The Sveconorwegian orogeny
This article reviews the geology of the Sveconorwegian orogen in south Scandinavia and
existing tectonic models for the Mesoproterozoic to Neoproterozoic Sveconorwegian …
existing tectonic models for the Mesoproterozoic to Neoproterozoic Sveconorwegian …
A geochemical classification for granitic rocks
BR Frost, CG Barnes, WJ Collins, RJ Arculus… - Journal of …, 2001 - academic.oup.com
This geochemical classification of granitic rocks is based upon three variables. These are
FeO/(FeO+ MgO)= Fe-number [or FeO tot/(FeO tot+ MgO)= Fe*], the modified alkali–lime …
FeO/(FeO+ MgO)= Fe-number [or FeO tot/(FeO tot+ MgO)= Fe*], the modified alkali–lime …
The “Taourirt” magmatic province, a marker of the closing stage of the Pan-African orogeny in the Tuareg shield: review of available data and Sr–Nd isotope evidence
A Azzouni-Sekkal, JP Liégeois… - Journal of African Earth …, 2003 - Elsevier
The Tuareg Shield, located between the Archaean to Palaeoproterozoic Saharan
metacraton and the West African craton, is composed of 23 recognized terranes that welded …
metacraton and the West African craton, is composed of 23 recognized terranes that welded …
Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and peralkaline granitoids. The use of sliding normalization
JP Liegeois, J Navez, J Hertogen, R Black - Lithos, 1998 - Elsevier
Abundant high-K calc-alkaline (HKCA) magmatism appears to be post-collisional and often
shifts to shoshonitic or alkaline–peralkaline compositions in the final stages of orogeny. The …
shifts to shoshonitic or alkaline–peralkaline compositions in the final stages of orogeny. The …
Low-degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogranite-porphyry, east Tibet: geochemical and Sr–Nd–Pb–Hf …
YH Jiang, SY Jiang, HF Ling, BZ Dai - Earth and Planetary Science Letters, 2006 - Elsevier
SHRIMP zircon U–Pb dating, mineral chemical, element geochemical and Sr–Nd–Pb–Hf
isotopic data have been determined for the Yulong monzogranite-porphyry in the eastern …
isotopic data have been determined for the Yulong monzogranite-porphyry in the eastern …
Origin and evolution of post-collisional magmatism: coeval Neoproterozoic calc-alkaline and alkaline suites of the Sinai Peninsula
Two Late Neoproterozoic post-collisional igneous suites, calc-alkaline (CA) and alkaline–
peralkaline (Alk), widely occur in the northernmost part of the Arabian–Nubian Shield. In …
peralkaline (Alk), widely occur in the northernmost part of the Arabian–Nubian Shield. In …
Origin and evolution of overlapping calc-alkaline and alkaline magmas: The Late Palaeozoic post-collisional igneous province of Transbaikalia (Russia)
BA Litvinovsky, AA Tsygankov, BM Jahn, Y Katzir… - Lithos, 2011 - Elsevier
The Late Palaeozoic voluminous magmatism in Transbaikalia, Russia (a territory of>
600,000 km2 to the east of Lake Baikal) is highly diverse and complex. Of special interest …
600,000 km2 to the east of Lake Baikal) is highly diverse and complex. Of special interest …
Zircon geochronology and Sr, Nd, Pb isotope geochemistry of granitoids from Bayuda Desert and Sabaloka (Sudan): evidence for a Bayudian event (920–900 Ma) …
D Küster, JP Liégeois, D Matukov, S Sergeev… - Precambrian …, 2008 - Elsevier
Results of zircon geochronology and Sr, Nd and Pb isotope investigations carried out on
granitoid rocks from the boundary of the Saharan Metacraton with the Arabian–Nubian …
granitoid rocks from the boundary of the Saharan Metacraton with the Arabian–Nubian …
New insights into the crustal growth of the Paleoproterozoic margin of the Archean Kéména-Man domain, West African craton (Guinea): Implications for gold mineral …
Abstract The Baoulé-Mossi Paleoproterozoic domain on the West African Craton is known
for its world-class orogenic gold deposits formed during the Eburnean orogeny between ca …
for its world-class orogenic gold deposits formed during the Eburnean orogeny between ca …
Petrogenesis of Tarom high-potassic granitoids in the Alborz–Azarbaijan belt, Iran: Geochemical, U–Pb zircon and Sr–Nd–Pb isotopic constraints
Abstract Large-scale Upper Eocene plutons in the Western Alborz–Azarbaijan orogenic belt
mostly show calc-alkaline and I-type geochemical features contrasted by the Tarom complex …
mostly show calc-alkaline and I-type geochemical features contrasted by the Tarom complex …