A petrographic study is made of the granitic and related metamorphic rocks at Harrison Hot Springs, B.C. this thesis contains a general treatment of the regional and structural geology of the general area. The petrography of the various rock types is discussed under two main headings the granitic rocks, and the metamorphic rocks. Heat given of by the intrusive magma converted the adjacent unmetamorphosed sediments to hornfelses of the cordierite-anthophyllite subfacies and pyroxene-hornfels facies. These rocks are arbitrarily subdivided into rock types on the basis of their mineraloglcal compositions, rather than on the field occurrence. These assemblages are discussed with reference to the facies classification and the mineraloglcal phase rule. It is concluded that the hornfelses were derived by thermal metamorphism of aluminous-chloritic argillaceous sediments; that the cordierite-anthophyllite hornfelses were originally rich in MgO and FeO metasomatism was not an important process In the formation of the metamorphic assemblages. / Arts, Faculty of / Geography, Department of / Graduate

京都大学 / 0048 / 新制・課程博士 / 博士(理学) / 甲第22264号 / 理博第4578号 / 新制||理||1657(附属図書館) / 京都大学大学院理学研究科地球惑星科学専攻 / (主査)准教授 松四 雄騎, 教授 千木良 雅弘, 教授 岩田 知孝 / 学位規則第4条第1項該当 / Doctor of Science / Kyoto University / DGAM

Le site de la carrière du mont Royal (BjFj-97), découvert en 1993 par Yvon Codère et inventorié en 1997 par l’équipe d’Ethnoscop Inc., constitue une énigme archéologique intéressante pour quiconque s’intéresse à la préhistoire de l’île de Montréal et de sa région adjacente. Lors des activités archéologiques de 1997, quelques idées furent émises quant à son affiliation chronologique et sa nature, suggérant une occupation remontant à l’Archaïque terminal (4000 à 3000 AA) orientée vers l’extraction et la transformation de la cornéenne, une pierre métamorphique résultant de la transformation du substrat rocheux en place suite à des intrusions magmatiques lors du Crétacé qui ont créé les Montérégiennes. Le matériel, comprenant plus de 10 000 déchets de taille et un peu plus de 70 artéfacts divers, ne fît pas l’objet d’analyses poussées hormis la datation approximative du site par un examen sommaire des pointes de projectile. Ce mémoire reprend les données de 1997 et apporte une perspective nouvelle au site en décrivant morphologiquement et technologiquement le débitage de la pierre de façon à comprendre la chaîne opératoire de la cornéenne, une matière peu étudiée, mais fort commune au Québec méridional, appréhender les possibilités de la matière et aborder les questions de datation. L’ensemble du matériel lithique fît l’objet d’une analyse lithique poussée axée sur le débitage et les produits finis et propose la prépondérance de la taille bifaciale, ponctuée par un débitage sur éclat conséquent. L’ensemble des étapes de la chaîne opératoire est présent sur le site de la carrière du mont Royal. La cornéenne est une matière difficile à tailler en raison de son imprévisibilité, liée à la structure même de la matière, menant à un fort taux d’échecs lors de l’élaboration des outils. La datation de l’occupation principale du site pointe vers l’Archaïque terminal, mais le caractère équivoque des diverses classes d’objets rend difficile sa définition absolue, faute d’objets parfaitement diagnostiques. Le site BjFj-97 ressemble grandement à un site homologue en Nouvelle-Angleterre où la cornéenne fût travaillée suivant le même schéma opératoire, suggérant un apparentement culturel possible. La cornéenne abonde et domine dans les assemblages archéologiques de la région montréalaise, substituant ainsi des matières de meilleure qualité absentes régionalement. Leurs correspondances chronologiques transcendent celles établies lors de l’analyse du matériel de la carrière et montrent un étalement chronologiquement plus étendu, de l’Archaïque laurentien au Sylvicole supérieur. La cornéenne se retrouve habituellement sous forme d’outils bifaciaux fonctionnels (bifaces, couteaux et pointes de projectile) de piètre facture et d’outils sur éclats (grattoirs et racloirs) rudimentaires, suggérant une signification strictement utilitaire, le propre des matières de basse qualité. Les modes d’extraction de la cornéenne restent inconnus sur le mont Royal. Le mont Royal est plus qu’un vulgaire point défensif, il constitue la base de la subsistance des populations préhistoriques de jadis où se trouvent les matériaux nécessaires à la taille d’outils de prédation liés à un mode de vie mobile où domine la chasse. / The Mount Royal quarry site (BjFj-97), discovered in 1993 by Yvon Codère and test pitted in 1997 by Ethnoscop Inc., is an interesting archaeological puzzle for anyone interested in the Montreal region prehistory. Following the 1997 archaeological testing, some ideas were raised about the quarry’s cultural affiliation and its chronological position. Archaeologists proposed a primary occupation focused on hornfels extraction and transformation dating back to the Terminal Archaic period (4000-3000 BP). Hornfels is a metamorphic rock that resulted from bedrock being “cooked” during cretaceous magmatic intrusion that created the Monteregian hills. The material recovered, includes more than 10,000 flakes and over 70 artefacts, and is analysed here for the first time. This thesis provides a new perspective on the Mount Royal quarry site describing morphologically and technologically the stone tool production in order to better understand the hornfels’ chaîne opératoire. This lithic material is common on archaeological sites in southern Quebec can help us to address some issues of dating the quarry site. The entire lithic collection was subjected to an extensive analysis including all of the debitage and finished products, and shows the dominance of bifacial flintknapping, with some flake tools also being produced. All stages f the lithic reduction sequence are present on the Mount Royal quarry site. Hornfels is a difficult material to work because of its unpredictability, due to structure of matter, leading to a high rate of failures in the manufacture of tools. The main occupation of the site is dated to the Terminal Archaic, but the equivocal nature of the various objects makes it difficult to clearly define the period of occupation and exploitation. Site BjFj-97 is similar to another site in New England where hornfels was worked using a similar lithic reduction sequence, suggesting a possible cultural kinship. Hornfels is common on sites in the Montreal area, often substituting for better materials. The presence of hornfels on these sites suggests a wider chronological spread than that established from the material analysis from the quarry and covers the Laurentian Archaic to Woodland periods. Hornfels is usually found in formal bifacial tool forms (bifaces, knives and projectile points) and less formal flakes tools (scrapers) suggesting a strictly utilitarian significance, characteristic of low quality materials. Little is known about hornfels extraction methods on the mountain. Mount Royal is more than a defensive point: it forms the basis of the livelihood of the prehistoric people where predation tools were associated with a mobile lifestyle dominated by hunting.

