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Reply to Comment of Y. Kolodny, A. Burg and A. Sneh on 'Combustion metamorphism in the Nabi Musa dome: new implications for a mud volcano origin of the Mottled Zone, Dead Sea area', by E. Sokol, I. Novikov, S. Zateeva, Ye. Vapnik, R. Shagam and O. Kozmenk

Autor: Ye. Vapnik, I. S. Novikov

Publikováno v: Basin Research. 25:115-120

The dominating paradigm for most Israeli and Jordanian geologists relates to the genesis of the Mottled Zone (MZ) to the surface combustion of bituminous chalk with common organic content below 15 wt.%. Our hypothesis (Sokol et al., 2007, 2008) also

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::bcb8662d404d7980234923a915cd4ee2
https://doi.org/10.1111/bre.12007

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Akademický článek

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Akademický článek

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Comment on 'Combustion metamorphism (CM) in the Nabi Musa dome: new implications for a mud volcanic origin of the Mottled Zone, Dead Sea area', by: E. Sokol, I. Novikov, S. Zateeva, Ye. Vapnik, R. Shagam and O. Kozmenko,Basin Research(2010)22, 414-438

Autor: Avihu Burg, Yehoshua Kolodny, Amihai Sneh

Publikováno v: Basin Research. 25:112-114

The paper by Sokol et al. (2010) deals with the “Mottled Zone” (MZ, or Hatrurim Formation) rocks exposed in Israel and Jordan. These rocks have been extensively studied by British (Wyllie et al., 1923; Lees, 1928; Milodowski et al., 1992), Israel

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3692cea8f08b2c892db29d1ac02a2ab7
https://doi.org/10.1111/bre.12009

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Akademický článek

Xenocrysts and megacrysts of alkaline olivine-basalt-basanite-nephelinite association Makhtesh Ramon (Israel): interaction with carrier magmas and crystallographic transformations

Autor: Z. Yudalevich, Ye. Vapnik

Publikováno v: Литосфера, Vol 18, Iss 5A, Pp 57-77 (2020)

The article considers xenocrysts and megacrysts hosted in the rocks of Early Cretaceous olivine-basalt-basanite-nephelinite association that outcropped in the erosion crater of Makhtesh Ramon (Natural Reserve of Mishmar ha-Nagev, Israel). This magmat

Externí odkaz: https://doaj.org/article/f963bbae56ab4cdea03e0ebd2e530fef

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Fluids in High-Pressure Granulites

Autor: Yu. M. Lebedeva, E. V. Savva, Ye. Vapnik, S. A. Bushmin, M. V. Ivanov

Publikováno v: Petrology. 28:17-46

Properties of fluids in high-pressure granulites were studied in HP granulites (~8.7–11 kbar, ~800–900°С) and syngranulite fluid infiltration-driven HP metasomatites (~11–9 kbar, ~920–850°С) from the Lapland granulite belt of the Fennosca

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1d8288ade990c557fcf669bc964509f9
https://doi.org/10.1134/s0869591120010026

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New minerals with a modular structure derived from hatrurite from the pyrometamorphic rocks. Part III. Gazeevite, BaCa6(SiO4)2(SO4)2O, from Israel and the Palestine Autonomy, South Levant, and from South Ossetia, Greater Caucasus

Autor: Piotr Dzierżanowski, Mateusz Dulski, E. V. Galuskin, A. G. Gurbanov, Frank Gfeller, Joachim Kusz, Ye. Vapnik, Irina O. Galuskina, M. Gardocki, Arkadiusz Krzątała, Thomas Armbruster

Publikováno v: Mineralogical Magazine. 81:499-513

The new mineral gazeevite, BaCa6(SiO4)2(SO4)2O (R3m,a= 7.1540(1),c= 25.1242(5) Å,V= 1113.58(3) Å3,Z= 3), was found in an altered xenolith in rhyodacites ofthe Shadil-Khokh volcano, Southern Ossetia and at three localities in larnite pyrometamorphic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8a81a78cf392de447929b1ed41e499f0
https://doi.org/10.1180/minmag.2016.080.105

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Composite dikes in four successive granitoid suites from Transbaikalia, Russia: The effect of silicic and mafic magma interaction on the chemical features of granitoids

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

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The role of mantle and the ancient continental crust in the generation of post-collisional high-K calc-alkaline and alkaline granites, with main reference to the Arabian-Nubian Shield

Autor: M. Eyal, Ye. Vapnik, B.A. Litvinovsky, Yehuda Eyal

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

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New minerals with a modular structure derived from hatrurite from the pyrometamorphic Hatrurim Complex. Part II. Zadovite, BaCa6[(SiO4)(PO4)](PO4)2F and aradite, BaCa6[(SiO4)(VO4)](VO4)2F, from paralavas of the Hatrurim Basin, Negev Desert, Israel

Autor: Frank Gfeller, A. Pakhomova, Thomas Armbruster, Ye. Vapnik, Piotr Dzierżanowski, Irina O. Galuskina, Mikhail N. Murashko, Roman Włodyka, E. V. Galuskin

Publikováno v: Mineralogical Magazine. 79:1073-1087

Zadovite, BaCa6[(SiO4)(PO4)](PO4)2F (R3m, a = 7.0966(1) Å, c = 25.7284(3), V = 1122.13(3) Å3, Z = 3) and aradite, BaCa6[(SiO4)(VO4)] (VO4)2F (R3m, a = 7.1300(1), c = 26.2033(9) Å, V = 1153.63(6) Å3, Z = 3) are two new mineral species of a novel m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a2fbae65eafd57a4410341a130af9614
https://doi.org/10.1180/minmag.2015.079.5.04

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