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Academic literature on the topic 'Uchi Lake'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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Journal articles on the topic "Uchi Lake"

1

Corfu, F., and G. M. Stott. "U–Pb geochronology of the central Uchi Subprovince, Superior Province." Canadian Journal of Earth Sciences 30, no. 6 (June 1, 1993): 1179–96. http://dx.doi.org/10.1139/e93-100.

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U–Pb zircon and titanite ages for rocks of the central Uchi Subprovince in northwestern Ontario indicate a late Archean magmatic and tectonic development spanning over 200 Ma. An early period at 2900–2800 Ma formed volcano-plutonic complexes, presumably linked to 3.1–2.8 Ga terrains of the northwestern Superior Province. A later period of southward growth by magmatic and tectonic accretion occurred at 2750–2710 Ma and was concluded by large scale compression and plutonism at 2700 Ma.The oldest 2890–2860 and 2840–2820 Ma components occur in the Pickle Lake and Meen–Dempster greenstone belts and as gneisses in the Seach–Achapi and the Lake St. Joseph batholiths in northern and central sectors of the region. Together with distinct 2750–2740 Ma volcano-plutonic complexes they form a collage assembled by multiple episodes of tectonic juxtaposition and magmatic accretion. Plutons of 2730–2710 Ma age are intrusive into these older, northern domains, whereas their volcanic counterparts compose the Lake St. Joseph and Miminiska – Fort Hope greenstone belts to the south. Late-tectonic to posttectonic granitoid rocks intruded a region extending from the northern Berens River Subprovince to the southern English River Subprovince at 2700 Ma. These plutons were cut by regional scale faults formed by residual north-northwest directed shortening. The timing of this movement seems to be recorded by titanite ages of 2690–2670 Ma. Reactivation of the same faults may account for Proterozoic Pb loss observed in some of the zircon populations. The age patterns are consistent with crustal growth along a continental margin in a north-dipping subduction environment.

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2

Lesher, C. M., A. M. Goodwin, I. H. Campbell, and M. P. Gorton. "Trace-element geochemistry of ore-associated and barren, felsic metavolcanic rocks in the Superior Province, Canada." Canadian Journal of Earth Sciences 23, no. 2 (February 1, 1986): 222–37. http://dx.doi.org/10.1139/e86-025.

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Archaean felsic metavolcanic rocks in the Superior Province of the Canadian Shield may be divided into three major groups on the basis of trace-element abundances and ratios. (1) FI felsic metavolcanic rocks are dacites and rhyodacites characterized by steep REE patterns with weakly negative to moderately positive Eu anomalies, high Zr/Y, low abundances of high-field-strength elements (e.g., HREE, Y, Zr, Hf), and high abundances of Sr. Examples occur in the Bowman Subgroup and Skead Group in the Abitibi Belt, in the Kakagi Lake, Lake of the Woods, Shoal Lake, and Sturgeon Lake areas of the Wabigoon Belt, and in the Confederation Lake area of the Uchi Belt. None of these horizons, as known, hosts base-metal sulphide deposits. (2) FII felsic metavolcanic rocks are rhyodacites and rhyolites characterized by gently sloping REE patterns with variable Eu anomalies, moderate Zr/Y, and intermediate abundances of HFS elements and Sr. Examples occur in the Misema Subgroup of the Abitibi Belt, in the Wabigoon Lake and Sturgeon Lake areas of the Wabigoon Belt, and in the Confederation Lake area of the Uchi Belt. Of these horizons, only those in the Sturgeon Lake area host base-metal sulphide deposits, and they exhibit the most pronounced negative Eu anomalies of this group. (3) FIII felsic metavolcanic rocks are rhyolites and high-silica rhyolites characterized by relatively flat REE patterns, which may be subdivided into two types. FIIIa felsic metavolcanic rocks exhibit variable negative Eu anomalies, low Zr/Y, and intermediate abundances of HFS elements and Sr. Examples occur in the Noranda mining district of the Abitibi Belt. FIIIb felsic metavolcanic rocks exhibit pronounced negative Eu anomalies, low Zr/Y, high abundances of HFS elements, and low abundances of Sr. Examples occur in the Kamiskotia, Kidd Creek, Matagami, and Noranda mining districts, the Garrison Subgroup in the Abitibi Belt, and at the South Bay mine in the Confederation Lake area of the Uchi Belt. All of these FIII horizons, with the exception of Garrison, host important base-metal sulphide deposits.These geochemical variations are interpreted to reflect differences in the petrogenesis of the felsic magmas, specifically, their formation or degree of modification in high-level magma chambers, which also influenced the formation of massive base-metal sulphide deposits. Most massive base-metal sulphide deposits in the Superior Province are underlain by subvolcanic magma chambers, which have been interpreted to have supplied heat to drive the ore-forming hydrothermal systems. FIII and some FII felsic volcanic rocks are interpreted to have been derived from these high-level magma chambers, accounting for their distinctive geochemical signatures and their association with massive base-metal sulphide mineralization. In contrast, FI felsic volcanic rocks are interpreted to have been derived from a deeper source and are considered to have escaped significant high-level modification, accounting for their distinctive geochemical signatures and the lack of associated base-metal sulphide mineralization. With certain limitations, the geochemistry of felsic metavolcanic rocks therefore may be used as a guide to identify prospective horizons for massive base-metal sulphide exploration in the Superior Province.

