New data on the Geochemistry of Gases in the Potash Deposits
The composition of the gas phase of salt rocks from a number of potash deposits located in Europe (Verkhnekamskoe, Starobinskoe) and Asia (Tubegatanskoe, Zhylyanskoe Satimolinskoe) was studied. It allowed dividing them into two groups. In Asian deposits, only authigenic dry gases were formed by diag...
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| Format: | Article |
| Language: | English |
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Perm Sate National Research University
2014-12-01
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| Series: | Vestnik Permskogo Universiteta: Seriâ Geologiâ |
| Subjects: | |
| Online Access: | http://geology-vestnik.psu.ru/index.php/geology/article/view/49 |
| _version_ | 1811270219289591808 |
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| author | I. I. Chaykovskiy O. V. Ivanov |
| author_facet | I. I. Chaykovskiy O. V. Ivanov |
| author_sort | I. I. Chaykovskiy |
| collection | DOAJ |
| description | The composition of the gas phase of salt rocks from a number of potash deposits located in Europe (Verkhnekamskoe, Starobinskoe) and Asia (Tubegatanskoe, Zhylyanskoe Satimolinskoe) was studied. It allowed dividing them into two groups. In Asian deposits, only authigenic dry gases were formed by diagenetic decomposition of organic matter. Structural exposure of these deposits led to the oxidation of methane and hydrogen and enrichment by carbon dioxide. European deposits were not structurally exposed to the oxidation process, but were exposed during salt rock formation. They experienced influx of heavy hydrocarbons from the underlying strata. The history of the formation of gas regime at the Verkhnekamskoe potash deposit could be divided into three stages. First stage may be characterized by a syngenetic capture of deep gases and authigenic organic matter converted during diagenesis to methane, which percentage gradually increases with an increase of the thickness of impermeable salt strata. Then the deep gases invaded the salt formation during sedimentation of the upper carnallite layers and top salt rock. Third stage was associated with folding processes accompanied by a mobilization of fluids scattered in the gas-fluid inclusions, and with probable influx of heavy hydrocarbons and carbon dioxide resulted in formation of the secondary salt zones. Replacement of carnallite layers leads to the release of isomorphous ammonium ion and formation of a hydrogen. |
| first_indexed | 2024-04-12T21:56:57Z |
| format | Article |
| id | doaj.art-0b16f4400690433fb4b48b30bf962fae |
| institution | Directory Open Access Journal |
| issn | 1994-3601 2313-4798 |
| language | English |
| last_indexed | 2024-04-12T21:56:57Z |
| publishDate | 2014-12-01 |
| publisher | Perm Sate National Research University |
| record_format | Article |
| series | Vestnik Permskogo Universiteta: Seriâ Geologiâ |
| spelling | doaj.art-0b16f4400690433fb4b48b30bf962fae2022-12-22T03:15:16ZengPerm Sate National Research UniversityVestnik Permskogo Universiteta: Seriâ Geologiâ1994-36012313-47982014-12-01425566510.17072/psu.geol.25.5645New data on the Geochemistry of Gases in the Potash DepositsI. I. Chaykovskiy0O. V. Ivanov1Горный институт УрО РАН, 614007, Пермь, ул. Сибирская 78аПермский национальный исследовательский политехнический университет, 614000, Пермь, Комсомольский пр., 29аThe composition of the gas phase of salt rocks from a number of potash deposits located in Europe (Verkhnekamskoe, Starobinskoe) and Asia (Tubegatanskoe, Zhylyanskoe Satimolinskoe) was studied. It allowed dividing them into two groups. In Asian deposits, only authigenic dry gases were formed by diagenetic decomposition of organic matter. Structural exposure of these deposits led to the oxidation of methane and hydrogen and enrichment by carbon dioxide. European deposits were not structurally exposed to the oxidation process, but were exposed during salt rock formation. They experienced influx of heavy hydrocarbons from the underlying strata. The history of the formation of gas regime at the Verkhnekamskoe potash deposit could be divided into three stages. First stage may be characterized by a syngenetic capture of deep gases and authigenic organic matter converted during diagenesis to methane, which percentage gradually increases with an increase of the thickness of impermeable salt strata. Then the deep gases invaded the salt formation during sedimentation of the upper carnallite layers and top salt rock. Third stage was associated with folding processes accompanied by a mobilization of fluids scattered in the gas-fluid inclusions, and with probable influx of heavy hydrocarbons and carbon dioxide resulted in formation of the secondary salt zones. Replacement of carnallite layers leads to the release of isomorphous ammonium ion and formation of a hydrogen.http://geology-vestnik.psu.ru/index.php/geology/article/view/49Верхнекамское месторождениесостав газовпервичные и вторичные соли |
| spellingShingle | I. I. Chaykovskiy O. V. Ivanov New data on the Geochemistry of Gases in the Potash Deposits Vestnik Permskogo Universiteta: Seriâ Geologiâ Верхнекамское месторождение состав газов первичные и вторичные соли |
| title | New data on the Geochemistry of Gases in the Potash Deposits |
| title_full | New data on the Geochemistry of Gases in the Potash Deposits |
| title_fullStr | New data on the Geochemistry of Gases in the Potash Deposits |
| title_full_unstemmed | New data on the Geochemistry of Gases in the Potash Deposits |
| title_short | New data on the Geochemistry of Gases in the Potash Deposits |
| title_sort | new data on the geochemistry of gases in the potash deposits |
| topic | Верхнекамское месторождение состав газов первичные и вторичные соли |
| url | http://geology-vestnik.psu.ru/index.php/geology/article/view/49 |
| work_keys_str_mv | AT iichaykovskiy newdataonthegeochemistryofgasesinthepotashdeposits AT ovivanov newdataonthegeochemistryofgasesinthepotashdeposits |