Late Quaternary history as a predicting base of future changing (in Russian).
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dc.contributor.author | Pavlidis, Yury A | |
dc.coverage.spatial | MEDIAN LATITUDE: 74.351867 * MEDIAN LONGITUDE: 51.884135 * SOUTH-BOUND LATITUDE: 68.416667 * WEST-BOUND LONGITUDE: 32.946667 * NORTH-BOUND LATITUDE: 79.420000 * EAST-BOUND LONGITUDE: 66.575000 * DATE/TIME START: 1984-07-01T00:00:00 * DATE/TIME END: 1987-09-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.00000 m * MAXIMUM DEPTH, sediment/rock: 2.02500 m | |
dc.date.accessioned | 2019-11-24T02:49:39Z | |
dc.date.available | 2019-11-24T02:49:39Z | |
dc.date.issued | 1998-07-20 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.53553 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.53553 | |
dc.identifier.citation | Pavlidis, Yury A; Ionin, A S; Scherbakov, F A; Dunaev, N N; Nikiforov, Sergey L (1986): Late Quaternary history as a predicting base of future changing (in Russian). GEOS, Moscow, 187 pp | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7439 | |
dc.format | text/tab-separated-values, 276 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.relation.isbasedon | Pavlidis, Yury A; Ionin, A S; Scherbakov, F A; Dunaev, N N; Nikiforov, Sergey L (1986): Late Quaternary history as a predicting base of future changing (in Russian). GEOS, Moscow, 187 pp | |
dc.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.subject | ADEPD | |
dc.subject | Atlantic Data Base for Exchange Processes at the Deep Sea Floor | |
dc.subject | Barents Sea | |
dc.subject | Calcium carbonate | |
dc.subject | Carbon, organic, total | |
dc.subject | DEPTH, sediment/rock | |
dc.subject | Element analysis TOC (Ljutsarev, 1986, Okeanologiya 26:704-708) | |
dc.subject | GC | |
dc.subject | Grab | |
dc.subject | GRAB | |
dc.subject | Gravity corer | |
dc.subject | Opal, biogenic silica | |
dc.subject | Professor Shtokman | |
dc.subject | PSh12 | |
dc.subject | PSh12-1263 | |
dc.subject | PSh12-1265 | |
dc.subject | PSh12-1266 | |
dc.subject | PSh12-1268 | |
dc.subject | PSh12-1269 | |
dc.subject | PSh12-1270 | |
dc.subject | PSh12-1271 | |
dc.subject | PSh12-1272 | |
dc.subject | PSh12-1273 | |
dc.subject | PSh12-1281 | |
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dc.subject | PSh12-1335 | |
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dc.subject | PSh12-1353 | |
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dc.subject | PSh12-1369 | |
dc.subject | PSh12-1370 | |
dc.subject | PSh12-1409 | |
dc.subject | PSh12-1410 | |
dc.subject | PSh12-1411 | |
dc.subject | PSh12-1412 | |
dc.subject | PSh12-1414 | |
dc.subject | PSh12-1415 | |
dc.subject | PSh12-1417 | |
dc.subject | PSh19 | |
dc.subject | PSh19-2060 | |
dc.subject | PSh19-2061 | |
dc.subject | PSh19-2062 | |
dc.subject | PSh19-2063 | |
dc.subject | PSh19-2064 | |
dc.subject | PSh19-2065 | |
dc.subject | PSh19-2066 | |
dc.subject | PSh19-2067 | |
dc.subject | PSh19-2120 | |
dc.subject | PSh19-2124 | |
dc.subject | PSh19-2136 | |
dc.subject | PSh19-2137 | |
dc.subject | PSh19-2138 | |
dc.subject | PSh19-2141 | |
dc.subject | PSh19-2142 | |
dc.subject | PSh19-2143 | |
dc.subject | PSh19-2144 | |
dc.subject | PSh19-2149 | |
dc.subject | PSh19-2163 | |
dc.subject | PSh19-2164 | |
dc.subject | PSh19-2167 | |
dc.subject | Quaternary Environment of the Eurasian North | |
dc.subject | QUEEN | |
dc.subject | Silicon Cycling in the World Ocean | |
dc.subject | SINOPS | |
dc.title | Late Quaternary history as a predicting base of future changing (in Russian). | |
dc.title.alternative | Opal, total organic carbon and calcium carbonate concentration of surface sediments | |
dc.type | Dataset |
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