precambrian metamorphic rocks around the Lake Vegår (Aust-Agder, southern Norway) by Jacques Touret

Cover of: precambrian metamorphic rocks around the Lake Vegår (Aust-Agder, southern Norway) | Jacques Touret

Published by Universitetsforlager in Oslo .

Written in English

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  • Petrology -- Norway -- Aust-Agder,
  • Rocks, Metamorphic

Edition Notes

Book details

SeriesNorges geologiske undersøkelse, nr. 257
LC ClassificationsQE475 T68
The Physical Object
Number of Pages45
ID Numbers
Open LibraryOL18680383M

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Additional Physical Format: Online version: Touret, Jacques L.R., Precambrian metamorphic rocks around the Lake Vegår (Aust-Agder, southern Norway). The Precambrian (or Pre-Cambrian, sometimes abbreviated pЄ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon.

The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. Jennings, C.W.,An explanatory text to accompany thescale fault and geologic maps of California: California Division of Mines and Geology, Bulletinp.

The Pre-Cambrian Earth Pre-Cambrian ( to bya) The PreCambrian represents the first 4 billion years of earth history (approx. 85%) Pre-Cambrian rocks make up the bulk of continental crustal rocks.

Mostly obscured by a relatively thin veneer of Phanerozoic sedimentary, igneous, and metamorphic rocks. Igneous, metamorphic, and metasedimentary rocks, which make up the Precambrian basement complex, underlie the entire state of Kansas (Fig. Most boreholes that have penetrated Precambrian rocks are located along the crests of anticlines or structural highs; therefore, the overall distribution of rock types is known only vaguely.

These rocks are visible at Pictured Rocks National Lakeshore. Source: Photograph by Randy Schaetzl, Professor of Geography - Michigan State University The Jacobsville sandstone, one of the most beautiful rocks in Michigan and also a sandstone formed during the. Precambrian Rocks in the Cordes Area, Yavapai County, Arizona By C.

ANDERSON GEOLOGICAL SURVEY BULLETIN A study of the stratigraphy and structure of the Precambrian stratified and intrusive rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: Cited by: 2. Stratigraphy, continued Precambrian Rocks. Precambrian rocks are not exposed in Kansas but are extensively known from well data.

Approximately 2, wells are known to have penetrated the Precambrian basement rock complex, which is shallowest at about feet, over the Nemaha ridge in northeastern Kansas, and deepest at about 9, feet in the Hugoton Embayment.

In the park, the Gunnison River cuts through Precambrian rock nearly 2 billion years old. Most of these rocks are metamorphic and show evidence of exposure to extreme pressures and temperatures. Some of the rocks are igneous and formed from magma that pushed its way up into cracks in the Earth's crust, where it cooled and crystallized.

the rocks of Powder Mill (Precambrian Y) age as well. Precambrian W rocks in the area have been affected by at least four sepa­ rate metamorphic events, although the Cited by: 3. Ion microprobe U-Th-Pb analyses of residual cores and metamorphic mantles of zircons from three high grade paragneisses from the Seve Nappe Complex, north-western Sweden, show that: 1) The sediments comprising the protolith of the Seve Nappes gneisses over a distance of km were probably derived from similarly-aged source terranes.

2) Those source terranes were dominated by Cited by: The Precambrian rocks, older than 2, m.y., in the Saganaga Lake-Northern Light Lake area on the Minnesota-Ontario boundary include a thick succession of metavolcanic rocks, chiefly greenstone but with some intermediate to silicic types, and minor metasediments; the Northern Light Gneiss; the Saganaga Tonalite; alkalic syenodiorite and granodiorite; and the Knife Lake Group.

The Precambrian period accounts for 88 per cent of geological time. Neoproterozoic. There are very varied deposits from the Neoproterozoic, including volcanic sequences, sedimentary rocks formed in environments from deep water to terrestrial, plutonic igneous rocks and metamorphic rocks.

