Zobrazeno 1 - 10
of 57
pro vyhledávání: '"B.A. Litvinovsky"'
Publikováno v:
Precambrian Research. 320:137-170
The Elat Metamorphic Complex (EMC), part of the Arabian-Nubian Shield exposed at Elat and Taba areas (S. Israel and NE Sinai, Egypt), records a full orogenic cycle from island arc to syncollisional stages that extended ∼240 My. New SIMS U–Pb dati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a96314ba8800a8d13cedda77f654599
https://doi.org/10.1016/j.precamres.2018.10.003
https://doi.org/10.1016/j.precamres.2018.10.003
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:
Lithos. :106049
Continental-scaled magmatic activity occurs after the end of collision-orogenic stages of the Wilson cycle. This post-collisional magmatism is widely exhibited, from 635 to 540 Ma, in a series of large Neoproterozoic (Pan-African) orogenic belts thro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5a82d144f8df030382c3c61dbfe604a
https://doi.org/10.1016/j.lithos.2021.106049
https://doi.org/10.1016/j.lithos.2021.106049
Publikováno v:
Lithos. 232:242-265
Granite is generally dominant in A-type igneous suites but these frequently include also alkali feldspar- and peralkaline- syenite and quartz syenite. Such syenites can provide essential information about magma sources and mode of generation of A-typ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::deffe3593c21924292025f70d53943a8
https://doi.org/10.1016/j.lithos.2015.06.008
https://doi.org/10.1016/j.lithos.2015.06.008
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:
Gondwana Research. 25:338-357
Four isolated metamorphic complexes located within post-collisional granitoids occupying up to 70% of the total area, were distinguished in Sinai (Egypt) and Elat area (southern Israel), the northernmost part of the Arabian–Nubian Shield. The metam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c165c54d349764590975fbf29412276d
https://doi.org/10.1016/j.gr.2013.03.016
https://doi.org/10.1016/j.gr.2013.03.016
Publikováno v:
Geology. 40:403-406
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 format
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1b0720eaab2d0d4f51e697e0432bad4
https://doi.org/10.1130/g32788.1
https://doi.org/10.1130/g32788.1
Publikováno v:
Lithos. 125:845-874
The Late Palaeozoic voluminous magmatism in Transbaikalia, Russia (a territory of > 600,000 km 2 to the east of Lake Baikal) is highly diverse and complex. Of special interest are (1) the significant overlap in time between magmatic suites commonly a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a9d4fe5525acd89f549b9b660b3b22f
https://doi.org/10.1016/j.lithos.2011.04.007
https://doi.org/10.1016/j.lithos.2011.04.007
Autor:
Bor-ming Jahn, B.A. Litvinovsky, D.Y. Liu, S.L. Presnyakov, Marc K. Reichow, A.A. Tsygankov, Sergey Sergeev, Ye.N. Lepekhina, A.N. Larionov
Publikováno v:
Russian Geology and Geophysics. 51:972-994
The Late Paleozoic intrusive rocks, mostly granitoids, totally occupy more than 200,000 km2 on the territory of Transbaikalia. Isotopic U-Pb zircon dating (about 30 samples from the most typical plutons) shows that the Late Paleozoic magmatic cycle l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8ffbb4c7d1e3af7fae496fdea7ead7c
https://doi.org/10.1016/j.rgg.2010.08.007
https://doi.org/10.1016/j.rgg.2010.08.007
Publikováno v:
Chemical Geology. 273:120-135
The Mongolian–Transbaikalian Belt (MTB) is the largest and most representative component of the Central-Asian network of Late Paleozoic and Mesozoic granites and syenites and associated volcanic rocks. The MTB incorporates over 350 individual pluto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f87231b7f25f8d9c8fff4a977228c32
https://doi.org/10.1016/j.chemgeo.2010.02.017
https://doi.org/10.1016/j.chemgeo.2010.02.017