Çeleken nebit ýatagynyň geologik gurluşy gyzylreňkli toplumyň, akçagyl, apşeron, postpliosen döwürleriniň çökündilerinden durýar. Galyndylar, esasan, gaýtalanýan toýun, çäge, alewrit dag jynslaryny öz içine alýar. Meýdança Günbatar Aligul, Dagajyk we Gündogar böleklerden ybarat.
\r\n\r\nNebit ýataklary, esasan, gyzylreňkli çökündiler toplumynda ýerleşýär, kesimde 11 sany önümli gatlak seljerilen. Uglewodorod birleşmeleriniň çäkleri çuňluk boýunça ulalýar we önümli gatlaklar meýdançanyň demirgazyk ganatynda ýerleşýär.
\r\n\r\nMeýdançanyň çäginde günbatardan gündogar ugur boýunça Günbatar Porsyköl, Gülgün Porsyköl we Dagajyk wulkanlary ýerleşýär. Wulkan önümleriniň häsiýetleri köp ýyllaryň dowamynda nebit we gaz ýataklarynyň gidrogeologiýa, gidrohimiýa hem-de nebitiň, gazyň we dag jynslarynyň geohimiýa laboratoriýalarynda öwrenilip gelinýär.
\r\n\r\nPliosen çökündileriniň tebigy gazlary erkin, nebitde we suwda erän gazlardyr. Olaryň esasyny metan, kümürturşy, azot gazlary düzýär. Gazlar kükürtsizligi bilen häsiýetlendirilýär. Suwuň, nebitiň çykymlary Günbatar Porsyköl, Gülgün Porsyköl wulkanlarynda gaz bilen bilelikde ýüze çykýar. Çeleken käniniň Dagajyk böleginde 1,9 kilometr çuňluga çenli alnan nebitler 1,5 göterim parafin saklaýar. Çuňluk artdygyça, nebitiň düzümindäki parafiniň mukdary artýar. Günbatar Porsyköl we Gülgün Porsyköl wulkanlarynyň nusgalyk nebitiniň dykyzlygy 0,969 — 0,994 aralygynda üýtgeýär.
\r\n\r\nLäbik wulkanlarynyň duzlulyk derejesi ortaça 25 — 300 g/1 çäklerde üýtgeýär we gidrokarbonatnatrili, sulfatnatrili, hlorkalsili görnüşlerden durýar. Olaryň düzüminde ýod, brom, bor mikroelementleri saklanýar. Wulkan suwlarynyň nusgasy yzygiderli öwrenilip gelinýär.
\r\n\r\nGünbatar Porsyköl läbik wulkanlarynyň suwlary 50 g/1 duzlulygy bilen häsiýetlendirilýär we gidrokarbonatnatrili, sulfatnatrili, hlormagnili görnüşe degişli. Suwda sulfatlaryň 1500 mg/1, bikarbonatlaryň 4000 mg/l çenli mukdary saklanýar.
\r\n\r\nGülgün Porsyköl läbik wulkanynyň suwlary gidrohimiki aýratynlyklary boýunça Günbatar Porsyköl wulkanynyň suwlaryna meňzeş, duzlulygy 25 — 30 g/1 barabar.
\r\n\r\nSoňky ýyllarda Çeleken meýdançasynyň çäginde grifon wulkanlarynyň emele gelmegi ýygylaşdy. Bu tebigy hadysalar ulanylýan guýularyň işleýiş düzgüniniň çylşyrymlaşmagyny ýüze çykarýar. 2015-nji ýylda emele gelen täze grifon wulkanynyň önümli gatlak şertlerine täsirini seljermek üçin «Galkynyşnebit» nebitgaz çykaryş müdirligi «Nebitgazylmytaslama» institutyna buýurma bilen ýüz tutdy. Meseläni çözmek üçin täze wulkanyň kraterinden nebit we suw nusgalary alyndy we barlaghana şertlerinde öwrenildi. Barlanan nusgalaryň haýsy önümli gatlaklara degişlidigi, wulkanyň köküniň çuňlugy anyklandy. Bu ugurda önümçilik hünärmenleri bilen bilelikde gözegçilik işleri alnyp barylýar. Gündogar Dagajyk wulkanynyň suwlary hlorkalsiý görnüşli, duzlulygy 150 — 160 g/1 barabardyr.