Multicellular life developed and diversified rapidly. The present investigation, carried out since as part of continuing studies of the Lower Precambrian rocks of northern Minnesota, has consisted of broad regional geologic mapping in the western half of the district and adjacent areas (Sims and others, ; Sims and others, ) and detailed mapping and study of critical areas (Gabbro Lake quadrangle, Green and others, ; and Green Cited by: 1.

Metamorphic rock, any rock that results from the alteration of preexisting rocks in response to changing conditions, such as variations in temperature, pressure, and mechanical stress, and the addition or subtraction of chemical components. The preexisting rocks may be igneous, sedimentary, or other metamorphic rocks.

The metamorphic rocks tell this tale of change but in them are many other records buried and lost. The western UP has a variety of Precambrian rocks formed through igneous or metamorphic activity: crystalline rocks. Many of these are NOT sedimentary rocks, such as are found in the Michigan Basin.

Geologic unit mapped in California: Conglomerate, shale, sandstone, limestone, dolomite, marble, gneiss, hornfels, and quartzite; may be Paleozoic in part. Petrology and Origin of Precambrian Metamorphic Rocks in the eastern Ruby Mountains, Sout i Montana (84 pp.) Precambrian schists and gneisses are exposed in much of the Ruby Mountains of southwestern Montana.

The major rock types include abundant quartz-feldspar gneiss, hornblende gneiss, amphibolite, quartzitic gneiss, and : Kevin Smith. The trondhjemitic Northern Light Gneiss, Saganaga Tonalite, and syenodioritic to granodioritic Icarus pluton are part of a typical Archean igneous sequence that began with the extrusion of large volumes of basic volcanics, which make up large parts of present-day greenstone belts, and ended with a small post-kine-matic alkalic stock.

within the rest of the Precambrian rocks in Nigeria, he grouped the rocks in this region as migmatite – gneiss complex comprising largely of sedimentary series with associated minor igneous rock intrusions which have been altered by metamorphic, migmatitic and granitic processes.

Odeyemi () suggestedFile Size: 1MB. Lake Agassiz prior to the disappearance of the ice sheet which prevented northward drainage to Hudson Bay. As can be seen in Figure 2, the Precambrian rocks of Minnesota occupy a central position in the North American continent.

This position is reflected in the present day drainage pattern of. Nonfoliated metamorphic rocks are formed around igneous intrusions where the temperatures are high but the pressures are relatively low and equal in all directions (confining pressure).

The original minerals within the rock recrystallize into larger sizes and the atoms become more tightly packed together, increasing the density of the rock.

Principles of Precambrian Geologyis an update to the book, Precambrian Geology: The Dynamic Evolution of the Continental Crust, by the same new edition covers the same topics in a more concise and accessible format and is replete with explanatory figures, tables, and by:   The Precambrian metamorphic rocks of Ceylon consist of basement gneisses, termed the Vijayan Series; which are overlain by supracrustal metasediments of the Highland Series and Southwest Group.

All these rocks have been formed deep in the earths crust under PT conditions of the granulite facies. The apparent differences in metamorphic grade, structure and ultimately topographical Cited by: All metamorphic rocks in Colorado are precambrian metagranite, monozite, schist, gneiss, pelite, phyllite, etc, occurring along the Yavapai-Mazatzal terrane suture zone.

Most were uplifted once during the Permian (the Ancestral Rockies), and so the second Laramide uplift (ongoing, began 65mya) is exposing ancient mountain roots. Gravelly Range, the low grade metamorphic rocks abut silliminite schists to the north and staurolite schist to the south (Vargo, ).

This work uses structural style, petrography, and field relationships to constrain possible protoliths and tectonic settings of the rocks of the central Gravelly Range. In doing so, it puts the central. Most of the rocks exposed along the length of the Black Canyon are Precambrian in age (older than million years) and are either metamorphic, or igneous, with some sedimentary layers evident along the North Rim.

