As a family dentistry provider in Midland, ON, we realize that all of our patients will have different dental needs.
At Georgian Shores Dental Centre, we are a family dentistry office that serves Midland, Ontario and surrounding areas. We are able to meet the dental needs of patients of all ages and are confident that you will be happy with your decision to make us your family’s dental office.
As a family dentistry provider, we realize that all of our patients will have different dental needs. For this reason, we provide a number of preventative and cosmetic dental procedures, including general dental checkups, root canals, teeth whitening, dental implants, and more. Our goal is to make sure we’re the only place you need to visit to maintain the health and beauty of your smile.
We understand that coming in to see a dentist, even if it’s just for a general checkup, can be an intimidating experience. Due to this, we will do everything we can to make sure the time you spend at our office is comfortable and rewarding. Not only will our dentists, hygienists, assistants, and administrative staff provide you with friendly service, but we also have many different amenities in our office, like televisions in every treatment room, which are designed to make your visit to our office more enjoyable.
As a patient-oriented family dentistry office that’s dedicated to educating our patients about their options and dental health, we are confident that you will benefit from allowing us to become your family’s dental provider. For more information about our services or to schedule an appointment, please contact us at Georgian Shores Dental Centre today.
At Georgian Shores Dental Centre, we offer family dentistry services in Collingwood and Midland, Ontario.
Our dental services in Midland, ON are complemented by a warm and comfortable environment that is designed for your comfort.
Your dental provider should be able to meet you and your family’s dental needs. At Georgian Shores Dental Centre, we are confident that we can do this because we provide a number of different cosmetic and preventative dental services.
Some of the dental services we provide include bonded fillings, tooth extractions, general dental checkups, crowns and bridges, and root canals. We also offer dental implants, porcelain veneers, and teeth whitening.
When you come into our office, whether it is for a general checkup or to find out more about dental implants, we will provide you with compassionate, focused care. Our dental services are also complemented by a warm and comfortable environment. In all of our treatment rooms, we have televisions, and our waiting rooms are equipped with Xbox 360.
Our goal is to turn seeing the dentist into an enjoyable and educational experience for your entire family. We are confident that when you make us your dental provider of choice, you will never want to go anywhere else for dental care in the Midland, Ontario area.
If you have any questions about our dental services and what we can do for you and your family, please reach out to us at Georgian Shores Dental Centre today. We look forward to having you visit our office and to meeting your dental needs now and in the years to come.
At Georgian Shores Dental Centre, we offer dental services in Collingwood, Midland, Thornbury and Penetanguishene, Ontario.
Definition of magnetic domains within the Rae Craton, mainland Canadian Shield, Nunavut, Northwest Territories, Saskatchewan, and Alberta: their magnetic signatures and relationship to geology
The Archean Rae craton, western Churchill Province, occupies a huge area within the northwestern mainland Canadian Shield. It extends >1600 km from the Talston magmatic zone northeastward to the east coast of Melville Peninsula, ranging in width from roughly 300 km to 900 km. The craton is covered by aeromagnetic data collected over many decades by Canada's National Aeromagnetic Survey Program, typically along lines 805 m apart at a flight elevation of 305 m. Additionally, many higher resolution aeromagnetic surveys have been completed during the last decade or so. The craton is geologically mapped at various scales, but most geological coverage is at a relatively large scale. For this reason magnetic data provided by the national program are considered to be of sufficient resolution to investigate relationships with geology.
Here, seventy-five magnetic domains are defined using textures, fabrics, patterns, orientations and intensities of residual total magnetic field anomalies and their derivative equivalents (first vertical derivative, tilt angle). Given that patterns and orientations of narrow derivative magnetic anomalies reflect closely geological structure, the magnetic domains can be viewed essentially as representative of structural domains. The maximum dimension of most domains is >100 km, but many attain dimensions of several 100 km. Although the Rae craton has an overall northeastward trend, a strong pattern of linear magnetic domains running parallel to this trend along the length of the craton is not apparent. A few generally relatively broad and parallel domains do run northeastward along the spine of the craton between roughly the Talston magmatic zone and Aberdeen sub-basin. Several narrower and typically less extensive domains also trend northeast within the Chesterfield block along the southeast margin of the craton southeast of the sub-basin. Where the southern part of the craton, south of the roughly east- trending Amer and Wager Bay shear zones, swings into a more eastward trend, linearity is lost and domains become smaller and more irregular in shape, with some trending across the craton.
The best developed linear pattern of domains probably lies between the Thelon magmatic zone and Chantrey fault zone, where several narrow to moderately wide, sub-parallel domains extend between the McDonald fault (and its northeastward projection) and Queen Maud Gulf. Eastward they change orientation progressively from northward to roughly N30°E towards the fault zone. A sense of a linear arrangement of domains is observed also on the Boothia and Melville peninsulas, with trends varying between approximately east-northeast and northeast. A broad area east of the Chantrey fault zone, north of the Amer and Wager Bay shear zones, south of the Boothia Peninsula and including the southern part of the Melville Peninsula contains some linear domains trending approximately northeast, but there are also sizable domains of irregular shape lacking an internal magnetic fabric characterized by prominent northeast trends.
Many close correlations between magnetic anomalies and mapped lithological units exist, but there are numerous examples where anomalies transect unit boundaries thus questioning boundary positions. Magnetic anomalies indicate probable lithological/compositional changes within many large gneissic units pointing to a need for more detailed mapping. Many examples of exceptionally strong magnetic highs are associated with mapped iron formations. Such highs in areas apparently lacking iron formations signify their potential presence. Magnetic patterns and signatures outline locations of small circular to roughly oval, unmapped igneous intrusions, and many faults not displayed on geological maps.
Magnetic maps of the Precambrian Rae craton in the northwestern portion of the mainland Canadian Shield are used to define magnetic domains. The principal magnetic maps were of the residual total magnetic field and the first vertical derivative and tilt angle of the field. The latter two maps provide images that reflect very closely geological structure, hence magnetic domains essentially portray structural domains. At the craton scale, the definition of the domains provides a different perspective for evaluating structural relationships and tectonic development. At more local scales relationships between magnetic signatures and mapped geology sometimes support mapping, and in other cases call into question the attribution of a certain rock-type or positioning of a contact. The magnetic maps also indicate areas designated as single unit that are obviously much more complex, and this is to be expected given that geological mapping in many areas is largely reconnaissance in nature.