1.0Сайт журналу «Геоінформатика»http://www.geology.com.ua/enАдміністраторhttp://www.geology.com.ua/en/blog/author/andriy/rich600338<blockquote class="wp-embedded-content" data-secret="LnQ4zRAruW"><a href="http://www.geology.com.ua/en/7486-2/"></a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="http://www.geology.com.ua/en/7486-2/embed/#?secret=LnQ4zRAruW" width="600" height="338" title="“” — Сайт журналу «Геоінформатика»" data-secret="LnQ4zRAruW" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script type="text/javascript"> /* <![CDATA[ */ /*! This file is auto-generated */ !function(d,l){"use strict";l.querySelector&&d.addEventListener&&"undefined"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!/[^a-zA-Z0-9]/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret="'+t.secret+'"]'),o=l.querySelectorAll('blockquote[data-secret="'+t.secret+'"]'),c=new RegExp("^https?:$","i"),i=0;i<o.length;i++)o[i].style.display="none";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute("style"),"height"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):"link"===t.message&&(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener("message",d.wp.receiveEmbedMessage,!1),l.addEventListener("DOMContentLoaded",function(){for(var e,t,s=l.querySelectorAll("iframe.wp-embedded-content"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute("data-secret"))||(t=Math.random().toString(36).substring(2,12),e.src+="#?secret="+t,e.setAttribute("data-secret",t)),e.contentWindow.postMessage({message:"ready",secret:t},"*")},!1)))}(window,document); //# sourceURL=http://www.geology.com.ua/wp-includes/js/wp-embed.min.js /* ]]> */ </script> Geoinformatika 2018; 3(67) : 25-35 УДК 553.24;553.21/24;553.9 OCEANIC WATER AS A BASIC SOURCE OF GENESIS OF HYDROCARBONS, GEOFLUIDS, DIAMOND STRUCTURES, MUD VOLCANOES, AND DEPOSITS OF NOBLE METALS IN VARIOUS REGIONS OF THE EARTH Harutyunyan A.V. National Polytechnic University of Armenia, 0009, Yerevan, Teryan Str. 105; e-mail: avhk@seua.am Purpose. Infiltration of oceanic water through a volcanogenic layer creates the 3-d serpentinized layer of the oceanic crust, where, due to serpentinization, horizontally bursting pressures appear, which makes the oceanic crust collide with the continental under-shelf and slope. This process leads to dehydration of the serpentinized rocks and the appearance of hydrogen, carbohydrates, geo-fluids, etc.  To illustrate, genesis of a gigantic deposit, the Mexican gulf, is given. Design /methodology /approach. As a result of tectonic processes, oceanic crust relics were preserved at various depths of the continental crust scattered across the Earth. Rise of pressure and temperature, oceanic crust relics of serpentinized rocks also get dehydrated, leading to the appearance of hydrogen, carbohydrates, geo-fluids, etc. Genesis of gigantic deposits in the Pre-Caspian depression and Western Siberia is given as illustration. Findings. The paper also deals with genesis of mud volcanoes, diamond-bearing structures, and noble metals deposits. Practical implications /conclusions. It is possible to conclude that the main source of hydrogen genesis is oceanic water, which reacts with the upper mantle ultrabasits, creating serpentinized rocks. Later, under certain thermobaric conditions, it goes out of the rocks both in the oceanic and continental crusts, thus generating hydrogen, which is the basic element of carbohydrates. Keywords: serpantinized rocks, hydrogen, dehydration, genesis of carbohydrates, geo-fluids, diamond-bearing structures, noble metals, mud volcanoes.   The full text of papers   References Aslanyan A.T., Arutyunyan A.V. Stanovleniye sredinno-okeanicheskikh khrebtov v svete eksperimental’nykh issledovaniy pri vysokikh termobaricheskikh parametrakh. Izv. AN Arm. SSR, Nauki o Zemle, 2, 1988. P 6. Aslanyan A.T., Arutyunyan A.V. K voprosu o glubinnom stroenii ofiolitovyh zon Malogo Kavkaza. Izvestya. AN ArmSSR. Nauki o Zemle. 