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3

Bethune, K. M., H. H. Helmstaedt, and V. J. McNicoll. "Structural analysis of the Miniss River and related faults, western Superior Province: post-collisional displacement initiated at terrane boundaries." Canadian Journal of Earth Sciences 43, no. 7 (July 1, 2006): 1031–54. http://dx.doi.org/10.1139/e06-017.

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Mountain building in the western part of the Archean Superior Province culminated with the formation of regional strike-slip faults. This paper reports on the kinematics and timing of several major faults at the juncture between the Uchi, English River, Winnipeg River, and western Wabigoon subprovinces. Sinistral-oblique mylonitization along the northeast-striking Miniss River fault occurred at 2681 [Formula: see text] Ma. This involved ~40 km of sinistral offset and a scissor-like motion whereby vertical displacement increased southwestward toward a restraining bend near Sioux Lookout. To the north, the Miniss River fault is intersected by the east-striking, dextral strike-slip Sydney Lake – Lake St. Joseph fault; the latter merges along strike with the Pashkokogan fault. Restoration of respective displacements indicates that the faults formed sequentially, not simultaneously in response to tectonic indentation. Dextral strike-slip motion along the Sydney Lake – Lake St. Joseph (– Pashkokogan) fault was instigated at ≤2670 Ma and drove greenschist-grade, dextral reactivation of the southwest segment of the Miniss River fault. U–Pb geochronology suggests that the latter coincides with an older terrane-boundary fault that juxtaposed ca. 2735 Ma juvenile, western Wabigoon arc complexes against ca. 3.05 Ga granitoid rocks of the Winnipeg River terrane. The Sydney Lake – Lake St. Joseph (– Pashkokogan) fault similarly demarcates a fundamental boundary between Uchian volcanoplutonic rocks and the English River accretionary prism. Strike-slip faults in this region therefore initiated at terrane boundaries and in some cases evolved so as to transect and displace these boundaries to accommodate further shortening during final stages of Archean orogenesis.

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4

Zeng, Fafu, and Andrew J. Calvert. "Imaging the upper part of the Red Lake greenstone belt, northwestern Ontario, with 3-D traveltime tomography." Canadian Journal of Earth Sciences 43, no. 7 (July 1, 2006): 849–63. http://dx.doi.org/10.1139/e06-027.

