Results 81 to 90 of about 23,165 (232)

An archean suture zone in the Tobacco Root Mountains? (1984) Evolution of Archean Continental Crust, SW Montana (1985) [PDF]

open access: yes
The Lake Plateau area of the Beartooth Mountains, Montana were mapped and geochemically sampled. The allochthonous nature of the Stillwater Complex was interpreted as a Cordilleran-style continental margin.
Kain, L., Mogk, D. W.
core   +1 more source

Physicochemical conditions of the formation of the Larino granite-gneiss dome (South Ural)

open access: yesGeoresursy
The Larino granite-gneiss dome is located on the border of the Aramil-Sukhtelya and Magnitogorsk megazones and is a two-headed anticlinal structure, the nuclear parts of which are composed of granitoids of the Pervomai and Larino massifs, and their ...
V. I. Snachev   +2 more
doaj   +1 more source

Transitional amphibolite-granulite facies granites, diorites and metavolcanic amphibolites in the Isukasia map sheet, southern West Greenland

open access: yesRapport Grønlands Geologiske Undersøgelse, 1982
Detailed mapping of the north-west quadrant of the 1: 100 000 scale Isukasia geological map sheet was begun in 1981 (fig. 16). The area was previously visited during the 1977 helicopter reconnaissance mapping programme (Allaart et al., 1978) and from this work the stratigraphy was known only in the broadest of terms.
R.P Hall, D.J Hughes
openaire   +2 more sources

Regional variation in the Amitsoq gneisses related to crustal levels during late Archean granulite facies metamorphism: Southern west Greenland [PDF]

open access: yes
The dominant lithology at Kangimut sangmissoq is described as nebulitic tonalitic gneiss containing highly distended plagioclase phyric amphibolites. The gneiss amphibolite complex was intruded by Nuk gneiss between 3.05 and 2.90 Ga and later (2.6 to 2.7
Bridgwater, D.   +2 more
core   +1 more source

Evidence from Rb–Sr mineral ages for multiple orogenic events in the Caledonides of Shetland, Scotland [PDF]

open access: yes, 2015
Shetland occupies a unique central location within the North Atlantic Caledonides. Thirty-three new high-precision Rb–Sr mineral ages indicate a polyorogenic history.
Bird, A. F.   +3 more
core   +3 more sources

Petrography and geochemistry of biotite gneiss and amphibolite mined as aggregates and the environmental impact of quarrying operations in Logbadjeck, Cameroon

open access: yesDiscover Geoscience
Logbadjeck is situated in the northern edge of the Congo Craton, Nyong Series, Cameroon. This paper presents the petrographic and geochemical characteristics of biotite gneiss and amphibolite mined as aggregates and the environmental impact of quarrying ...
Anicet Feudjio Tiabou   +5 more
doaj   +1 more source

Scheme of mineral facies of metamorphic rocks and its application to the Fennoscandian shield with representative sites of orogenic gold mineralization

open access: yesTransactions of the Karelian Research Centre of the Russian Academy of Sciences, 2015
Our recent studies of metamorphism within the Fennoscandian (or Baltic) Shield area with representative sites of orogenic gold mineralization based on the scheme of mineral facies of metamorphic rocks introduced earlier inspired thorough revision of that
Сергей Алексеевич Бушмин   +3 more
doaj   +1 more source

Significance of the late Archaean granulite facies terrain boundaries, Southern West Greenland [PDF]

open access: yes
Three distinct episodes and occurrences of granulite metamorphism in West Greenland are described: (1) the oldest fragmentary granulites occur within the 3.6-Ga Amitsoq gneisses and appear to have formed 200 Ma after the continental crust in which they ...
Friend, C. R. L.   +2 more
core   +1 more source

The Sanford Underground Research Facility at Homestake

open access: yes, 2014
The former Homestake gold mine in Lead, South Dakota is being transformed into a dedicated laboratory to pursue underground research in rare-process physics, as well as offering research opportunities in other disciplines such as biology, geology and ...
Heise, J.
core   +2 more sources

Varying rock responses as an indicator of changes in CO2-H2O fluid composition [PDF]

open access: yes
The formation of the late Archean charnockite zone of southern India was ascribed to dehydration recrystallization due to an influx of CO2. Pressure temperature conditions for the metamorphism were calculated at about 750 C and 7.5 Kbar.
Friend, C. R. L.
core   +1 more source

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