Recent tectonomagmatic reactivation of the Kolyuchino-Mechigmen zone of the Chukchi Peninsula from data on the composition of gases in hydrothermal springs
Thirty-three groups of thermal mineral springs in the Chukchi Peninsula are studied. The thermal fluids of the Kolyuchino-Mechigmen Zone (KMZ) show specific characteristics. The zone corresponds to recent depression with occurrences of basic volcanism and high seismicity. Characteristic features of...
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| Veröffentlicht in: | Geotectonics 2010-11, Vol.44 (6), p.529-540 |
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| creator | Polyak, B. G. Lavrushin, V. Yu Cheshko, A. L. Prasolov, E. M. Kamensky, I. L. |
| description | Thirty-three groups of thermal mineral springs in the Chukchi Peninsula are studied. The thermal fluids of the Kolyuchino-Mechigmen Zone (KMZ) show specific characteristics. The zone corresponds to recent depression with occurrences of basic volcanism and high seismicity. Characteristic features of the gases in the springs of the KMZ include the predominance of carbon dioxide, high percentage of mantle-derived helium, enrichment of CO
2
in
13
C, admixture of nonatmospheric nitrogen, excess in
40
Ar and
15
N relative to the atmosphere, maximal depletion of thermal water in deuterium and heavy oxygen isotope, and the highest estimates of deep temperature in reservoirs of hydrothermal fluid. All these features indicate the contemporary ascent of a mantle diapir that supplied helium enriched in
3
He and thermal energy to the crust, thus provoking thermal metamorphism of rocks and degradation of permafrost. |
| doi_str_mv | 10.1134/S0016852110060063 |
| format | Article |
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2
in
13
C, admixture of nonatmospheric nitrogen, excess in
40
Ar and
15
N relative to the atmosphere, maximal depletion of thermal water in deuterium and heavy oxygen isotope, and the highest estimates of deep temperature in reservoirs of hydrothermal fluid. All these features indicate the contemporary ascent of a mantle diapir that supplied helium enriched in
3
He and thermal energy to the crust, thus provoking thermal metamorphism of rocks and degradation of permafrost.</description><identifier>ISSN: 0016-8521</identifier><identifier>EISSN: 1556-1976</identifier><identifier>DOI: 10.1134/S0016852110060063</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Carbon dioxide ; Deuterium ; Diapirs ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geophysics ; Helium ; Magma ; Metamorphism ; Mineral springs ; Oxygen isotopes ; Permafrost ; Plate tectonics ; Soil degradation ; Structural Geology ; Thermal energy ; Thermal water ; Thermodynamics</subject><ispartof>Geotectonics, 2010-11, Vol.44 (6), p.529-540</ispartof><rights>Pleiades Publishing, Ltd. 2010</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a338t-fa22df02d6371ec68d86f868b68a1dd67673249f264bb72068f23b62736610ad3</citedby><cites>FETCH-LOGICAL-a338t-fa22df02d6371ec68d86f868b68a1dd67673249f264bb72068f23b62736610ad3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0016852110060063$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0016852110060063$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Polyak, B. G.</creatorcontrib><creatorcontrib>Lavrushin, V. Yu</creatorcontrib><creatorcontrib>Cheshko, A. L.</creatorcontrib><creatorcontrib>Prasolov, E. M.</creatorcontrib><creatorcontrib>Kamensky, I. L.</creatorcontrib><title>Recent tectonomagmatic reactivation of the Kolyuchino-Mechigmen zone of the Chukchi Peninsula from data on the composition of gases in hydrothermal springs</title><title>Geotectonics</title><addtitle>Geotecton</addtitle><description>Thirty-three groups of thermal mineral springs in the Chukchi Peninsula are studied. The thermal fluids of the Kolyuchino-Mechigmen Zone (KMZ) show specific characteristics. The zone corresponds to recent depression with occurrences of basic volcanism and high seismicity. Characteristic features of the gases in the springs of the KMZ include the predominance of carbon dioxide, high percentage of mantle-derived helium, enrichment of CO