The rocks in the Black Canyon have a wide variety of minerals. Here is a brief look at some of them and where they may be found. From rocks of the Ishua Super Group in Greenland come possibly the earliest cells, as much as billion years oldest known rocks on Earth are billion years old and are from Arctic Canada.

Thus, life appears to have begun soon after the cooling of the Earth and formation of the atmosphere and oceans. Precambrian metamorphic conditions and crustal evolution, northeastern Alberta, Canada. Precambrian Res., A complex of Precambrian po]ymetamorphie gneisses and granitoids of the Churchill structural province, northeastern Alberta, Canada has been examined structurally, petrographically, chemically and by: Geology of the Older Precambrian Rocks in the Vicinity of Clear Creek and Zoroaster Canyon, Grand Canyon, Arizona.

M.S. thesis, Western Washington State College, 78 pp. Lingley, W.S., Some structures in older Precambrian rocks of the Clear Creek- Cited by: Metamorphic rocks started out as some other type of rock, but have been substantially changed from their original igneous, sedimentary, or earlier metamorphic form.

Metamorphic rocks form when rocks are subjected to high heat, high pressure, hot mineral-rich fluids or. The Precambrian is an informal name for the eons of the geologic timescale that came before the current Phanerozoic eon.

It spans from the formation of Earth around Ma (million years ago) to. Precambrian rocks in the bottom of the canyon at Hance Rapids, eastern Grand Canyon. The lower red rock unit is siltstone and shale, and the upper rock is sandstone.

There is also a dark-colored igneous rock. What are the relative ages of these three rocks. Paleozoic rocks. A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the full-text.

Paul W. Gast, J. Laurence Kulp and Leon E. Long, Reply to Osterwald's discussion of “Absolute age of early Precambrian rocks in the Bighorn Basin of Wyoming and Montana, and southwestern Manitoba”, Journal of Geophysical Research, 64, 9, (), ().

Strategraphy and Metamorphism of Late Precambrian Rocks in Central Northeastern Nevada and Adjacent Utah [Misch and Hazzard] on *FREE* shipping on qualifying offers. Strategraphy and Metamorphism of Late Precambrian Rocks in Central Northeastern Nevada and Adjacent UtahAuthor: Misch and Hazzard.

Venugopal ). The metamorphic grade continues to increase southward to homblende granulite facies west of Åmli (Ploquin, written comm. ) and near the lake Vegår (Touret ), to granulite facies along the Ska­ gerrak coast (Bugge ).

Concomitant with the southerly increase in grade. Precambrian shields comprise the cores of the continents and extend under Phanerozoic cover sequences. The shields consist of Archean cratons welded together and surrounded by Proterozoic orogens (ancient mountain belts).

Figure 1 is a map of the world showing areas where Precambrian rocks are exposed at the surface. The Phanerozoic represents theFile Size: KB. If you like this lecture from the IGH Conference, you can get it and over 70 more at: Dr.

Snelling completed a. Peak Metamorphic Suite (SPMS) and the Indian Creek Metamorphic Suite (ICMS). Additionally, metamorphic monazites from the Tobacco Root Mountains yield bimodal ages: Ga and Ga, the latter being assigned to the Big Sky orogeny (Cheney et al., b). ICMS rocks have both ages, whereas SPMS rocks only contain the Ga Size: 1MB.

CHAPTER(1:(PRECAMBRIAN(ROCKS(OF(THE(GRANDCANYON! JOSHUA’GARBER’ INTRODUCTION(! InhisexpeditionthroughtheGrandCanyon,JohnWesleyPowellidentifiedand! .rocks in Lakselv valley are therefore Precambrian rocks.

In Norway these rocks are known as "grunnfjell" and the term Pre-Eocambrian has been applied to them (for example HoltedahlPl. 1). 1 The actual contact between the sedimentary rocks in the Lakselv valley area and the underlying metamorphic rocks was observed in three places that.

I had the children put a book on top of the bag (to distribute the pressure more evenly) and count to Your sedimentary rock has metamorphosed into a metamorphic rock! You can see the mineral components are basically the same, but they look totally different.

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