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Seismic reflection line 2B was shot across the Archean Red Lake greenstone belt and Sydney Lake fault zone that marks the northern boundary of the English River metasedimentary belt, as part of the Western Superior Lithoprobe transect. Three-dimensional tomographic inversion of first arrival traveltimes recorded in this survey delineate the subsurface to depths as great as 1.5 km around this crooked two-dimensional seismic line. Within the Red Lake greenstone belt, P-wave velocities of 6.2–7.0 km s–1 occur at 500 m depth in the Mesoarchean Balmer assemblage, clearly distinguishable from the lower velocities of 5.1–6.1 km s–1 of the Neoarchean Confederation assemblage. Although the overall range of velocities in the metasedimentary rocks of the English River subprovince is similar to that found in the Confederation assemblage, lower velocities of 5.1–5.4 km s–1 are found in the upper 300 m of the metasedimentary rocks. In particular, two 2–3 km wide, east-northeast-striking zones of low velocity are associated with the Sydney Lake fault zone and the Pakwash Lake fault zone. Correlation of the velocities with the coincident reflection section suggests that these two faults delineate a fault-bounded block in the hanging wall of a more northerly fault zone that crops out within the Uchi subprovince. Anomalous regions of low velocity, which occur at the boundary between the Confederation and Balmer assemblages, and within the Balmer assemblage, may also be related to shear zones that have minimal near-surface expression, felsic lithologies, or hydrothermal alteration of the basalts.

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Percival, J. A., V. McNicoll, and A. H. Bailes. "Strike-slip juxtaposition of ca. 2.72 Ga juvenile arc and >2.98 Ga continent margin sequences and its implications for Archean terrane accretion, western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (July 1, 2006): 895–927. http://dx.doi.org/10.1139/e06-039.

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The North Caribou terrane of the western Superior Province attained continental thickness (~35 km) by 2997 Ma. It records a subsequent 300 million years history of continental fragmentation, arc magmatism, and terrane accretion. At Lake Winnipeg the ~2978 Ma Lewis–Storey quartzite–komatiite–iron formation assemblage marks Mesoarchean breakup. Unlike the relatively continuous 2980–2735 Ma stratigraphic record of the Red Lake and Birch–Uchi greenstone belts to the east, little of this interval is recorded at Lake Winnipeg. Rather, two belts of younger, juvenile rocks are tectonically juxtaposed: the Black Island assemblage of isotopically depleted, 2723 Ma basalt, and calc-alkaline andesite; and Rice Lake greenstone belt of basalt, calc-alkaline andesite, and dacite (2731–2729 Ma). Collectively these terranes represent a short-lived island-arc–back-arc system that docked with the southwestern North Caribou margin along a northwest-trending, dextral, transpressive, D1 suture. This zone is marked by the highly deformed coarse clastic Guano Island sequence (<2728 Ma) that contains detritus of North Caribou affinity and is interpreted as a strike-slip basin deposit. Younger clastic sequences, including the Hole River (<2708 Ma), San Antonio (<2705 Ma), and English River (<2704 Ma) assemblages, occur in east–west belts that may have been deposited during the terminal collision (D2, D3) between the North Caribou terrane and continental crust of the Winnipeg River terrane to the south. Several terrane docking events within a framework of north-dipping subduction and continental arc magmatism appear necessary to explain structural and stratigraphic relationships in the 2735–2700 Ma interval.

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6

Young, M. D., V. McNicoll, H. Helmstaedt, T. Skulski, and J. A. Percival. "Pickle Lake revisited: New structural, geochronological and geochemical constraints on greenstone belt assembly, western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (July 1, 2006): 821–47. http://dx.doi.org/10.1139/e06-036.

