Chemical structure and 13C NMR spectra of the kerogen of carbonaceous rock masses

被引：14

作者：

Bushnev, D. A. ^{[1
]}

Burdel'naya, N. S. ^{[1
]}

Mokeev, M. V. ^{[2
]}

Gribanov, A. V. ^{[2
]}

机构：

[1] Russian Acad Sci, Inst Geol, Komi Sci Ctr, Ural Div, Syktyvkar, Russia

[2] Russian Acad Sci, Inst Macromol Cpds, St Petersburg 199004, Russia

来源：

DOKLADY EARTH SCIENCES | 2010年 / 430卷 / 02期

关键词：

KASHPIR OIL SHALES; SPECTROSCOPY;

D O I：

10.1134/S1028334X10020145

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The spectra of the kerogen from the Middle Volga oil shales of the Volga-Pechora shale province and from the Ukhta domanik's carbonaceous deposits have been studied. In the Middle Volga and domanik kerogens, carbon-oxygen bonding types have been revealed as dominant. Significant distinctions between the two kerogen types have been established. The presence of oxygen in carbonyl and phenol groups is typical for the domanik kerogen, and also in ether bonds for the kerogen of the Middle Volga shale rock mass, which are of considerable importance in its structure.

引用

页码：210 / 213

页数：4

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