No description available.

Mid-ocean ridge hydrothermal systems are known to extend to deep levels of the oceanic crust, including the plutonic section, but little is known about the timing and nature of fluid-rock interactions at these levels. To investigate the temporal and spatial characteristics of hydrothermal alteration in the lower crust, this study investigates a suite of hydrothermally altered (<5 to >20% hydrous alteration) gabbroic rocks recovered from the Hess Deep Rift, where 1.2 Ma fast-spreading East Pacific Rise crust is well-exposed. These samples were altered to amphibole-dominated assemblages with chlorite-rich samples occurring in a restricted region of the field area. Hornfels, indicative of reheated, previously altered rocks, are clustered in the central part of the field area. The entire sample suite has elevated 87Sr/86Sr (mean: 0.70257±0.00007 (2σ), n=16) with respect to fresh rock (0.7024). Bulk rock 87Sr/86Sr is strongly correlated with percentage of hydrous alteration and weakly correlated with bulk rock Sr content. The distribution of Sr in igneous and metamorphic minerals suggests that greenshist-facies alteration assemblages (chlorite, actinolitic amphibole, albitic plagioclase) lose Sr to the fluid while amphibolite-facies secondary assemblages (secondary hornblende, anorthitic plagioclase) take up Sr. The temperature-dependent mobilization of Sr in hydrothermal systems has implications for the 87Sr/86Sr and ultimately fluid/rock ratio calculations based on the assessed 87Sr/86Sr systematics. Considering Sr behaviour, minimum fluid/rock ratios of ~1 were calculated for the plutonic section. Due to the large uncertainty regarding fluid Sr composition at depth and the sensitivity of fluid/rock ratio calculations on this parameter, a model combining the sheeted dike complex and the plutonic section to one hydrothermal system is introduced, yielding a fluid/rock ratio of 0.5. This value may be more realistic since the fluid composition entering and exiting the sheeted dike complex is better constrained. The regional distribution of hornfelsed material with elevated 87Sr/86Sr suggests that fluid ingress into the upper plutonics at Hess Deep occurred on-axis in a dynamic interface of a vertically migrating axial magma chamber (AMC) and the base of the hydrothermal system. / Graduate