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New field work, U–Pb ages, geochemical data, and Sm–Nd isotopic analyses have established the timing and determined the nature of volcanism, deformation, and tectonic assembly of the Pickle Lake greenstone belt in the Uchi subprovince of the western Superior Province of the Canadian Shield. The >2860 Ma Pickle Crow assemblage has been redefined to include the former Northern Pickle assemblage on the basis of stratigraphic continuity and similar volcanic geochemistry between the two units across a previously inferred fault contact. The Pickle Crow assemblage consists of tholeiitic basalt with thin, but laterally extensive, oxide-facies iron formation overlain by alkalic basalts and minor calc-alkaline andesites to dacites with primitive Nd isotopic compositions (εNd2.89 Ga = +2.1 to +2.4) suggestive of deposition in a sediment-starved oceanic basin. The ~2 km thick ~2836 Ma Kaminiskag assemblage (former Woman assemblage) consists of tholeiitic basalt interbedded with intermediate and rare felsic pyroclastic flows with primitive Nd isotopic compositions (εNd2.836 Ga = +2.4). Two samples of intermediate volcanic rocks interbedded with southeast-younging pillowed basalt, previously inferred to be part of the Pickle Crow assemblage, yielded U–Pb zircon ages of 2744 [Formula: see text] Ma and 2729 ± 3 Ma. These rocks are thus part of the younger Confederation assemblage, which consists of intercalated basalt and dacite (εNd2.74 Ga = +0.1 to +0.8) exhibiting diverse compositions probably reflecting eruption in a continental margin arc to back-arc setting. The contact between the Confederation and Kaminiskag assemblages is assumed to be a fault. The greenstone belt is intruded by late syn- to posttectonic plutons including the composite quartz dioritic to gabbroic July Falls stock with a new U–Pb zircon age of 2749 [Formula: see text] Ma, and the ~2741 to 2740 Ma trondhjemitic to granodioritic Ochig Lake pluton and Pickle Lake stock, as well as the ~2697 to 2716 Ma Hooker–Burkoski stock. The earliest recognized deformation (D1) is recorded by a local bedding-parallel foliation in the Pickle Crow assemblage. This foliation is truncated by the ~2735 Ma Albany quartz–feldspar porphyry dyke and is not recognized in the volcanic rocks of the Confederation assemblage. The early deformation event is attributed to overturning of the Pickle Crow assemblage prior to deposition of the ~2744 to 2729 Ma Confederation assemblage. Subsequent deformation and development of a regionally penetrative planar fabric (S2) postdates ~2729 Ma volcanism, pre-dates the intrusion of the ca. <2716 Ma Hooker–Burkoski stock and is host to gold mineralization.

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7

Vesnina, L. V., T. O. Ronzhina, N. V. Zelentsov, G. A. Romanenko, I. Yu Teryaeva, and D. G. Elizariev. "PRODUCTIVITY OF SOME LAKES OF THE KOSH-AGACH DISTRICT OF THE REPUBLIC OF ALTAI." Innovations and Food Safety, no. 2 (July 2, 2020): 94–101. http://dx.doi.org/10.31677/2311-0651-2019-24-2-94-101.

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The Republic of Altai has a large length of watercourses and significant areas of lakes of fishery importance. The collection of materials was carried out in the field season of 2018 on the lakes: Uch-Kol (Three Lakes), Kamyshevoye and Lake without a name, located within the borders of Kosh-Agach district of the Altai Republic. Research has covered the entire water area. In the course of the research it was noted that Lake Uch-Kol consists of three successive basins with a total area of 7.9 hectares. The upper lake basin has an area of 5.5 hectares. The average lake basin has an area of 1.8 hectares. The lower lake basin has an area of 0.6 ha. Higher aquatic vegetation in the pond is missing. Lake zooplankton is represented by one species of Cladocera and two species of Copepoda. Lake Zoobenthos Uch-Kol is represented by a representative of the r. Gammarus. The area of Kamyshevoye Lake is 7.4 ha. The pond has a slightly elongated shape from west to east. In the zooplankton of the reservoir of mass development, branchy and rotifers reach. Chironomid larvae and caddisfruits dominate in the structure of zoobenthos. The area of the lake without a name is 29.4 hectares. The reservoir has a form elongated from the northeast to the southwest. In terms of numbers and biomass, Copepoda copepads are the dominant group in zooplankton. The dominant position in the zoobenthos composition is occupied by caddis flies and gammarids. All studied water bodies have low biological productivity. Phytoplankton is represented mainly by diatoms and green algae. The ichthyological fauna of Lake Uch-Kol and Lake Kamyshevoye is represented by an oligoid type of ichthyocenosis. The ichthyological fauna in the Lake without a name is missing.

