1 edition of Tectono-metamorphic evolution of the Raahe-Ladoga zone found in the catalog.
Tectono-metamorphic evolution of the Raahe-Ladoga zone
Includes bibliographical references (p. 96).
|Other titles||Raahe-Ladoga zone.|
|Statement||edited by Kalevi Korsman.|
|Series||Bulletin / Geological Survey of Finland,, 343, Bulletin (Geologian tutkimuskeskus (Finland)) ;, 343.|
|LC Classifications||QE633.F5 T43 1988|
|The Physical Object|
|Pagination||96 p. :|
|Number of Pages||96|
|LC Control Number||88202675|
Tectono-metamorphic evolution of the pre-Athabasca basement within the Wollaston–Mudjatik Transition Zone, Saskatchewan Pauline Jeanneret, Philippe Goncalves, Cyril Durand, Pierre Trap, Didier Marquer, David Quirt, Patrick LedruCited by: Gupta, P., & Rai Choudhuri, A. (). Tectono-metamorphic evolution of the amphibolite and granulite facies rocks of the Sandmata Complex, central Rajasthan. Indian Minerals, 6(1–2), – Google ScholarAuthor: D. B. Guha.
Petrological and fluid-inclusion data of high-grade metapelitic gneisses that occur as enclaves and in the immediate surroundings of the Ga old Bulai granitoid intrusive are presented in this chapter. The Bulai intrusive is an important time marker in the tectono-metamorphic evolution of the Central Zone of the Limpopo Complex. The host-rock gneisses show one generation of garnet Cited by: 9. Tectonic mélange is an ideal research target to use to decipher the tectono-metamorphic evolution of an orogenic belt, and therefore it is necessary to further explore the metamorphic evolution of tectonic mélanges. In the km-long Paleozoic Dunhuang orogenic belt, northwest China, only two localities of tectonic mélange have been by: 9.
STEFANO CATALANO, ROSOLINO CIRRINCIONE, PAOLO MAZZOLENI, FRANCESCO PAVANO, ANTONIO PEZZINO, GINO ROMAGNOLI, GIUSEPPE TORTORICI; The effects of a Meso-Alpine collision event on the tectono-metamorphic evolution of Cited by: 3. The core zone corresponds to the zone of highest strain and is well defined structurally by the occurrence of gouges and/or foliated cataclasites and physically by separating a hanging wall from a footwall. Deformation in the fault zones occurred under greenschist facies to seafloor conditions and within the stability field of by:
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Tectono-Metamorphic Evolution of the Raahe-Ladoga Zone by Kalevi Korsman Unknown, 96 Pages, Published ISBN / ISBN / The figures were drawn by Minna Ahokas, Pir- jo Hyvarinen and Elsa : ISBN: OCLC Number: Description: 96 pages: illustrations, maps ; 25 cm. Series Title: Bulletin (Geologian tutkimuskeskus (Finland.
Combining our results with the P–T and structural evolution of the Piedmont zone, we propose a four stages tectonic and metamorphic evolution for the Internal Alps (Table 4 and Fig. 15). (1) Between 60 and 50 Ma, burial of the Piedmont zone in an oceanic subduction context (top to the NW thrusting).Cited by: Several tectonic and tectono-metamorphic models have been proposed in the literature, but each of them strongly relies on how the units within the Nevado-Filábride complex are defined.
Brouwer () first distinguished two formations based on lithological criteria: the lowermost Crystalline of Sierra Nevada and the Mischungszone – mixed – zone.
Since that, the division has remained a matter of debate Author: Ángel Santamaría-López, Pierre Lanari, Carlos Sanz de Galdeano. Approximately 90% of gold deposits lie within the ~km wide contact-aureole, and most of these are concentrated in, and just beyond, the biotite-albite-epidote zone (km from granitoid.
The Tethyan Sedimentary Sequence, one of the major tectonic units of the Himalayan belt cropping out in the inner portion of the Himalayan belt, has been investigated in SE Tibet to unravel its. The aim of this paper is to constrain the tectono-metamorphic evolution in another tract of the Middle Tuscan Range (Fig.