\r\n\r\nGünbatar Porsyköl we Gülgün Porsyköl läbik wulkanlarynyň kökleri has gadymy, mezozoý çökündilerinde ýerleşýär. Hlorkalsiý esasly dürli erginleriň gidrohimiki aýratynlyklary we ýokary duzly suwlaryň döreýşi basseýniň sedimentasiýa şertleri bilen üznüksiz baglanyşyklydyr.
\r\n\r\nLäbik wulkanlary nebitgaz ýataklarynyň emele gelmeginde, saklanmagynda, üýtgemelerinde kesgitleýji orny eýeleýär. Olar çökündileriniň nebitgazlylygynyň esasy görkezijisi bolup galýar. Geologik gurluş, nebitgazlylyk we wulkançylyk ýeke-täk genetiki bitewüligi düzýär.
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Çeşme: «Nebit-gaz» gazeti
"},"en":{"title":"Mud volcanoes of Cheleken reveal the secrets of Turkmenistan's oil deposits","description":"The geological structure of the Çeleken oil field consists of deposits of the red-bed series, Akchagylian, Apsheronian and post-Pliocene periods. The deposits mainly include alternating clay, sandy and siltstone rocks. The area consists of the Western Aligul, Dagajyk and Eastern sections.
\r\n\r\nOil deposits are mainly located in the red-bed deposit complex; 11 productive formations have been analyzed in the section. The boundaries of hydrocarbon compounds increase with depth, and the productive formations are located on the northern flank of the area.
\r\n\r\nWithin the area, running from west to east, are the Western Porsyköl, Pink (Gülgün) Porsyköl and Dagajyk volcanoes. The properties of volcanic products have been studied for many years in the laboratories of hydrogeology, hydrochemistry of oil and gas fields, as well as geochemistry of oil, gas and rocks.
\r\n\r\nNatural gases of the Pliocene deposits are free gases, as well as gases dissolved in oil and water. Their basis consists of methane, carbon dioxide and nitrogen. The gases are characterized by the absence of sulfur. Water and oil seeps at the Western Porsyköl and Pink (Gülgün) Porsyköl volcanoes occur together with gas. In the Dagajyk section of the Cheleken oil field, oil obtained from depths of up to 1.9 kilometers contains 1.5 percent paraffin. With increasing depth, the paraffin content in the oil increases. The density of oil samples from the Western Porsyköl and Pink (Gülgün) Porsyköl volcanoes ranges between 0.969 and 0.994.
\r\n\r\nThe mineralization level [salinity] of the mud volcanoes averages between 25 and 300 g/l and consists of sodium bicarbonate, sodium sulfate and calcium chloride types. They contain trace elements of iodine, bromine and boron. Samples of volcanic waters are studied on a regular basis.
\r\n\r\nThe waters of the Western Porsyköl mud volcanoes are characterized by a mineralization of 50 g/l and belong to the sodium bicarbonate, sodium sulfate and magnesium chloride type. The water contains up to 1,500 mg/l of sulfates and up to 4,000 mg/l of bicarbonates.
\r\n\r\nThe waters of the Pink (Gülgün) Porsyköl mud volcano are similar in hydrochemical characteristics to the waters of the Western Porsykel volcano; their mineralization equals 25–30 g/l.
\r\n\r\nIn recent years, the formation of gryphon volcanoes has increased within the Çeleken area. These natural phenomena cause complications in the operating conditions of the wells in use. To analyze the impact of a new gryphon formed in 2015 on the conditions of the productive formation, «Galkynyşnebit» oil and gas production department placed an order with a «Nebitgazylmytaslama» institute. To resolve the problem, oil and water samples were taken from the crater of the new volcano and studied under laboratory conditions. It was determined which productive formations the studied samples belonged to, as well as the depth of the volcano's root. Monitoring work in this direction is being carried out jointly with production specialists. The waters of the Eastern Dagajyk volcano are of the calcium chloride type, with a mineralization of 150–160 g/l.
\r\n\r\nThe roots of the Western Porsyköl and Pink (Gülgün) Porsyköl mud volcanoes are more ancient; they are located in Mesozoic deposits. The hydrochemical characteristics of various calcium chloride-based solutions and the formation of highly mineralized waters are continuously related to the sedimentation conditions of the basin.
