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Friday, July 24, 2020 | History

2 edition of Preliminary report and interpretation of alteration in the Eye-Dashawa Lakes Pluton found in the catalog.

Preliminary report and interpretation of alteration in the Eye-Dashawa Lakes Pluton

Atomic Energy of Canada Limited.

Preliminary report and interpretation of alteration in the Eye-Dashawa Lakes Pluton

by Atomic Energy of Canada Limited.

  • 59 Want to read
  • 27 Currently reading

Published by s.n in S.l .
Written in English


Edition Notes

1

SeriesTechnical record (Atomic Energy of Canada Ltd) -- 178
ContributionsKamineri, D., Dugal, J.
ID Numbers
Open LibraryOL21968676M

B L A I N E D E W E Y BLA INE MAJ OR D EWEY MA JOR N 2 4 0 0 R d E 06 Rd N 2 4 6 6 R d N 2 3 7 0 R d E Rd S t a t e H w y 5 8 A E Rd E Rd N 2 4 6 0 R d L o u i e ' s L n E Rd E Rd N 2 4 9 0 R d N 2 4. A detailed study of apatite and biotite compositions in multiple intrusive phases from five composite plutons in the northern Canadian Cordillera was undertaken with the aim of determining the composition of magmatic fluids relative to F:Cl:OH for several plutons―both barren and mineralizing―and for specific intrusive phases from each pluton that may be related to nearby tungsten skarns.

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Preliminary report and interpretation of alteration in the Eye-Dashawa Lakes Pluton by Atomic Energy of Canada Limited. Download PDF EPUB FB2

The foUowing features suggebd, that fractures have controlled the alteration in the Eye-Dashwa lakes pluton: (1) Fillings such as ep,dote and chlorite,n these roc, ks have an indLgenous source and can be traced into the rock matrix, where partial or total replace- ment of primary plagioclase feldspars and ferromagnesmn minerals has oc- by: 2.

Geology of the Eye--Dashwa lakes pluton The Eye--Dashwa lakes pluton occurs with- in the Superior Structural Province of the Canadian Shield, and is located ~30 km NW of Atikokan, NW Ontario (Fig. Peterman et al. () reported an age of + 23 Myr. for this pluton, based on U--Pb concor- dia of by: The variation of magnetic susceptibility in the Eye-Dashwa lakes granitic pluton near Atikokan, Ontario, Canada, is almost entirely associated with the oxidation of the Fe-Ti oxide minerals.

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Preliminary report on the geology and controlling parameters of the Goldcorp Inc. High Grade zone, Red Lake mine, Ontario 1 Benoît Dubé, Kenneth Williamson, and Michel Malo 2. In this paper, we summarize the timing and kinematics of extension and exhumation of midcrustal rocks in Eocene metamorphic core complexes located north and south of the Lewis and Clark fault major metamorphic core complexes and detachment fault systems adjacent to the Lewis and Clark fault zone include, on the northern side, the Priest River complex; on the southern side, the.

Geophysical Study of Meteorite Impact Structures Our preliminary interpretation is that the Alamosa River pluton was emplaced by multiple, successive magmatic pulses. Here we report on our. PDF | This article provides a preliminary interpretation of the Coompana aeromagnetic survey.

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The Chibougamau pluton is a Neoarchean multiphase intrusion that is related to Cu–Au porphyry-style deposits. In Archean greenstone belts, porphyries are marginal and poorly documented mineralizations. Such deposits are, however, important in the Chibougamau area, where the main historical mining camp (Central Camp) is a magmato-hydrothermal system.

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Glacial Lakes of Puget Sound: Preliminary Paper is an article from The Journal of Geology, Volume View more articles from The Journal of The National Lakes Assessment (NLA) is a statistical survey of the condition of our nation's lakes, ponds, and reservoirs.

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Comprehensive Eye Exams – For adults and [email protected]{osti_, title = {Transport phenomena in hydrothermal systems: cooling plutons}, author = {Norton, D and Knight, J}, abstractNote = {The nature of heat and mass transport in plutonic environments has been described by partial differential equations and simulated by numerical approximation.

A series of heuristic models based on these equations describes the general features .Magmatic and hydrothermal systems are intimately linked, significantly overlapping through time but persisting in different parts of a system.

New preliminary U-Pb and trace element petrochronology from zircon and titanite demonstrate the protracted and episodic record of magmatic and hydrothermal processes in the Alta stock–Little Cottonwood stock plutonic and volcanic system.