| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2017 |
|
Морозов Владимир Петрович, автор
|
| Другие авторы |
EL-KADI MOHAMMAD |
|
Юсеф Ибрахем , автор
|
| Библиографическое описание на языке оригинала |
DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA |
| Аннотация |
Jorunal of petrolume geology |
| Ключевые слова |
Diagenesis, reservoir, sandstone, upper Triassic, Euphrates graben, Syria. |
| Место издания |
UK |
| Название журнала |
Jorunal of petrolume geology
|
| Издательство |
Wiley Online Library, Journal of Petroleum Geology |
| URL |
http://onlinelibrary.wiley.com/journal/10.1111/(ISSN)1747-5457 |
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=165477 |
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Морозов Владимир Петрович |
ru_RU |
| dc.contributor.author |
Юсеф Ибрахем |
ru_RU |
| dc.date.accessioned |
2017-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2017-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2017 |
ru_RU |
| dc.identifier.citation |
DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=165477 |
ru_RU |
| dc.description.abstract |
Jorunal of petrolume geology |
ru_RU |
| dc.description.abstract |
The upper Triassic sandstones are typically of quartz arenite; detrital quartz is the dominant phase (mean 74%). The authigenic minerals within the sandstones include quartz overgrowth (0.3~9%), kaolinite (traces~11%), chlorite (traces~13%), illite (traces~4%), illite-smectite mixture (traces~7%), dolomite (traces to 17%), siderite (traces to 23%), pyrite (traces to ~3%), anhydrite (traces~2%), barite (traces~6%), and anatase in traces amounts. The pore types recognized in the studied samples are intergranular pores, intragranular, oversized, micro-pores and fracture pores. The porosity values are ranges from 1% to 18% (with an average of 10%). The permeability values, ranging from 100 to 3880 millidarcy The diagenetic history of the upper Triassic sandstone has been greatly influenced by early diagenetic processes which included development of haematite, infiltration of detrital clay, precipitation of K-feldspar, precipitation of kaolinite, chlorite, pyrite, siderite, and anatase. |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.publisher |
Wiley Online Library, Journal of Petroleum Geology |
ru_RU |
| dc.subject |
Diagenesis |
ru_RU |
| dc.subject |
reservoir |
ru_RU |
| dc.subject |
sandstone |
ru_RU |
| dc.subject |
upper Triassic |
ru_RU |
| dc.subject |
Euphrates graben |
ru_RU |
| dc.subject |
Syria. |
ru_RU |
| dc.title |
DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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