1B) located 40 km to the north with respect to the easternmost area where HP-LT assemblage was documented (Monte Leoni area, Giorgetti et al., ). Petrographic, mineralogical and structural data are therefore presented to discuss the development of Mg–carpholite bearing quartz Cited by: FH1 Program Preliminary Safety Analysis Report Chapter 1: General Plant Description Tectono-metamorphic evolution of the Raahe-Ladoga zone, Introduction.
Preliminary Safety Analysis. Tectono-metamorphic evolution of the Neyriz metamorphic complex, Quri-Kor-e-Sefid area (Sanandaj-Sirjan Zone, SW Iran)Cited by: Tectono-metamorphic evolution. Left column: line and area balanced profiles, right column: temperature evolution for selected stages of the tectono-metamorphic history of the Helvetic Alps in Western Switzerland indicated by by: Cite this paper M.
Tairou and P. Affaton, "Structural Organization and Tectono-Metamorphic Evolution of the Pan-African Suture Zone: Case of the Kabye and Kpaza Massifs in the Dahomeyide Orogen in Northern Togo (West Africa)," International Journal of Geosciences, Vol.
4 No. 1,pp. doi: /ijgCited by: 3. Tectono-metamorphic evolution of an evaporitic décollement as recorded by mineral and fluid geochemistry: The “Nappe des Gypses” (Western Alps) case study Article in Lithos The tectono-metamorphic evolution of the Site peridotites was described by Beslier et al.
Here, four stages were recognized, high-temperature ( ° ° C) ductile shearing, limited partial melting, subsolidus reequilibration in the plagioclase field at.
The Paleoproterozoic tectono-metamorphic evolution of the pre-Athabasca basement (∼ Ga) within the Wollaston–Mudjatik Transition Zone (WMTZ) (Saskatchewan, Canada) has been characterized using both exposed basement and drill cores Cited by: A 50 to m wide mylonite zone, with a D2 top-to-NW sense of shear marks the boundary to the Simano Nappe.
Throughout the Leventina Nappe only small. This is a suitable setting in which to study the relationship between tectono-metamorphic evolution and argon isotope records in white micas.
This paper reports the results of a detailed microtextural and microchemical study and in situ 40 Ar– 39 Ar laser experiments on metamorphic samples from the garnet zone to the sillimanite + K-feldspar Cited by: The Kabye and Kpaza Massifs correspond to two main granulitic suites in the suture zone of the Pan-African Dahomeyide orogenic belt, in northern Togo.
The Kabye Massif is composed of an important west verging nappe pile subdivided into two petrographic units. The nappes in its western petrographic unit are made up of leucocratic garnetbearing granulites defined as the “Lassa-Soumdina Cited by: 3.
The Bulai intrusive is an important time marker in the tectono-metamorphic evolution of the Central Zone of the Limpopo Complex. The host-rock gneisses show one generation of garnet, cordierite, and sillimanite, whereas the enclave gneisses show two different generations of garnet (Grt 1,2), cordierite (Crd 1,2), and sillimanite (Sil 1,2).
Rütti R., Marquer D., Thompson A.B. () Tertiary tectono-metamorphic evolution of the European margin during Alpine collison: example of the Leventina Nappe (Central Alps, Switzerland). In: Froitzheim N., Schmid S.M. (eds) Orogenic Processes in the Alpine Collision Zone. Swiss Journal of Geosciences Supplement, vol 3.
Birkhäuser, BaselCited by: 7. Tectono-metamorphic evolution of the Raahe-Ladoga zone Teollisuuden tukijalasta verkostoyhteiskunnan osaksi The 13th International Symposium on Deep Seismic Profiling of the Continents and Their Margins: JuneSaariselkä, Inari, Finland: [programme and abstracts].
Tectono-metamorphic evolution of the pre-Athabasca basement within the Wollaston–Mudjatik Transition Zone, Saskatchewan. Pauline Jeanneret, Philippe Goncalves, Cyril Durand, Pierre Trap, Didier Marquer, David Quirt, Patrick Ledru.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.crust in the Eastern Alps – the Eclogite Zone.
Despite being amongst Earth’s best studied orogens, little is understood about the rates of Alpine metamorphism within an inﬂuential role in the tectono–metamorphic evolution of the Eastern Alps and in overthrust terrains in general.