Углеводороды Из Вулканического Района. Нефтепроявления В Кальдере Вулкана Узон На Камчатке

Галимов, Э. М.; Севастьянов, В. С.; Карпов, Г. А.; Камалеева, А. И.; Кузнецова, О. В.; Коноплева, И. В.; Власова, Л. Н.

doi:10.7868/s0016752515120043

Cited by 4 publications

(1 citation statement)

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“…Выделения углеводородов от -29.91 до -31.24‰. Более подробные данные об этой ча-сти исследования приведены в [6]. Обращает на себя внимание сходство изотопного состава мик-роалмазов и вулканического метана.…”

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Микрокристаллические Алмазы В Океанической Литосфере И Их Возможная Природа

Галимов¹,

Севастьянов²,

Карпов³

et al. 2016

Докл. РАН

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Микрокристаллические Алмазы В Океанической Литосфере И Их Возможная Природа

Галимов¹,

Севастьянов²,

Карпов³

et al. 2016

Докл. РАН

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Features of deep structure of the Uzon volcano caldera in Kamchatka and the explosive funnel in Yamal

Yakymchuk¹,

Корчагін²

2020

Dopov. Nac. akad. nauk Ukr.

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The results of a reconnaissance survey of local zones within the oil site of the Uzon volcano, Bogachevskoye oil field, and site of the explosive crater in Yamal are presented. Experimental studies using the direct-prospecting technology of a frequency-resonance processing and interpretation of satellite images and photographs are carried out to study the features of the deep structures of the survey areas. The results of instrumental measurements indicate that all survey sites are located above volcanoes of sedimentary rocks, within which the synthesis of oil, condensate and gas is almost always carried out at the 57 km border. In the contours of HC-generating volcanoes, there are deep channels through which oil, condensate, and gas migrate to the upper horizons of the cross-section and can replenish the already formed deposits in HC fields. In the absence of reliable seals over such channels, oil, condensate, and gas can migrate to the surface, and gas further enters the atmosphere. Measurements within a relatively large area around the Uzon volcano confirmed the presence of all previously identified types of volcanoes. These are volcanoes filled with: 1) salt; 2) sedimentary rocks of 1-6 groups; 3) limestones; 4) dolomites; 5) marls; 6) siliceous rocks; 7) granites; 8) basalts; 9) ultramafic rocks; 10) kimberlites. Additional evidence obtained by instrumental measurements in favor of the deep (abiogenic) genesis of oil, condensate, and gas is of fundamental importance. Numerous facts of fixing the signals from oil, condensate, and gas at the boundary of their synthesis 57 km within the survey areas and in other regions of the world allow us to state that abiogenic methane is migrating into Earth’s atmosphere in colossal volumes! Local zones of the gas migration into the atmosphere can serve as indicators of the activity of volcanoes in which hydrocarbons are synthesized. In these cases, drilling wells in the areas of the location of deep channels for the migration of abiogenic hydrocarbons to the upper horizons of the cross-section may be associated with great risks — with emergency situations during the drilling.

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Geochemical Significance of Bicyclic Sesquiterpanes in Hydrothermal Oil of the Uzon Volcano Caldera (Kamchatka)

Konopleva,

Sevastianov

2023

Geohimiâ

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The composition and relative content of C14-C16 bicyclic sesquiterpanes in oil seeps from thermal springs of the Uzon Caldera have been studied by GC-MS technique. It is shown that C16 homodrimanes prevail in oil composition, C15 drimane content is insignificant, and C14 nordrimanes are present in trace amounts. Homodrimane with biological configuration 8α(H) was detected. Bicyclic sesquiterpanes of Uzon oil are probably its derivatives. It has been revealed that the relative content of C15 drimanes increases with the oil maturity. A sesquiterpane maturity index, which has not been used previously in organic geochemistry, is proposed.

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Углеводороды Из Вулканического Района. Нефтепроявления В Кальдере Вулкана Узон На Камчатке

Cited by 4 publications

References 0 publications

Микрокристаллические Алмазы В Океанической Литосфере И Их Возможная Природа

Микрокристаллические Алмазы В Океанической Литосфере И Их Возможная Природа

Features of deep structure of the Uzon volcano caldera in Kamchatka and the explosive funnel in Yamal

Geochemical Significance of Bicyclic Sesquiterpanes in Hydrothermal Oil of the Uzon Volcano Caldera (Kamchatka)

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