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2 edition of Clastic breccias at the Slates Islands complex impact structure, northern Lake Superior found in the catalog.

Clastic breccias at the Slates Islands complex impact structure, northern Lake Superior

Clastic breccias at the Slates Islands complex impact structure, northern Lake Superior

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Published by National Aeronautics and Space Administration, National Technical Information Service, distributor in [Washington, DC, Springfield, Va .
Written in English

    Subjects:
  • Islands.,
  • Archipelagoes.,
  • Craters.,
  • Impact.

  • Edition Notes

    StatementB.O. Dressler ... [et al.].
    Series[NASA contractor report] -- NASA-CR-204185., NASA contractor report -- NASA CR-204185.
    ContributionsDressler, Burkhard O., United States. National Aeronautics and Space Administration.
    The Physical Object
    FormatMicroform
    Pagination1 v.
    ID Numbers
    Open LibraryOL15538246M


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Clastic breccias at the Slates Islands complex impact structure, northern Lake Superior Download PDF EPUB FB2

TECTONOPHYSICS I ELSEVIER Tectonophysics () Breccia formation at a complex impact crater: Slate Islands, Lake Superior, Ontario, Canada B.O. Dressier *, Northern Lake Superior book. Sharpton Lunar and Planetary Institute, Bay Area Boulevard, Houston, TXUSA Received 21 May ; accepted 6 January Abstract The Slate Islands impact Cited by: Get this from a library.

Clastic breccias at the Slates Islands complex impact structure, northern Lake Superior. [Burkhard O Dressler; United States. National Aeronautics and Space Administration.;].

We describe in some detail the various clastic breccias encountered on the islands during our and field work and relate them to the various phases of the impact process. The Slate Islands impact structure is the eroded remnant of a ∼30–32 km-diameter complex impact structure located in northern Lake Superior, Ontario, Canada.

Focusing on clastic systems, and using a combination of seismic examples and models, we present two aspects of stratigraphic trap exploration: (1) the regional and local factors that favour the development of stratigraphic trap edges; and (2) a systematic method for defining and risking the trap edges, avoiding the common problem of over-risking.

Abstract Geological strain analysis of sedimentary rocks is commonly carried out using clast-based techniques. In the absence of valid strain markers, it can be difficult to identify the presence of an early tectonic fabric development and resulting layer parallel shortening (LPS).

This banner text can have markup. web; books; video; audio; software; images; Toggle navigation. The Lake Superior Legacy Collection Field Notebooks,p. 19 BAYLEY, W.S. (a) Marquette Region, Michigan. The Lake Superior Legacy Collection Field Notebooks,45 p. BAYLEY, W.S.

(b) Marquette Iron Range Northeast of Negaunee. The Lake Superior Legacy Collection Field Notebooks,51 p. A Bibliography - Western Michigan University. Download PDF. 1 downloads 16 Oxford, Pergamon Press, p. Eights, J.,Outlines of the geological structure of Lake Superior mineral region belonging to the New York and Lake Superior Mining Company, 21 p.A paleomagnetic reversal in the Osler Volcanic Group, Northern Lake.

EPA/ IDENTIFICATION AND ASSESSMENT OF ASBESTOS EMISSIONS FROM INCIDENTAL SOURCES OF ASBESTOS by R. Kuryvial, R.A. Wood, and Battelle, Columbus Laboratories King Avenue, Columbus, Ohio Contract No.

Task 24 Program Element No. 1AB ROAP No. 21AFA EPA Project Officer: D.K. Oestreich. This book is the first to give a comprehensive and detailed overview of the complete geography of Slovenia in English. Only very few countries, Clastic breccias at the Slates Islands complex impact structure considerably larger ones, can boast the landscape diversity found in Slovenia since the Alps, the Pannonian Basin, the Dinaric Alps, and the Mediterranean meet and interweave in this small corner of Central Europe, as do.

gabbro of the Gem Park complex, a composite funnel- shaped intrusive 11 miles northwest of Westcliffe (loc. The location and arrangement of fenite and car­ bonatite dikes in the complex suggest the existence of an unexposed massive carbonatite at an unknown depth near the center of the complex.

Such a massFile Size: 13MB. Cambrian strata are deployed in a complex anticlinorial structure (De Vos et al., ) forming the core of the Brabant Massif.

The megasequence begins with the km thick Blanmont Formation (base not seen), comprising massive tourmaline-bearing sandstone and quartzite with slate intercalations, for which a rift environment is inferred Cited by: 3.

a textbook of geology by amadeus grabau w. \\ s.b., mass. inst. of technology; s.m., s.d., harvard professor of pal/eontology in the government university of peking, china, and paleontologist to the chinese geological survey formerly lecturer in mineralogy and in geology in tufts.