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8

Nishikawa, Chihiro. "Underwater Cultural Heritage in Asia Pacific and the UNESCO Convention on the Protection of the Underwater Cultural Heritage." International Journal of Asia Pacific Studies 17, no. 2 (July 30, 2021): 15–38. http://dx.doi.org/10.21315/ijaps2021.17.2.2.

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Underwater cultural heritage (UCH) is a precious part of humanity’s shared history and heritage as it provides vital evidence and information about the interaction of humans with oceans, lakes and rivers. The Convention on the Protection of the Underwater Cultural Heritage was adopted by the General Conference of UNESCO (United Nations Educational, Scientific and Cultural Organization) in 2001 to protect this heritage which has become significantly vulnerable to threats such as pillaging, commercial exploitation and the development of the seabed with the evolution of marine technology in the latter half of the 20th century. The Convention celebrates its 20th anniversary in 2021 and has been ratified by 68 countries. Its annex, which provides rules about the activities directed at UCH, has become a major reference and is recognised as the established scientific standard for underwater archaeology and research today. Despite the growing recognition and application by the international community, the Convention has been ratified only by four countries in the Asia-Pacific region. Many underwater sites and shipwrecks have been commercially salvaged, particularly in Southeast Asia, and numerous artefacts recovered from the sites were often put up for auction, leading to irrevocable damage and loss of this valuable cultural heritage to future generations. This article as one of the themed articles dedicated to the UCH in Asia Pacific argues the roles of the Convention and the challenges and opportunities for the protection of UCH particularly in Southeast Asia. UCH contributes to the achievement of the Sustainable Development Goals and can play an important role in sustainable community and economic development. Its values and importance deserve to be widely recognised and advocated. Efforts for safeguarding cultural heritage in Asia Pacific needs to be pursued and enhanced through joining the 2001 Convention and with international support and cooperation.

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Dissertations / Theses on the topic "Uchi Lake"

1

Tarnocai, Charles A. "Gold mineralization at the Campbell Mine, Red Lake greenstone belt, Uchi subprovince, Ontario." Thesis, University of Ottawa (Canada), 2001. http://hdl.handle.net/10393/6216.

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The Campbell mine is located in the eastern part of the Red Lake greenstone belt, Uchi Subprovince. Auriferous veins are parallel to S2, and are termed foliation parallel auriferous veins (NW striking, SW dipping). Auriferous veins also occur in shear zones which are oblique to the regional NW trending foliation (foliation-oblique deformation zones). These auriferous veins occur proximal to the F2 fold hinges. The deformation zones are typically meters to 10's of meters wide, and are characterized by more intense foliation development, and abundant carbonate veins and veinlets. Progressive D2 shortening resulted in a late D2 decollement along the southwestern limb of the Balmer synform, cutting and offsetting auriferous mineralization. Several stages of hydrothermal activity are recognized in the Campbell mine area. Subsequent Au mineralization occurs in quartz veins and quartz + arsenopyrite hydrothermal breccias within quartz + carbonate veins; thus most of the Au mineralization overprints pre-existing quartz + carbonates within the D2 shear zones. Native gold from amphibolite facies domains contains significant Ag, precluding that it formed by the thermal decomposition of aurostibite. Therefore, the spatial variations in occurrence of Au phases reflect the deposition of Au during the peak metamorphism. Higher metamorphic grade rocks are extended westward along the auriferous shear zones, suggesting heat transfer along shear zones by hydrothermal fluids. This suggests a magmatic heat source to the east for auriferous hydrothermal activity. Hence, Au mineralization likely took place during the emplacement of the marginal phase of the Trout Lake batholith. The lack of Type II inclusions in high Au grade breccias is interpreted as a result of the selective loss of H2O following phase separation. Phase separation is probably the most important mechanism for the mineralization of high Au grades (>500 g/t Au) at the mine. The gold-related wallrock alteration at the Campbell Mine is similar to that in other Archean Au deposits hosted by lower amphibolite facies mafic rocks, such as the Coolgardie goldfields (Knight et al., 2000) and the Norseman district deposits (Mueller, 1992). The P-T conditions for the auriferous hydrothermal activity at many Archean lode-type deposits define a low P and high T path. The path indicates much higher temperatures than the Archean geotherm, suggesting either a contribution of heat from contemporaneous magmas to auriferous fluids, or rapid transfer of heat from deep levels. For syn-metamorphic Au deposits, the data support a magmatic heat source. This is in accord with the low P/high T conditions of the metamorphism accompanying the Au deposits. For post-peak metamorphic deposits, the data suggest transport of heat from a source external to the greenstone sequence. (Abstract shortened by UMI.)

