| 000 | 03545nla2a2200445 4500 | ||
|---|---|---|---|
| 001 | 639774 | ||
| 005 | 20231030040330.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\4286 | ||
| 035 | _aRU\TPU\network\4285 | ||
| 090 | _a639774 | ||
| 100 | _a20150323a2015 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 105 | _ay z 100zy | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aLithology evaluation of a Bazhenov formation reservoir usingseismic and well log analysis _fN. Yu. Lomakina, V. B. Belozerov, N. V. Bukhanov |
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| 203 |
_aText _celectronic |
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| 300 | _aTitle screen | ||
| 320 | _a[References: 7 tit.] | ||
| 330 | _aThe Bazhenov formation is the analog of the Bakken formation; these formations are source rocks and contain tight reservoirs of a tectonic-hydrothermal model. The interpretation of well logs begins with the identification of the Bazhenov marker and tracing a carbonate layer within the Bazhenov formation by GR, neutron and DT logs. The thickness of this layer varies from 1 to 2 m. The next step is seismic interpretation. The creation of 2D seismic forward models is presented in this paper. In these models, the behavior of the amplitude with and without a carbonate layer was studied. These models allow tracing the sign of a carbonate layer (negative amplitude peak). The analysis of 3D seismic cube slices was performed. An amplitude map was created. The distribution of carbonate rock was detected according to this map. Thus, using this approach a thin layer was determined within the Bazhenov formation. | ||
| 333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
| 461 | 0 |
_0(RuTPU)RU\TPU\network\2499 _tIOP Conference Series: Earth and Environmental Science |
|
| 463 | 0 |
_0(RuTPU)RU\TPU\network\4016 _tVol. 24 : Scientific and Technical Challenges in the Well Drilling Progress, 24–27 November 2014, Tomsk, Russia _o[proceedings] _fNational Research Tomsk Polytechnic University (TPU) _v[012047, 10 p.] _d2015 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aлитология | |
| 610 | 1 | _aпласты | |
| 610 | 1 | _aбаженовская свита | |
| 610 | 1 | _aколлекторы | |
| 610 | 1 | _aкарбонатные породы | |
| 610 | 1 | _aуглеводородное сырье | |
| 610 | 1 | _aсейсмические данные | |
| 700 | 1 |
_aLomakina _bN. Yu. _cgeologist _cengineer of Tomsk Polytechnic University _f1990- _gNataliya Yurievna _2stltpush _3(RuTPU)RU\TPU\pers\34044 |
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| 701 | 1 |
_aBelozerov _bV. B. _cgeologist _cProfessor of Tomsk Polytechnic University, doctor of geological-mineralogical Sciences _f1951- _gVladimir Borisovich _2stltpush _3(RuTPU)RU\TPU\pers\33275 |
|
| 701 | 1 |
_aBukhanov _bN. V. _cgeologist _cengineer of Tomsk Polytechnic University _f1986- _gNikita Vladimirovich _2stltpush _3(RuTPU)RU\TPU\pers\34016 |
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| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bЦентр подготовки и переподготовки специалистов нефтегазового дела (ЦППС НД) _bЛаборатория геологии месторождений нефти и газа (ЛГМНГ) _h5263 _2stltpush _3(RuTPU)RU\TPU\col\19125 |
| 801 | 2 |
_aRU _b63413507 _c20161226 _gRCR |
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| 856 | 4 | _uhttp://dx.doi.org/10.1088/1755-1315/24/1/012047 | |
| 942 | _cCF | ||