(Proceedings of the International Conferences on Basement Tectonics 2) Warren B. Hamilton (Auth.), Mervin J. Bartholomew, Donald W. Hyndman, David W. Mogk, Robert Mason (Eds.)-Basement Tectonics 8_ Ch. From here it a hundred over at a point well Lake flowed eastward through Maurepas, Lake Pontchartrain, and Lake Borgne into Mississippi Sound, inundating a wide area, causing months.

The river great damage, and halting railroad traffic for two the Yellow Sea. In The discovery of deficits in Nd/ Nd in mafic rocks of the Nuvvuagittuq supracrustal belt (NSB) has triggered a debate about the possible preservation of Hadean (pre‐ Ga) crustal remnants in the little‐known but areally extensive Innuksuac complex (‐ Ga, Inukjuak domain, Northeast Superior Province, Canada).

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Overlapping species boundaries and hybridization within the Montastrea annularis reef coral complex in the Pleistocene of the Bahama Islands. Paleobiology 30(3) A. Budd and K. Johnson. Lake beds 1, 2 and 3 occur in the wettest phase of nextyear cycle, and Lake bed 4 is the first of (probably) three lake beds marking out the nextyear cycle.

These upper two ~, year cycles occur in the wettest phase of ayear cycle, while the lowest (with lake bed 0) is in the driest phase. Between the front range of the Andes and the Cordillera Vilcapampa there is a broad stretch of mountain country in the lee of the front range which rises to 7, feet (2, m.) at Abra Tocate, and falls off to low hills about Rosalina.

It is all very rough in that there are nowhere any flats except for the narrow playa strips along the streams. † Tota Lake is located 1 h from Sogamoso, a city 3 h away from Bogotá by car (Chap.

† Guatavita Lake is 2 h from Bogotá by car (Chap. † The Bogotá “savanna” surrounds Bogotá and has abundant roads and transportation; likewise, the Tequendama Waterfall is located 2 h away by car (Chap. 10). Notes General Note: Produced by the Organizing Committee of the 16th International Congress of Speleology.

Published by the Czech Speleological Society and the SPELEO and in the co-operation with the International Union of SpeleologyEdited by Michal Filippi, Pavel BosaÌ k Contents Preface Session: Karst And Caves In Carbonate Rocks, Salt And GypsumKarst. The Natural Stone Database for Northern Ireland was constructed to address the paucity of information available to stone conservation practitioners.

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It is obvious now that Darwin did not quite understand the complex structure of the region, as can be seen in the geological map of figure 2, where a western backthrust puts the Auquilco Formation on top of the Agrio Formation and a second fore-thrust repeats again the Agrio and Chachao Formations (Pángaro et al.Giambiagi et al.

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Progressive Metamorphism. Establishment and Definition of the Metamorphic Zones: In his pioneer work upon progressive metamorphism in the Scottish Highlands, Barrow ( and ) established a sequence of metamorphic zones based upon the mineralogical changes observed to take place in sediments of pelitic composition, with gradually increasing metamorphism.

I seek to reconstruct the balance between sediment storage and yield across multiple drainage basin scales in a large (1 km2) watershed in the Northern Cascade range, British Columbia and Washington.

Chilliwack Valley and surrounding area has been the site of numerous studies that have detailed much of its Quaternary sedimentary history. In the present study this Cited by: 2. The Azores islands, owing to their complex geographical and geodynamic setting, are exposed to tsunami events associated with different triggering mechanisms, local or distant.

Since the settlement of the Azores, in the fifteenth century, there have been numerous accounts that relate coastal area flooding episodes with unusually high waves that.

Neto de Carvalho, C. & Rodrigues, J. (eds.) (). New challenges with geotourism. Proceedings of the 8th European Geoparks Conference, Idanha-a-Nova, pp.

Geological study of the Adirondacks began in the s with the forays of Ebenezer Emmons, under the aegis of New York State. Scientific research has continued unabated, and in. G-areilaso do la Vega's description of tho Inca conquests in Antisuyu are well known (Royal Commentaries of the Yncas, Book 4, Chapters 16 Hakluyt Soc.

Publs., 1st Ser., No. 41, and Book 7, Chapters 13 No. 45, ). Salcamayhua a. who. also. chronicles. these. of the eastern valleys. On one. complex and Lower Miocene coarse clastic sediments with tuff intercalations.

K-Ar measurements gave the age of trachyandesite between 16 and Ma (PAMIĆ et al., ). In this study, two 3D seismic volumes as well as a broad network of 2D seismic reflection profiles were used in the subsurface mapping of the Lower Miocene sedimentary bodies.

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Int. J. Earth Sci., 92, Coarse-grained cataclastic breccias up to 50 m thick are exposed along brittle faults striking NE and NW outside the impact crater.

Similar cataclastic breccias are also found within the impact crater but are usually less than a few meters thick. Polymictic clastic matrix breccia is found exclusively within the impact crater.