... the older pyritic quartz-pebble conglomerates at the base of the Matinenda Formation in the Elliot Lake and Blind River areas, these conglomerates contain no uraninite and are polymict with material derived from a highly restricted catchment area with marked local and regional topographic relief. Porous...

... conglomerate ore of the Elliot Lake – Blind River area. The sandstones also contain paraconglomerate units at several stratigraphic levels which are lithologically similar to the Ramsay Lake and Bruce Formations.Trends in Huronian stratigraphy on the North Shore of Lake Huron suggest that in the Morin Township...

...Grant M. Young Abstract Mapping in the McGregor Bay area of Ontario has shown the presence of a sequence of formations which closely resembles that of the original Huronian of the Bruce Mines–Blind River area. Iron-rich siltstones and argillites above the Lorrain formation are correlated...

... the Huronian at Lauzon Bay in the Blind River area of Ontario and has a complex history of alteration events, addition of allochthonous material, and low-grade metamorphism. Much of this history can be deciphered, and changes in mineralogy and bulk and mineral chemistry can be assigned to separate alteration...

...Duncan R. Derry Abstract The 10 U mines now in production in the Blind River area of Ontario have provided considerable new evidence on the origin of the deposits and have been the subject of a number of studies by government, company, and research geologists. An attempt is here made to coordinate...

...E. W. Nuffield Abstract The Blind River area, situated on the north shore of Lake Huron about 80 miles east of Sault Ste. Marie, was last year the scene of a modern staking rush following the discovery of economically-significant amounts of uranium in Long township. The original find was at one...

... are from the Elliot Lake – Blind River and Agnew Lake areas, which experienced subgreenschist and biotite-grade greenschist metamorphism, respectively. Both areas, but particularly the lower grade area, contain some K-rich samples, with much of the K in detrital-appearing K-feldspar. In places K-feldspar...

... and relocated hypocenters, whereas the other combines geological and geophysical data from the study area. Upon analyzing these two fault models and the relocated hypocenter data, we propose that the seismogenic fault in the Yangbi earthquake is an undiscovered blind fault or a secondary blind fault...

...] and geomorphological studies [Clauzon et al., 1996 b ; Dubar and Guglielmi, 1997] show evidences for an uplift of the Ligurian coast increasing east of the Var river. The analysis of 70 seismic-reflection profiles allows us to better characterise and quantify the deformation from Antibes to Imperia (fig. 1). We...

... of west flowing rivers appear to be guided by longitudinal coastal faults. Severe sea erosion in Dakshina Kannada was initiated by the increase of pore water pressure in the coast-parallel river bends and blind tributaries, resulting from massive fluvial discharge during monsoon period. The storm waves...

...J. P. KENNETT; N. D. WATKINS Abstract The paleomagnetic stratigraphy, biostratigraphy, and paleoclimatology have been studied in two marine sections of late Miocene to early Pliocene age in New Zealand. A total of over 850 separately oriented cores were collected from 270 sites. The Blind River...

... of the Rock Springs uplift demonstrates that growth of the underlying blind thrust system produced an area of comparatively low accommodation space within the subsiding Green River Basin. The concurrent growth of the Rock Springs and Uinta uplifts does not support a rotation of shortening direction from east...

... River, remnants of this fold-thrust belt define a miniature valley and ridge province. Faults of the HVB die out to the west as blind thrusts in the basal units of the Catskill clastic wedge. Structural geometries displayed in the HVB vary rapidly along strike and are locally complicated by internal...

...D. S. Robertson; N. C. Steenland Abstract Ore conglomerates of the Blind River [Ontario, Canada], area lie at or near the base of the Huronian sedimentary section in discontinuous, sheetlike, partly overlapping, SE.-trending zones within a major NNE. belt. They are part of a sequence of detrital...

... basin, California. The modeled uplift matches well the geologic pattern of uplift associated with the Santa Fe Springs and Coyote Hills segments of the Puente Hills thrust fault but does not match structures to the west of the San Gabriel River. To better match the geologic patterns in this area...

... from the blind thrust related surface uplift, and the Pataliyon anticline in the northern part of the range ( Fig. 10 ). These rivers cross the Dhanaura anticline in south and are marked by prominent knick points and high SL index zones along the anticlinal axis ( Fig. 5 ). Drainage map of the area...

... area has established a strati- graphic succession similar to that of the Huronian of the Bruce Mines-Blind River area. Seven lithologic units are recognized, as follows is ascending order: Mississagi, Bruce, Espanola, Serpent, Gowganda, Lorrain formations and Banded Chert-like Siltstone. The Huronian...