| 000 | 03458nlm1a2200457 4500 | ||
|---|---|---|---|
| 001 | 664160 | ||
| 005 | 20231030041920.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\35344 | ||
| 035 | _aRU\TPU\network\11852 | ||
| 090 | _a664160 | ||
| 100 | _a20210330a2019 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 102 | _aUS | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aSources of the Paleomagnetic Signal in Iron-Rich Marine Sedimentary Rocks _fM. A. Rudmin, A. K. Mazurov, V. I. Sergienko [et al.] |
|
| 203 |
_aText _celectronic |
||
| 300 | _aTitle screen | ||
| 320 | _a[References: p. 125 (10 tit.)] | ||
| 330 | _aIn this work, the results of interpreting the variation of the magnetic signal of iron-rich marine sedimentary rocks were presented by the example of the Cretaceous-Paleogene section of the Bakchar iron ore deposit (Western Siberia). The anomalous values of the magnetic susceptibility are determined by two factors: first, a superimposed diagenetic process accompanied by the formation of pyrrhotite, greigite, and siderite among ooidal ironstones; and second, an increase in the continental runoff, causing the accumulation of terrigenous magnetite and ilmenite in the siltstone as the climate becomes increasingly humid and the weathering intensifies. It was shown that the elevated values of the magnetic susceptibility in iron-rich deposits can be due to the formation of ferrimagnetic iron sulfides, which is indicative of methane mobilization through ancient bottom sediments. | ||
| 333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
| 461 | _tDoklady Chemistry | ||
| 463 |
_tVol. 486, No. 1 _v[P. 122-125] _d2019 |
||
| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aсигналы | |
| 610 | 1 | _aосадочные породы | |
| 610 | 1 | _aжелезо | |
| 610 | 1 | _aместорождения | |
| 610 | 1 | _aмагнитная восприимчивость | |
| 610 | 1 | _aдонные отложения | |
| 701 | 1 |
_aRudmin _bM. A. _cgeologist _cEngineer-researcher of Tomsk Polytechnic University _f1989- _gMaksim Andreevich _2stltpush _3(RuTPU)RU\TPU\pers\33254 |
|
| 701 | 1 |
_aMazurov _bA. K. _cgeologist _cProfessor of Tomsk Polytechnic University, Doctor sciences _f1951- _gAleksey Karpovich _2stltpush _3(RuTPU)RU\TPU\pers\30165 |
|
| 701 | 1 |
_aSergienko _bV. I. _gValentin |
|
| 701 | 1 |
_aSavichev _bO. G. _cgeologist _cProfessor of Tomsk Polytechnic University, doctor of geographical sciences _f1967- _gOleg Gennadievich _2stltpush _3(RuTPU)RU\TPU\pers\34024 |
|
| 701 | 1 |
_aSemiletov _bI. P. _cgeographer _cProfessor of Tomsk Polytechnic University, doctor of geographical Sciences _f1955- _gIgor Petrovich _2stltpush _3(RuTPU)RU\TPU\pers\34220 |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра геологии и разведки полезных ископаемых (ГРПИ) _bМеждународная научно-образовательная лаборатория изучения углерода арктических морей (МНОЛ ИУАМ) _h7398 _2stltpush _3(RuTPU)RU\TPU\col\20711 |
| 801 | 2 |
_aRU _b63413507 _c20210330 _gRCR |
|
| 856 | 4 | _uhttps://doi.org/10.1134/S0012500819050021 | |
| 942 | _cCF | ||