B
B.A. Litvinovsky
Researcher at Ben-Gurion University of the Negev
Publications - 26
Citations - 1957
B.A. Litvinovsky is an academic researcher from Ben-Gurion University of the Negev. The author has contributed to research in topics: Silicic & Mafic. The author has an hindex of 20, co-authored 26 publications receiving 1713 citations. Previous affiliations of B.A. Litvinovsky include University of Chicago & Russian Academy.
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Peralkaline granitoid magmatism in the Mongolian-Transbaikalian Belt: Evolution, petrogenesis and tectonic significance
TL;DR: In the Central Asian Orogenic Belt (CAOB) as discussed by the authors, voluminous peralkaline and alkaline (alkali-feldspar) granitoids and genetically related bimodal volcanics were emplaced in three stages from Early Permian to late Mesozoic: 295-270 Ma, 230-190 Ma and 150-120 Ma.
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Origin and evolution of post-collisional magmatism: Coeval Neoproterozoic calc-alkaline and alkaline suites of the Sinai Peninsula
TL;DR: In this article, the authors compared the geochemical properties of calc-alkaline and peralkaline granitoids from the two igneous suites in the northernmost part of the Arabian-Nubian Shield.
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Petrogenesis of syenite-granite suites from the Bryansky Complex (Transbaikalia, Russia): Implications for the origin of A-type granitoid magmas
B.A. Litvinovsky,Bor-ming Jahn,A.N. Zanvilevich,Andrew D. Saunders,S. Poulain,D. V. Kuz’min,Marc K. Reichow,A.V. Titov +7 more
TL;DR: Two syenite-granite suites, metaluminous and peralkaline, that form the Bryansky Complex in Transbaikalia, Russia, have been studied with the aim to constrain the existing models of A-type granitoid magma generation.
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Silicic Magma Formation in Overthickened Crust: Melting of Charnockite and Leucogranite at 15, 20 and 25 kbar
TL;DR: In this article, the authors show that at degrees of melting below 15, 20 and 25 kbar, the granitic>15 kbar were melt composition obtained in the experiments diVers from that ofperformed on Archaean biotite-bearing charnockite of opx-bearing A-type granite.
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The Sa'al volcano-sedimentary complex (Sinai, Egypt): A latest Mesoproterozoic volcanic arc in the northern Arabian Nubian Shield
Yaron Be'eri-Shlevin,Yaron Be'eri-Shlevin,M. Eyal,Yehuda Eyal,Martin J. Whitehouse,B.A. Litvinovsky +5 more
TL;DR: In this article, new zircon U-Pb age data and geochemistry for the Sa9al metamorphic complex (SMC) in Sinai (Egypt) provide the first robust evidence of latest Mesoproterozoic island arc rocks at the northernmost Arabian-Nubian Shield, possibly indicating that formation of the shield commenced prior to 870 Ma.