Community Care Access Centre accountability reforms: executive director perceptions /

The purpose of this study was to explore how four purposefully selected executive directors of Community Care Access Centres (CCACs) understood the idea of accountability, and how they viewed the accountability reforms that had been imposed on their sector of health care over the previous three years. Data were collected through personal interviews and a reflective journal. An analysis of key documents and the reflective journal informed the data analysis. The findings suggest that executive directors perceive that accountability relationships have shifted since reforms have been implemented. They noted that CCACs have become more accountable to the provincial government at the expense of accountability to the local community. From their perspective, the demand for greater standardization and bureaucratization has left fewer opportunities to adapt programs to meet particular community needs and has slowed the ability to respond quickly to community inquiries and concerns.

Geology of the Rankin Inlet area, Northwest Territories /

The Rankin Inlet area, on the west shore of Hudson Bay in the Northwest Territories, is in the Churchill Structural Province. Metamorphosed volcanic and sedimentary rocks, previously mapped as Archean and part of the Kaminak Group, underlie most of the area. The Rankin Inlet Group consists of greywacke, with minor conglomeratic greywacke, quartzite and dolomite, overlain by massive and pillowed basaltic flows. Gabbro sills intrude the sediments near the base of the volcanic sequence and three serpentinite sills outcrop at the base of the volcanic sequence. The sediments are in fault-contact with quartz monzonite to the south and were intruded by granitic rocks to the northwest. Two periods of folding were defined by the mapping. The first generation folds are recumbent isoclinal folds, with northwest-trending and northeast-dipping axial planes, formed through gravitational sliding. The second generation folds are symmetrically disposed about the axis of the granitic intrusion and have east-southeast trending and nearly vertical axial planes. Whole-rock analysis of 64 rock samples indicates that metasomatic alteration accompanied the intrusion of both the granitic rocks and the serpentinite. The volcanic rocks, gabbro and serpentinite were derived from a magma of oceanic tholeiitic affinities. The stratigraphic sequence and chemistry of the volcanic rocks of the Rankin Inlet Group indicate that this assemblage is correlative with the Hurwitz Group rather than the Kaminak Group and is therefore Aphebian in age.