\r\n\r\nMud volcanoes play a determining role in the formation, preservation and alteration of oil and gas deposits. They remain the primary indicator of the petroleum potential of deposits. The geological structure, petroleum potential and volcanism form a single genetic unity.
\r\n\r\n\r\n\r\n
\r\n\r\n
Source: «Nebit-gaz» newspaper
\r\n\r\n"},"ru":{"title":"Грязевые вулканы Челекена раскрывают секреты нефтяных залежей Туркменистана","description":"
Геологическое строение нефтяного месторождения Челекен состоит из отложений красноцветной толщи, акчагыльского, апшеронского и постплиоценового периодов. Отложения в основном включают в себя чередующиеся глинистые, песчаные и алевритовые горные породы. Площадь состоит из Западного Алигула, Дагаджика и Восточной частей.
\r\n\r\nНефтяные залежи в основном располагаются в комплексе красноцветных отложений, в разрезе проанализировано 11 продуктивных пластов. Границы углеводородных соединений увеличиваются по глубине, и продуктивные пласты располагаются на северном крыле площади.
\r\n\r\nВ пределах площади в направлении с запада на восток расположены вулканы Западный Порсыкёль, Розовый (Гюльгюн) Порсыкёль и Дагаджик. Свойства вулканических продуктов на протяжении многих лет изучаются в лабораториях гидрогеологии, гидрохимии нефтегазовых месторождений, а также геохимии нефти, газа и горных пород.
\r\n\r\nПриродные газы плиоценовых отложений — это свободные, а также растворенные в нефти и воде газы. Их основу составляют метан, углекислый газ и азот. Газы характеризуются отсутствием серы. Выходы воды и нефти на вулканах Западный Порсыкёль и Розовый (Гюльгюн) Порсыкёль проявляются совместно с газом. В части Дагаджик Челекенского месторождения нефти, полученные с глубины до 1,9 километра, содержат 1,5 процента парафина. С увеличением глубины количество парафина в составе нефти возрастает. Плотность образцов нефти вулканов Западный Порсыкёль и Розовый (Гюльгюн) Порсыкёль варьируется в пределах 0,969 — 0,994.
\r\n\r\nУровень минерализации [солености] грязевых вулканов в среднем колеблется в пределах 25 — 300 г/л и состоит из гидрокарбонатно-натриевого, сульфатно-натриевого и хлоркальциевого типов. В их составе содержатся микроэлементы йод, бром, бор. Образцы вулканических вод изучаются на регулярной основе.
\r\n\r\nВоды грязевых вулканов Западного Порсыкёля характеризуются минерализацией 50 г/л и относятся к гидрокарбонатно-натриевому, сульфатно-натриевому и хлормагниевому типу. В воде содержится сульфатов до 1500 мг/л, бикарбонатов до 4000 мг/л.
\r\n\r\nВоды грязевого вулкана Розовый (Гюльгюн) Порсыкёль по гидрохимическим особенностям похожи на воды вулкана Западный Порсыкёль, их минерализация равна 25 — 30 g/l [25 — 30 г/л].
\r\n\r\nВ последние годы в пределах Челекенской площади участилось образование грифонных вулканов. Эти природные явления вызывают усложнение режима работы эксплуатируемых скважин. Для анализа влияния нового грифона, образовавшегося в 2015 году, на условия продуктивного пласта нефтегазодобывающее управление «Галкынышнебит» обратилось с заказом в институт «Небитгазылмытаслама». Для решения проблемы из кратера нового вулкана были взяты пробы нефти и воды и изучены в лабораторных условиях. Было определено, к каким продуктивным пластам относятся исследованные образцы, а также глубина корня вулкана. В этом направлении совместно со специалистами производства ведутся работы по мониторингу. Воды вулкана Восточный Дагаджик хлоркальциевого типа, их минерализация равна 150 — 160 г/л.
\r\n\r\nКорни грязевых вулканов Западный Порсыкёль и Розовый (Гюльгюн) Порсыкёль более древние, они располагаются в мезозойских отложениях. Гидрохимические особенности различных растворов на хлоркальциевой основе и формирование высокоминерализованных вод непрерывно связаны с седиментационными условиями бассейна.
