Background heat flow values in the region of the Sea of Okhotsk
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| Autori principali: | , , , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2006
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| _version_ | 1867169983428034560 |
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| author | Verzhbitsky, Evgeny V Berlin, Yury M Kononov, Mikhail V Marina, Mariya M |
| author_facet | Verzhbitsky, Evgeny V Berlin, Yury M Kononov, Mikhail V Marina, Mariya M |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Particular features of tectonic structure and anomalous distribution of geothermal, geomagnetic, and gravity fields in the region of the Sea of Okhotsk are considered. On the basis of heat flow data, ages of large-scale structures in the Sea of Okhotsk are estimated at 65 Ma for the Central Okhotsk Rise and 36 Ma for the South Okhotsk Basin. Age of the South Okhotsk Basin is confirmed by data on kinematics and corresponds to 50 km thickness of the lithosphere. This is in accordance with thickness value obtained by magnetotelluric soundings. Comparative analysis of model geothermal background and measured heat flow values on the Akademii Nauk Rise is performed. Analysis points to abnormally high (~20%) measured heat flow agrees with high negative gradient of gravity anomalies. Estimates of deep heat flow and basement age of riftogenic basins in the Sea of Okhotsk were carried out in the following areas: Deryugin Basin (18 Ma, Early Miocene), TINRO Basin (12 Ma, Middle Miocene), and West Kamchatka Basin (23 Ma, Late Oligocene). Temperatures at boundaries of the main lithological complexes of the sedimentary cover are calculated and zones of oil and gas generation are defined. On the basis of geothermal, magnetic, structural, and other geological-geophysical data a kinematic model of the region of the Sea of Okhotsk for period of 36 Ma was calculated and constructed. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_767388 |
| institution | PANGAEA |
| language | en |
| publishDate | 2006 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Background heat flow values in the region of the Sea of Okhotsk Verzhbitsky, Evgeny V Berlin, Yury M Kononov, Mikhail V Marina, Mariya M Archive of Ocean Data; ARCOD; Area/locality; Event label; Heat flow; Kamchatka Peninsula; Latitude of event; Longitude of event; Sakhalin Island; Sea of Okhotsk; Tatar Strait; VK06-1; VK06-10; VK06-11; VK06-12; VK06-13; VK06-14; VK06-15; VK06-16; VK06-17; VK06-18; VK06-19; VK06-2; VK06-20; VK06-21; VK06-22; VK06-23; VK06-24; VK06-25; VK06-26; VK06-27; VK06-28; VK06-29; VK06-3; VK06-30; VK06-31; VK06-32; VK06-33; VK06-34; VK06-35; VK06-36; VK06-37; VK06-38; VK06-39; VK06-4; VK06-40; VK06-41; VK06-42; VK06-43; VK06-44; VK06-5; VK06-6; VK06-7; VK06-8; VK06-9 Particular features of tectonic structure and anomalous distribution of geothermal, geomagnetic, and gravity fields in the region of the Sea of Okhotsk are considered. On the basis of heat flow data, ages of large-scale structures in the Sea of Okhotsk are estimated at 65 Ma for the Central Okhotsk Rise and 36 Ma for the South Okhotsk Basin. Age of the South Okhotsk Basin is confirmed by data on kinematics and corresponds to 50 km thickness of the lithosphere. This is in accordance with thickness value obtained by magnetotelluric soundings. Comparative analysis of model geothermal background and measured heat flow values on the Akademii Nauk Rise is performed. Analysis points to abnormally high (~20%) measured heat flow agrees with high negative gradient of gravity anomalies. Estimates of deep heat flow and basement age of riftogenic basins in the Sea of Okhotsk were carried out in the following areas: Deryugin Basin (18 Ma, Early Miocene), TINRO Basin (12 Ma, Middle Miocene), and West Kamchatka Basin (23 Ma, Late Oligocene). Temperatures at boundaries of the main lithological complexes of the sedimentary cover are calculated and zones of oil and gas generation are defined. On the basis of geothermal, magnetic, structural, and other geological-geophysical data a kinematic model of the region of the Sea of Okhotsk for period of 36 Ma was calculated and constructed. |
| title | Background heat flow values in the region of the Sea of Okhotsk |
| topic | Archive of Ocean Data; ARCOD; Area/locality; Event label; Heat flow; Kamchatka Peninsula; Latitude of event; Longitude of event; Sakhalin Island; Sea of Okhotsk; Tatar Strait; VK06-1; VK06-10; VK06-11; VK06-12; VK06-13; VK06-14; VK06-15; VK06-16; VK06-17; VK06-18; VK06-19; VK06-2; VK06-20; VK06-21; VK06-22; VK06-23; VK06-24; VK06-25; VK06-26; VK06-27; VK06-28; VK06-29; VK06-3; VK06-30; VK06-31; VK06-32; VK06-33; VK06-34; VK06-35; VK06-36; VK06-37; VK06-38; VK06-39; VK06-4; VK06-40; VK06-41; VK06-42; VK06-43; VK06-44; VK06-5; VK06-6; VK06-7; VK06-8; VK06-9 |
| url | https://doi.org/10.1594/PANGAEA.767388 |