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2

Borowik, Alexandra. "Structural analysis in the footwall of the Uchi-English River subprovince boundary, Red Lake region, northwestern Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0024/MQ33941.pdf.

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3

Crews, Michael James. "Patterns of total strain in the walls of two greenstone assemblage boundaries, western Birch-Uchi (Confederation Lake) Belt, NW Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0003/MQ46013.pdf.

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Books on the topic "Uchi Lake"

1

Survey, Ontario Geological. Gravity Study of the Birch, Uchi, and Red Lakes Area: District of Kenora (Patricia Portion). S.l: s.n, 1986.

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2

K, Gupta V. Gravity study of the Birch, Uchi, and Red Lakes area: District of Kenora (Patricia Portion). Toronto, Ont: Ontario Ministry of Northern Development and Mines, 1986.

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3

Noble, Stephen Russell. Geology, geochemistry and isotope geology of the Trout Lake batholith and the Uchi-Confederation Lakes greenstone belt, Northwestern Ontario. 1989.

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4

Borowik, Alexandra. Structural analysis in the footwall of the Uchi-English River subprovince boundary, Red Lake region, northwestern Ontario. 1998.

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5

Crews, Michael James. Patterns of total strain in the walls of two greenstone assemblage boundaries, Western Birch-Uchi (Confederation Lake) Belt, NW Ontario. 1999.

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Book chapters on the topic "Uchi Lake"

1

Matsushita, Satoshi, and Hiroshi Kitazato. "Seasonality in the Benthic Foraminiferal Community and the Life History of Trochammina Hadai Uchio in Hamana Lake, Japan." In Paleoecology, Biostratigraphy, Paleoceanography and Taxonomy of Agglutinated Foraminifera, 695–715. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-3350-0_24.

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Reports on the topic "Uchi Lake"

1

Sanborn-Barrie, M., N. Rogers, and T. Skulski. Geology and tectonostratigraphic assemblages, east Uchi Subprovince, Red Lake and Birch-Uchi belts, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215111.

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Sanborn-Barrie, M., N. Rogers, T. Skulski, J. Parker, V. McNicoll, and J. Devaney. Geology and tectonostratigraphic assemblages, east Uchi Subprovince, Red Lake and Birch-Uchi belts, Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215355.

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Poulsen, K. H., D. E. Ames, S. Lau, and W. C. Brisbin. Preliminary Report On the Structural Setting of Gold in the Rice Lake area, Uchi Subprovince, southeastern Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120646.

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Brommecker, R., K. H. Poulsen, and C. J. Hodgson. Preliminary Report On the Structural Setting of Gold At the Gunnar Mine in the Beresford Lake area, Uchi Subprovince, southeastern Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126878.

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Tomlinson, K. Y., and N. Rogers. Neodymium-isotopic characteristics of the Uchi-Confederation Lakes region, northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210856.

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