\r\n\r\nГрязевые вулканы занимают определяющую роль в формировании, сохранении и изменениях нефтегазовых залежей. Они остаются главным показателем нефтегазоносности отложений. Геологическое строение, нефтегазоносность и вулканизм составляют единую генетическую целостность.
\r\n\r\n\r\n\r\n
Источник: газета «Небит-газ»
"}},"title":"Mud volcanoes of Cheleken reveal the secrets of Turkmenistan's oil deposits","description":"The geological structure of the Çeleken oil field consists of deposits of the red-bed series, Akchagylian, Apsheronian and post-Pliocene periods. The deposits mainly include alternating clay, sandy and siltstone rocks. The area consists of the Western Aligul, Dagajyk and Eastern sections.
\r\n\r\nOil deposits are mainly located in the red-bed deposit complex; 11 productive formations have been analyzed in the section. The boundaries of hydrocarbon compounds increase with depth, and the productive formations are located on the northern flank of the area.
\r\n\r\nWithin the area, running from west to east, are the Western Porsyköl, Pink (Gülgün) Porsyköl and Dagajyk volcanoes. The properties of volcanic products have been studied for many years in the laboratories of hydrogeology, hydrochemistry of oil and gas fields, as well as geochemistry of oil, gas and rocks.
\r\n\r\nNatural gases of the Pliocene deposits are free gases, as well as gases dissolved in oil and water. Their basis consists of methane, carbon dioxide and nitrogen. The gases are characterized by the absence of sulfur. Water and oil seeps at the Western Porsyköl and Pink (Gülgün) Porsyköl volcanoes occur together with gas. In the Dagajyk section of the Cheleken oil field, oil obtained from depths of up to 1.9 kilometers contains 1.5 percent paraffin. With increasing depth, the paraffin content in the oil increases. The density of oil samples from the Western Porsyköl and Pink (Gülgün) Porsyköl volcanoes ranges between 0.969 and 0.994.
\r\n\r\nThe mineralization level [salinity] of the mud volcanoes averages between 25 and 300 g/l and consists of sodium bicarbonate, sodium sulfate and calcium chloride types. They contain trace elements of iodine, bromine and boron. Samples of volcanic waters are studied on a regular basis.
\r\n\r\nThe waters of the Western Porsyköl mud volcanoes are characterized by a mineralization of 50 g/l and belong to the sodium bicarbonate, sodium sulfate and magnesium chloride type. The water contains up to 1,500 mg/l of sulfates and up to 4,000 mg/l of bicarbonates.
\r\n\r\nThe waters of the Pink (Gülgün) Porsyköl mud volcano are similar in hydrochemical characteristics to the waters of the Western Porsykel volcano; their mineralization equals 25–30 g/l.
\r\n\r\nIn recent years, the formation of gryphon volcanoes has increased within the Çeleken area. These natural phenomena cause complications in the operating conditions of the wells in use. To analyze the impact of a new gryphon formed in 2015 on the conditions of the productive formation, «Galkynyşnebit» oil and gas production department placed an order with a «Nebitgazylmytaslama» institute. To resolve the problem, oil and water samples were taken from the crater of the new volcano and studied under laboratory conditions. It was determined which productive formations the studied samples belonged to, as well as the depth of the volcano's root. Monitoring work in this direction is being carried out jointly with production specialists. The waters of the Eastern Dagajyk volcano are of the calcium chloride type, with a mineralization of 150–160 g/l.
\r\n\r\nThe roots of the Western Porsyköl and Pink (Gülgün) Porsyköl mud volcanoes are more ancient; they are located in Mesozoic deposits. The hydrochemical characteristics of various calcium chloride-based solutions and the formation of highly mineralized waters are continuously related to the sedimentation conditions of the basin.
\r\n\r\nMud volcanoes play a determining role in the formation, preservation and alteration of oil and gas deposits. They remain the primary indicator of the petroleum potential of deposits. The geological structure, petroleum potential and volcanism form a single genetic unity.
\r\n\r\n\r\n\r\n
\r\n\r\n
Source: «Nebit-gaz» newspaper
\r\n\r\n","time_create":"2026-06-16T12:46:39.617546+05:00","time_update":"2026-06-16T12:47:08.319100+05:00","is_active":true,"news_date":"2026-06-16T12:46:22+05:00","image":"https://tmgeology.gov.tm/media/posts/19gryavulkbuni006.jpg","video":null,"category":1}