Zobrazeno 1 - 10
of 49
pro vyhledávání: '"A.N. Zanvilevich"'
Autor:
N.S. Karmanov, Bor-ming Jahn, B.A. Litvinovsky, S.V. Kanakin, A.N. Zanvilevich, Ye. Vapnik, S.M. Wickham
Publikováno v:
Journal of Asian Earth Sciences. 136:16-39
In the study area of 60 by 15 km, located south of Lake Baikal, coeval mafic rocks form small intrusive bodies, synplutonic dikes and composite mafic-felsic dikes in four successive Late Paleozoic and Early Mesozoic syenite and granite suites. Mafic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d15e63b7ecacb5803db9ed29b29096ed
https://doi.org/10.1016/j.jseaes.2016.12.037
https://doi.org/10.1016/j.jseaes.2016.12.037
Publikováno v:
American Journal of Science. 314:462-507
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bf062793331dafab9e54ca9e0ff77cd
https://doi.org/10.2475/02.2014.02
https://doi.org/10.2475/02.2014.02
Publikováno v:
Chemical Geology. 269:153-179
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 Sinai (Egypt) and southern Israel they occupy up to 80% of the expo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::036277d6f1e06160fd280b09d25fe502
https://doi.org/10.1016/j.chemgeo.2009.09.010
https://doi.org/10.1016/j.chemgeo.2009.09.010
Publikováno v:
Lithos. 113:521-539
article i nfo The Central Asian Orogenic Belt (CAOB) is well-known for its massive generation of juvenile crust in the Phanerozoic. In eastern CAOB, voluminous peralkaline and alkaline (alkali-feldspar) granitoids and genetically related bimodal volc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2e4c4e538500cdefd2c1b514e4a8226
https://doi.org/10.1016/j.lithos.2009.06.015
https://doi.org/10.1016/j.lithos.2009.06.015
Autor:
A.N. Zanvilevich, Bor-ming Jahn, B.A. Litvinovsky, M. J. Spicuzza, John W. Valley, M. Eyal, Yaron Katzir, Y. Beeri, Ye. Vapnik
Publikováno v:
Lithos. 97:336-364
Late Neoproterozoic bimodal dyke suites are abundant in the Arabian–Nubian Shield. In southern Israel this suite includes dominant alkaline quartz porphyry dykes, rare mafic dykes, and numerous composite dykes with felsic interiors and mafic margin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eca3fc26eb84fd6e20de3808eb6b56ea
https://doi.org/10.1016/j.lithos.2007.01.004
https://doi.org/10.1016/j.lithos.2007.01.004
Autor:
M. Eyal, E. Shimshilashvili, Yaron Katzir, Y. Beeri, A.N. Zanvilevich, Bor-ming Jahn, B.A. Litvinovsky, John W. Valley, I. Pelly
Publikováno v:
Lithos. 95:208-228
The central pluton within the Neoproterozoic Katharina Ring Complex (area of Gebel Mussa, traditionally believed to be the biblical Mt. Sinai) shows a vertical compositional zoning: syenogranite makes up the bulk of the pluton and grades upwards to a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd53aafff1bdeb37b5a711736ba194bc
https://doi.org/10.1016/j.lithos.2006.07.013
https://doi.org/10.1016/j.lithos.2006.07.013
Publikováno v:
Israel Journal of Earth Sciences. 55:69-93
Katzir, Y., Litvinovsky, B., Eyal, M., Zanvilevich, A., and Vapnik, Y. 2006. Four successive episodes of Late Pan-African dikes in the central Elat area, southern Israel.lsr. J. Earth Sci. 55: 69-93. Four successive Late Pan-African dike suites are r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::195da3e60f48006f7810773ec183d394
https://doi.org/10.1560/ijes_55_2_69
https://doi.org/10.1560/ijes_55_2_69
Publikováno v:
Journal of African Earth Sciences. 40:115-136
Calc-alkaline leucocratic granites that were emplaced at the late post-collision stage of the Pan-African orogeny are abundant in the northern half of the Arabian-Nubian Shield. Commonly, they are referred to as the Younger Granite II suite. In south
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37a8a19f4613fc7a1f62e2109287c696
https://doi.org/10.1016/j.jafrearsci.2004.11.005
https://doi.org/10.1016/j.jafrearsci.2004.11.005
Publikováno v:
Lithos. 64:97-130
The Oshurkovo Complex is a plutonic sheeted complex which represents numerous successive magmatic injections into an expanding system of subparallel and subvertical fractures. It comprises a wide range of rock types including alkali monzodiorite, mon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c12ae6f3bdfa4efcd753779b0b17395a
https://doi.org/10.1016/s0024-4937(02)00179-2
https://doi.org/10.1016/s0024-4937(02)00179-2
Autor:
Andrew D. Saunders, Marc K. Reichow, A.N. Zanvilevich, Bor-ming Jahn, B.A. Litvinovsky, D. V. Kuz’min, A.V. Titov, S. Poulain
Publikováno v:
Chemical Geology. 189:105-133
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. The Bryansky Complex is a large
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8bd16fec8263ce5d1a8984fbd3ad1480
https://doi.org/10.1016/s0009-2541(02)00142-0
https://doi.org/10.1016/s0009-2541(02)00142-0