| 000 | 01534nab a2200241 4500 | ||
|---|---|---|---|
| 005 | 20260521175404.0 | ||
| 008 | 260224s2018 xxu ing | ||
| 041 | _aInglés | ||
| 100 | 1 |
_aKosakowski, P. _958241 |
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| 100 | 1 |
_aKoltun, Y. _958242 |
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| 100 | 1 |
_aMachowski, G. _958243 |
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| 100 | 1 |
_aPoprawa, P. _958244 |
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| 100 | 1 |
_aPapiernik, B. _958245 |
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| 245 | 0 | 0 |
_aThe geochemical characteristics of the oligocene - lower miocene menilite formation in the polish and ukranian outer carpathians _bA review |
| 260 | _cjul. 2018 | ||
| 270 | _a22/01/2019 ; 22/01/2019 | ||
| 300 | _a17 p. ; 319-336 | ||
| 520 | _aTranscripción del resumen del autor: The principal source rocks in the Outer Carpathians are organic-rich shales in the Oligocene to Lower Miocene Menilite Formation. The average total organic carbon (TOC) content in the Menilite Formation is 4-8 wt%; the maximum measured is 26 wt%. Organic matter (OM) is oil-prone Type II kerogen derived mainly from algae and cyanobacteria which was deposited under euxinic conditions. The thermal maturity of the Menilite shales varies significantly within the Outer Carpathians, both vertically in relation to burial depth and laterally in different tectonic units, and increases from external to internal parts of the orogenic belt. Maturity in general ranges from immature to different phases of the "oil window" and up to the "gas window". | ||
| 581 | _a3 | ||
| 773 | 0 | _tJournal of Petroleum Geology | |
| 942 |
_cARTICULO _2ddc |
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| 999 |
_c192376 _d192376 |
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