower stability. Species abundance in Mull and their decrease in Skye during Angulata-Bucklandi Zone times signifies a northward increase in environmental instability. Smectites are present in the Planorbis-Bucklandi Zone shales. The Semicostatum-Turneri Zones are composed of non expanding clays; the smectite formed by erosion of previously exposed alkaline igneous rocks under warm, alkaline, low rainfall conditions. Progressive transgression covered the source area and a change to more acidic conditions with higher rainfall also promoted the formation of "ironstones" and chlorites. The Angulata and Bucklandi Zones comprise bioclastic, oolitic, carbonate and siliciclastic sediments signifying shallow marginal marine semi-enclosed basins. Thin laterally impersistent beds of coarse,poorly sorted pebbles signify an unstable hinterland; during the Semicostatum and Turneri Zones fully marine conditions were established. Ferruginous beds are oolitic in Skye. They probably formed as "mud balls" and due to acid leaching of feldspars. Phosphatic nodules are calciumhydroxyapatite. The limestone/shale "rhythms" are explained by a combined primary and diagenetic origin. The limestones consist of low-Mg calcite Both ferroan and non ferroan calcite are present. Tectonic stresses and diagenesis deformed crystals and formed veins. Sr⁺² values show a decline as the carbonate fraction increases. Three different ranges are distinguished for three facies and ages. Sr concentration is bimodal and probably inherited from the original sediments. The northern and southern basins evolved separately, sedimentation was controlled by differential tilting, uplift and subsidence. Palaeoslopes were gentle, to the west-northwest and south-southwest. Local topography (e.g. Central Strath High) modified the slopes; no movement occurred along the main faults of the area. Sedimentation relates to the "taphrogenic rifting stage" proposed for the North Sea Mesozoic.