2 edition of Manicouagan, Quebec, Paleomagnetic Results. found in the catalog.
Manicouagan, Quebec, Paleomagnetic Results.
Canada. Dept. of Energy, Mines and Resources. Observatories Branch.
|Other titles||Paleomagnetic Results From Manicouagan, Quebec.|
|Series||Contributions from the Dominion Observatory -- V|
The paleomagnetic angle of _____, also known as magnetic dip, is measured between the Earth's surface and a line of magnetic force directed toward a magnetic pole. Inclination A line from a given location to the magnetic pole will be offset from a line to the respective geographic pole by . Undeformed and unmetamorphosed diabase dykes up to 5 m wide occur in an area of ∼ km 2 about 50 km northwest of Montreal near the village of Sainte-Sophie. The dykes are subvertical and oriented east–west. The most common phenocryst phase is plagioclase (1–2 mm, exceptionally 10 mm), followed by olivine, and in one dyke, : Michael D. Higgins, Fatim Hankard, Morgan Ganerød, Rob Van der Voo.
Quebec's Manicouagan Crater is one of the largest fairly well-preserved impact craters on Earth. A ring-shaped hydroelectric reservoir lake 70 km in diameter occupies the centre of the crater. Discover Lake Manicouagan in Rivière-aux-Outardes, Québec: A lake formed in the basin of a massive impact crater takes the shape of an unbroken ring when viewed from g: Paleomagnetic.
The reported paleomagnetic study was carried out on 53 oriented samples ( specimens) at 10 sites in the eastern Gaspé Peninsula. All sampled geological units are composed of sub vertical diabase dykes that cut the sedimentary formations of late Early Devonian – early Middle Devonian by: 5. COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle coronavirus.
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Home > Journals > Canadian Journal of Earth Sciences > List of Issues > Volume 4, Number 4, August > MANICOUAGAN, QUEBEC, PALEOMAGNETIC RESULTS Article «Previous TOC Next»Cited by: Download Citation | Manicouagan, Quebec, paleomagnetic results | The remanent magnetization of dacitic material from Manicouagan, Quebec, Manicouagan examined.
Author: W. Robertson. Petrology, structure and origin of the Manicouagan Melt Sheet, Quebec, Canada: A preliminary report. Geophysical Research Letters, 3(2), 49– Gault D.E., Greeley R., Exploratory experiments of impact craters formed in viscous-fluid targets - analogues for Martian rampart craters, We report rock magnetic and paleomagnetic data from the ~ Ma Manicouagan (Canada) impact crater based on 25 widely distributed sites of impact melt and basement rocks collected at the surface as well as from boreholes drilled to depths ≤ km.
Titanomagnetite and titanohematite carry the magnetic remanence in impact melts above m elevation and in most basement by: 8.
The remanent magnetization of dacitic material from Manicouagan, Quebec, was examined. Laboratory thermal Manicouagan support the view that viscous buildup in situ was small and secondary components Author: Elena Vesselinov. This magnetostratigraphic age is consistent with the radiometric age of the Manicouagan impact that formed the second largest known crater in the Phanerozoic at Quebec, Canada.
The results of this study, as well as previous studies, suggest that the chert section, which includes the ejecta layer, was deposited within a paleolatitude range of Paleomagnetic Results.
book Cited by: 6. In addition, the normal polarity interpretation for the ejecta layer is consistent with the paleomagnetic data of Manicouagan melt rock (Robertson, ). These results are interpreted to show that the ejecta layer in the Sakahogi section was the product of a large meteoritic impact event that formed the km-wide Manicouagan by: 6.
The remanent magnetization of dacitic material from Manicouagan, Quebec, was examined. Laboratory thermal studies support the view that viscous buildup in situ was small and secondary components Author: Abraham Hollander. a stratigraphic analysis of the subsurface data relating to the chazy group in the st.
lawrence lowland of eastern canada. Paleomagnetic results from samples of the Chugwater Group near Lander, Wyoming, show a regular progression in pole positions from bottom to top of the se- quence. This pole position trend of about 25matches very well the North American appar- ent Cited by: RESULTS AND DISCUSSION (a) Maniccmagan Results for the Manicouagan samples are given in Fig.
1 and Table 1. Two items are note- worthy. The first is that one of the two samples (M-2) gives an age that agrees with the K-Ar determination on a fine-grained andite, Cited by: 2. Paleomagnetic Results  We sampled 52 cores at 12 sites using a gas‐powered drill.
The cores were oriented with magnetic and sun compasses, the latter to correct for local declination anomalies. Four sites were drilled in impact melt breccias, while eight sites come from basement rocks of variable lithologies lying within a radius of 16 km from the crater's estimated center at °N Cited by: Three‐dimensional modeling of the prominent ( nT) magnetic anomaly at the center of the Manicouagan structure in Quebec indicates the presence of Cited by: The remanent magnetization of dacitic material from Manicouagan, Quebec, was examined.
Laboratory thermal studies support the view that viscous buildup in situ was small and secondary components. Manicouagan Impact Crater, Quebec, Canada. Manicouagan is one of the largest known terrestrial impact craters.
It is 65 kilometers (40 miles) in diameter, but it is worth remembering that this is small compared with some of the larger lunar structures that measure more than km ( miles) across.
The remanent magnetization of dacitic material from Manicouagan, Quebec, was examined. Laboratory thermal studies support the view that viscous buildup in situ was small and secondary components Author: Michael Lewis-Beck.
ELSEVIER Earth and Planetary Science Letters () EPSL Palaeomagnetism of the ejecta-bearing Bunyeroo Formation, late Neoproterozoic, Adelaide fold belt, and the age of the Acraman impact Phillip W.
Schmidt a,1, George E. WilliamS b, a CSIRO Division of Exploration and Mining, PO BoxNorth R. de, NSWAustralia b Department of Geology and Geophysics, Unh ersiry of Cited by: EARTH AND PLANETARY SCIENCE LETTERS 6 () NORTH-HOLLAND PUBLISHING COMP., AMSTERDAM A PALEOMAGNETIC STUDY OF VOLCANIC ROCKS FROM MISTASTIN LAKE, LABRADOR, CANADA and ELLE Geological Survey of Canada, Booth Street, Ottawa, Canada Revised manuscript received 23 May Paleomagnetic data are Cited by: Outfitters in Manicouagan.
Are you a fan of hunting, fishing or other outdoor activities. Book your summer vacation at one of the outfitters in Manicouagan and take advantage of the wide selection of inns or cottages to stay g: Paleomagnetic.
Extinctions within major pelagic groups (e.g., radiolarians and conodonts) occurred in a stepwise fashion during the last 15 Myr of the Triassic.
Although a marked decline in the diversity of Cited by:. The results of the synthetic test indicate that for the northern and southern edges of this source, the method can distinguish the present-day and paleomagnetic fields with the same spatial resolution as the analytic signal has for identifying magnetization by: 3.; I asked Hydro-Quebec to put the actual and past levels on the web but got only a phone number in answer).
Twenty-ﬁve years Manicouagan Reservoir water level. Ticks at January 1 of each year. Vegetation: thanks to the high water level, the shores appeared quite natural with grasses and low shrub down to the Size: KB.Get directions, reviews and information for Quebec MRC Manicouagan in Baie-Comeau, g: Paleomagnetic.