2
in
13
C, admixture of nonatmospheric nitrogen, excess in
40
Ar and
15
N relative to the atmosphere, maximal depletion of thermal water in deuterium and heavy oxygen isotope, and the highest estimates of deep temperature in reservoirs of hydrothermal fluid. All these features indicate the contemporary ascent of a mantle diapir that supplied helium enriched in
3
He and thermal energy to the crust, thus provoking thermal metamorphism of rocks and degradation of permafrost.</description><subject>Carbon dioxide</subject><subject>Deuterium</subject><subject>Diapirs</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geophysics</subject><subject>Helium</subject><subject>Magma</subject><subject>Metamorphism</subject><subject>Mineral springs</subject><subject>Oxygen isotopes</subject><subject>Permafrost</subject><subject>Plate tectonics</subject><subject>Soil degradation</subject><subject>Structural Geology</subject><subject>Thermal energy</subject><subject>Thermal water</subject><subject>Thermodynamics</subject><issn>0016-8521</issn><issn>1556-1976</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kctKxDAUhoMoOI4-gLvgvppLJ02XMnjDEcXLuqRN0nZskzFJhfFVfFlTqrgQIXBC_u__cw4HgGOMTjGm6dkTQpjxBcEYIRYP3QEzvFiwBOcZ2wWzUU5GfR8ceL9GiKKozsDno6qUCTCoKlhje1H3IrQVdEpUoX2Pd2ug1TA0Ct7abjtUTWtscqdirXtl4Ic16gdYNsNrfIcPyrTGD52A2tkeShEEjDEjUtl-Y337E1sLrzxsDWy20tkIuF500G9ca2p_CPa06Lw6-q5z8HJ58by8Tlb3VzfL81UiKOUh0YIQqRGRjGZYVYxLzjRnvGRcYClZxjJK0lwTlpZlRhDjmtCSkYwyhpGQdA5OptyNs2-D8qFY28GZ-GXBaZ6lOaEoQniCKme9d0oXscleuG2BUTGuoPizgughk2caSLnf4P9NX__Tip0</recordid><startdate>20101101</startdate><enddate>20101101</enddate><creator>Polyak, B. 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Yu</creatorcontrib><creatorcontrib>Cheshko, A. L.</creatorcontrib><creatorcontrib>Prasolov, E. M.</creatorcontrib><creatorcontrib>Kamensky, I. 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G.</au><au>Lavrushin, V. Yu</au><au>Cheshko, A. L.</au><au>Prasolov, E. M.</au><au>Kamensky, I. L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Recent tectonomagmatic reactivation of the Kolyuchino-Mechigmen zone of the Chukchi Peninsula from data on the composition of gases in hydrothermal springs</atitle><jtitle>Geotectonics</jtitle><stitle>Geotecton</stitle><date>2010-11-01</date><risdate>2010</risdate><volume>44</volume><issue>6</issue><spage>529</spage><epage>540</epage><pages>529-540</pages><issn>0016-8521</issn><eissn>1556-1976</eissn><abstract>Thirty-three groups of thermal mineral springs in the Chukchi Peninsula are studied. The thermal fluids of the Kolyuchino-Mechigmen Zone (KMZ) show specific characteristics. The zone corresponds to recent depression with occurrences of basic volcanism and high seismicity. Characteristic features of the gases in the springs of the KMZ include the predominance of carbon dioxide, high percentage of mantle-derived helium, enrichment of CO
2
in
13
C, admixture of nonatmospheric nitrogen, excess in
40
Ar and
15
N relative to the atmosphere, maximal depletion of thermal water in deuterium and heavy oxygen isotope, and the highest estimates of deep temperature in reservoirs of hydrothermal fluid. All these features indicate the contemporary ascent of a mantle diapir that supplied helium enriched in
3
He and thermal energy to the crust, thus provoking thermal metamorphism of rocks and degradation of permafrost.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0016852110060063</doi><tpages>12</tpages></addata></record> |
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| subjects | Carbon dioxide Deuterium Diapirs Earth and Environmental Science Earth Sciences Geochemistry Geophysics Helium Magma Metamorphism Mineral springs Oxygen isotopes Permafrost Plate tectonics Soil degradation Structural Geology Thermal energy Thermal water Thermodynamics |
| title | Recent tectonomagmatic reactivation of the Kolyuchino-Mechigmen zone of the Chukchi Peninsula from data on the composition of gases in hydrothermal springs |
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