1988. N 5. P. 54—58. Arutyunyan A.V. O mekhanizme formirovaniya uglevodorodnykh komponentov v svyazi s evolyutsiyey zemnoy kory Malogo Kavkaza. Geologiya i razvedka. Izvestiya vuzov Rossiyskoy Federatsii. 1999. N 1. P. 141—146. https://docs.google.com/document/d/1INywnASQE3viVOoi5RKelicovO9qZMk0sHq3XRnpEmE/edit usp=sharinghttps://docs.google.com/document/d/1INywnASQE3viVOoi5RKelicovO9qZMk0sHq3XRnpEmE/edit?usp=sharing Arutyunyan A. V. Zemnaya kora Malogo Kavkaza, ofiolity, vulkanizm, neftegazonosnost’, seysmichnost’. Vestnik ONZ RAN. 2010. N 2. NZ6006. doi: 10.2205/2010NZ000024, 2010.http://onznews.wdcb.ru/publications/v02/2010NZ000024.pdf Arutyunyan A. V. Geoflyuidy, neft’, voda, kimberlity i almaz: genezis i akku¬mulyatsiya v zemnoy kore (na primere Malogo Kavkaza). http://journal.deepoil.ru/images/stories/docs/DO-1-3-2013/5_Arutunayn_1-3-2013.pdf Arutyunyan A.V. Ot serpentinizatsii do deserpentinizatsii ili ot okeanicheskoy kory do gornykh khrebtov i drevnikh platform. Tezisi, 3-ye Kudryavtsevskiye chteniya. Vserossiyskaya konferentsiya po glubinnomu genezisu nefti. Moskva, TSGE,2014.https://drive.google.com/open?id=0B3iWda0UzHQuTW5OSDJaaUxCOHc Arutyunyan A.V. Degidratatsiya porod kak istochnik genezisa geoflyuidov, uglevodorodov, almazonosnykh struktur, gryazevykh vulkanov i mestorozhdeniy blagorodnykh metallov v razlichnykh regionakh Zemli. NEDROPOL’ZOVANIYe — 21 vek. 2017. N 1. https://drive.google.com/open?id=0B3iWda0UzHQuU2gwa21Qd2MyTjQ Gavrilov V.P. Vozmozhnyye mekhanizmy yestestvennogo vospolneniya zapasov nef¬tya¬nykh i gazovykh mestorozhdeniyakh. Geologiya nefti i gaza. 2008. N 1. Garagash I.A. Formirovanie zon proniknovenia glubinnoi nefti v verhnie sloi Zemli «3-e Kudryavtsevskiye chteniya»: tezisy docladov. Moscow, 2016. Genshaft U.S., Uhanyan A.K. Ksenolity I megacristally v lavah Gegamskogo nagor’ya (Armenia). Phyziko-chemicheskye issledovaniya productov glunnogo magmatizma. Moscow: Nauka, 1982. Dmitriyevskiy A.N., Balanyuk I.Ye., Sorokhtin O.G., Dongaryan L.SH. Serpentinity okeanicheskoy kory – istochnik obrazovaniya uglevodorodov. Geologiya nefti i gaza. 2002. N 3. Lobkovskiy L.I. Geodinamika zon spredinga, subduktsii i dvukhyarusnaya tektonika plit. Moscow: Nauka, 1988. Marakushev A.A., Marakushev C.A. Endogennoe obrazovanie assoiacii uglevodorodnuh s solyanuh zalejei. Glubinnaya neft’. 2013. Vol. 1, N 1. Rybalka A.V., Kashubina T.V., Petrov G.A.,Kashubin S.N. Sredneural’skiy Transekt: Novyye dannyye po glubinnomu stroyeniyu Urala. Modeli zemnoy kory i verkhney mantii po rezul’tatam glubinnogo seysmoprofilirovaniya. Materialy Mezhdunarodnogo nauchno-prakticheskogo seminara 18—20 sentyabrya 2007 g. Rybalka A.V., Petrov G.A., Kashubina T.V., Kulikov V.A., Yegorkin A.V., Dushin V.A., Kashubin S.N. Glubinnoye stroyeniye Urala po dannym polyarno-uralskogo transekta. Regional’naya geologiya i metallogeniya. 2011. N 48. Yudin V.V., Remizov D.N. Sbalansirovannaya geodinamicheskaya model’ po profilyu Polyarnoural’skiy transekt. V kn.: Geologiya i mineral’nyye resursy Yevropeyskogo severo-vostoka Rossii. Materialy XVI Geologicheskogo s’yezda Respubliki Komi 15—17 aprelya 2014 g. Syktyvkar, 2014. Shnyukov Ye.F., Panin N.S., Dinu K., Maslakov N.A., Paryshev A.A. Gryazevoy vulkanizm v Rumynii.Geologiya i poleznyye iskopayemyye mirovogo okeana. N 2, 2008. Shnyukov Ye.F., Sokol E.V., Nigmatulina Ye.N., Ivanchenko V.V.,Yushin A.A. Zoloto v gryazevykh vulkanakh Kerchenskogo poluostrova kak pokazatel’ glubinnosti gryazevulkanicheskikh flyuidov. Geologiya i poleznyye iskopayemyye mirovogo okeana. N 4, 2013. https://drive.google.com/open?id=0B3iWda0UzHQualZ2WmxQTE1XMHc Stampfli, G. M. Tethyan oceans. Tectonics and Magmatism in Turkey and the Surrounding Area. Published by The Geological Society. London. 2000. N 173.